<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-5614200336220321753</id><updated>2012-01-02T13:32:10.967-08:00</updated><category term='renison'/><category term='calcite'/><category term='coronadite'/><category term='clinochlore'/><category term='girilambone'/><category term='quartz'/><category term='whim creek'/><category term='wolfram camp'/><category term='chlorite'/><category term='tulendeena'/><category term='que river'/><category term='löllingite'/><category term='dolomite'/><category term='olympic dam'/><category term='dome rock'/><category term='hunter valley'/><category term='dundas'/><category term='pyromorphite'/><category term='agardite-y'/><category term='flinders'/><category term='emerald'/><category term='axinite-fe'/><category term='agardite'/><category term='browns prospect'/><category term='colebrook hill'/><category term='barite'/><category term='new south wales'/><category term='beryl'/><category term='hematite'/><category term='ashburton downs'/><category term='mitchell plateau'/><category term='wulfenite'/><category term='bismuth'/><category term='dravite'/><category term='azurite'/><category term='yowah'/><category term='crocoite'/><category term='coulsellite'/><category term='ferrimolybdite'/><category term='heazlewood'/><category term='auckland'/><category term='phillip island'/><category term='sphalerite'/><category term='cerussite'/><category term='hannayite'/><category term='acanthite'/><category term='heulandite'/><category term='axinite'/><category term='south australia'/><category term='hisingerite'/><category term='copper'/><category term='mt bischoff'/><category term='vivianite'/><category term='magnet mine'/><category term='western australia'/><category term='epidote'/><category term='fluorite'/><category term='bullabulling'/><category term='broken hill'/><category term='anatase'/><category term='thomsonite-ca'/><category term='ikaite'/><category term='waitakere'/><category term='glendonite'/><category term='alstonite'/><category term='coolac'/><category term='new zealand'/><category term='stolzite'/><category term='gartrellite'/><category term='kintore'/><category term='thomsonite'/><category term='gibbsite'/><category term='pseudomalachite'/><category term='muscovite'/><category term='yinnietharra'/><category term='spessartine'/><category term='gypsum'/><category term='rum jungle'/><category term='siderite'/><category term='pelion mine'/><category term='queensland'/><category term='northern territory'/><category term='feldspar'/><category term='analcime'/><category term='harts range'/><category term='lord brassey'/><category term='adelaide mine'/><category term='tasmania'/><category term='roxby downs'/><category term='bismuthinite'/><category term='bickers quarry'/><category term='pyrite'/><category term='natrolite'/><category term='luina'/><category term='victoria'/><category term='puttapa'/><category term='arsenopyrite'/><category term='libethenite'/><category term='mt moliagul'/><category term='oakleigh creek'/><category term='adamite'/><category term='minium'/><category term='opal'/><category term='tabba tabba'/><category term='galena'/><category term='mt lightning'/><category term='skipton'/><category term='block 14'/><category term='albite'/><category term='chlorargyrite'/><category term='sunderland bluff'/><category term='garawilla'/><category term='mt cleveland'/><category term='sulphur'/><category term='kimberley'/><category term='marrawah'/><category term='corop'/><category term='lake boga'/><category term='rosebery'/><category term='kitty miller bay'/><category term='hellyerite'/><category term='smithsonite'/><category term='mesolite'/><category term='lévyne'/><category term='tourmaline'/><title type='text'>⤱ Mineral Spot ⤱</title><subtitle type='html'>Information about minerals and localities, particularly in Australia and New Zealand</subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://mineral-spot.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>61</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3858476397754434125</id><published>2010-08-31T05:22:00.000-07:00</published><updated>2010-08-31T05:22:33.534-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='hellyerite'/><category scheme='http://www.blogger.com/atom/ns#' term='heazlewood'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='lord brassey'/><title type='text'>⤱ Hellyerite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THzyz-_bccI/AAAAAAAABG0/SOZgtysFis4/s1600/1498-hellyerite-lordbrassey-1.jpg" imageanchor="1" linkindex="74" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THzyz-_bccI/AAAAAAAABG0/SOZgtysFis4/s320/1498-hellyerite-lordbrassey-1.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Hellyerite is a very rare and unstable nickel carbonate mineral with a formula of NiCO&lt;sub&gt;3&lt;/sub&gt;.6H&lt;sub&gt;2&lt;/sub&gt;O.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Type Locality, the Lord Brassey Mine, Heazlewood district, Tasmania.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3858476397754434125?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3858476397754434125'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3858476397754434125'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/hellyerite.html' title='⤱ Hellyerite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THzyz-_bccI/AAAAAAAABG0/SOZgtysFis4/s72-c/1498-hellyerite-lordbrassey-1.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3502238595746684495</id><published>2010-08-31T05:14:00.000-07:00</published><updated>2010-08-31T05:14:57.113-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='skipton'/><category scheme='http://www.blogger.com/atom/ns#' term='hannayite'/><title type='text'>⤱ Hannayite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THzw8WtCYZI/AAAAAAAABGs/f8-r6aQyesk/s1600/1493-hannayite-skipton-01.jpg" imageanchor="1" linkindex="108" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THzw8WtCYZI/AAAAAAAABGs/f8-r6aQyesk/s320/1493-hannayite-skipton-01.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Hannayite is a very rare phosphate mineral that forms in cave guano. Its formula is (NH&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;Mg&lt;sub&gt;3&lt;/sub&gt;H&lt;sub&gt;4&lt;/sub&gt;(PO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;4&lt;/sub&gt;.8H&lt;sub&gt;2&lt;/sub&gt;O.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Type Locality, Skipton Cave, Victoria.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3502238595746684495?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3502238595746684495'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3502238595746684495'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/hannayite.html' title='⤱ Hannayite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THzw8WtCYZI/AAAAAAAABGs/f8-r6aQyesk/s72-c/1493-hannayite-skipton-01.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3630725520910774811</id><published>2010-08-31T05:07:00.000-07:00</published><updated>2010-08-31T05:07:12.110-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='kimberley'/><category scheme='http://www.blogger.com/atom/ns#' term='epidote'/><category scheme='http://www.blogger.com/atom/ns#' term='western australia'/><category scheme='http://www.blogger.com/atom/ns#' term='mitchell plateau'/><title type='text'>⤱ Epidote ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THzuarL0XiI/AAAAAAAABGk/-ETt21PNp9E/s1600/1492-epidote-kimberley.jpg" imageanchor="1" linkindex="181" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THzuarL0XiI/AAAAAAAABGk/-ETt21PNp9E/s320/1492-epidote-kimberley.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Epidote is a pistachio green silicate mineral that usually forms as transparent prismatic crystals. Its formula is Ca&lt;sub&gt;2&lt;/sub&gt;(Fe,Al)&lt;sub&gt;3&lt;/sub&gt;(SiO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;(OH).&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Mitchell Plateau in the Kimberley region of Western Australia.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3630725520910774811?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3630725520910774811'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3630725520910774811'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/epidote.html' title='⤱ Epidote ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THzuarL0XiI/AAAAAAAABGk/-ETt21PNp9E/s72-c/1492-epidote-kimberley.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-4150941601576981466</id><published>2010-08-31T04:55:00.000-07:00</published><updated>2010-08-31T04:55:37.368-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='emerald'/><category scheme='http://www.blogger.com/atom/ns#' term='bullabulling'/><category scheme='http://www.blogger.com/atom/ns#' term='western australia'/><category scheme='http://www.blogger.com/atom/ns#' term='beryl'/><title type='text'>⤱ Beryl ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/THztMJIFlpI/AAAAAAAABGc/cDUO0mXFvEc/s1600/1491-emerald-bullabulling.jpg" imageanchor="1" linkindex="91" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/THztMJIFlpI/AAAAAAAABGc/cDUO0mXFvEc/s320/1491-emerald-bullabulling.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Beryl is a beryllium silicate, formula Be&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;6&lt;/sub&gt;O&lt;sub&gt;18&lt;/sub&gt;, and provides us with a number of gem varieties such as emerald (green), aquamarine (blue) and morganite (pink). It often occurs as prismatic crystals embedded in the surrounding matrix and can be difficult to extract without damage.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a specimen of green emerald beryl from Bullabulling in Western Australia.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-4150941601576981466?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4150941601576981466'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4150941601576981466'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/beryl_31.html' title='⤱ Beryl ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/THztMJIFlpI/AAAAAAAABGc/cDUO0mXFvEc/s72-c/1491-emerald-bullabulling.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-8620550209870848588</id><published>2010-08-31T04:51:00.000-07:00</published><updated>2010-08-31T04:51:56.235-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='azurite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='girilambone'/><title type='text'>⤱ Azurite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/THzrS9_OE5I/AAAAAAAABGU/gIcILGX47ss/s1600/1489-azurite-girilambone.jpg" imageanchor="1" linkindex="17" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/THzrS9_OE5I/AAAAAAAABGU/gIcILGX47ss/s320/1489-azurite-girilambone.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Azurite is a deep blue common secondary copper carbonate mineral found in the oxidised zone of copper ore bodies. Its formula is Cu&lt;sub&gt;3&lt;/sub&gt;(CO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;(OH)&lt;sub&gt;2&lt;/sub&gt;.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from Girilambone, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-8620550209870848588?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/8620550209870848588'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/8620550209870848588'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/azurite.html' title='⤱ Azurite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/THzrS9_OE5I/AAAAAAAABGU/gIcILGX47ss/s72-c/1489-azurite-girilambone.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6010188482732012799</id><published>2010-08-31T04:43:00.000-07:00</published><updated>2010-08-31T04:43:57.015-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='libethenite'/><category scheme='http://www.blogger.com/atom/ns#' term='girilambone'/><title type='text'>⤱ Libethenite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THzqxUQOVNI/AAAAAAAABGM/PHemyqDPsXs/s1600/1476-libethenite-girilambone.jpg" imageanchor="1" linkindex="345" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THzqxUQOVNI/AAAAAAAABGM/PHemyqDPsXs/s320/1476-libethenite-girilambone.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Libethenite is a green copper phosphate mineral with a formula of Cu&lt;sub&gt;2&lt;/sub&gt;PO&lt;sub&gt;4&lt;/sub&gt;OH.&lt;br /&gt;&lt;br /&gt;This specimen is from Girilambone, New South Wales. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6010188482732012799?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6010188482732012799'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6010188482732012799'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/libethenite_2937.html' title='⤱ Libethenite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THzqxUQOVNI/AAAAAAAABGM/PHemyqDPsXs/s72-c/1476-libethenite-girilambone.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-1538444374625504530</id><published>2010-08-31T04:40:00.000-07:00</published><updated>2010-08-31T04:40:27.074-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='pseudomalachite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='girilambone'/><title type='text'>⤱ Pseudomalachite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THzopdm_hbI/AAAAAAAABGE/5Gxkwoo-bEQ/s1600/1466-pseudomalachite-girilambone.jpg" imageanchor="1" linkindex="119" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THzopdm_hbI/AAAAAAAABGE/5Gxkwoo-bEQ/s320/1466-pseudomalachite-girilambone.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Psuedomalachite is a blue-green copper phosphate often confused with malachite. Crystals are rare. Its formula is Cu&lt;sub&gt;5&lt;/sub&gt;(PO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;(OH)&lt;sub&gt;4&lt;/sub&gt;.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from Girilambone, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-1538444374625504530?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1538444374625504530'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1538444374625504530'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/pseudomalachite.html' title='⤱ Pseudomalachite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THzopdm_hbI/AAAAAAAABGE/5Gxkwoo-bEQ/s72-c/1466-pseudomalachite-girilambone.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3270923943017430242</id><published>2010-08-31T04:32:00.000-07:00</published><updated>2010-08-31T04:32:50.991-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='libethenite'/><category scheme='http://www.blogger.com/atom/ns#' term='girilambone'/><title type='text'>⤱ Libethenite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THzoHZTxOAI/AAAAAAAABF8/6e7gbFgX-9s/s1600/1465-libethenite-girilambone.jpg" imageanchor="1" linkindex="19" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THzoHZTxOAI/AAAAAAAABF8/6e7gbFgX-9s/s320/1465-libethenite-girilambone.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;Libethenite is a green copper phosphate mineral with a formula of Cu&lt;sub&gt;2&lt;/sub&gt;PO&lt;sub&gt;4&lt;/sub&gt;OH.&lt;br /&gt;&lt;br /&gt;This specimen is from Girilambone, New South Wales.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3270923943017430242?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3270923943017430242'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3270923943017430242'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/libethenite_31.html' title='⤱ Libethenite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THzoHZTxOAI/AAAAAAAABF8/6e7gbFgX-9s/s72-c/1465-libethenite-girilambone.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-107533786890188608</id><published>2010-08-26T05:12:00.000-07:00</published><updated>2010-08-26T05:12:28.998-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='libethenite'/><category scheme='http://www.blogger.com/atom/ns#' term='girilambone'/><title type='text'>⤱ Libethenite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/THZX8N8fUmI/AAAAAAAABF0/_KdsicPj5j8/s1600/1462-libethenite-girilambone.jpg" imageanchor="1" linkindex="397" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/THZX8N8fUmI/AAAAAAAABF0/_KdsicPj5j8/s320/1462-libethenite-girilambone.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Libethenite is a green copper phosphate mineral with a formula of Cu&lt;sub&gt;2&lt;/sub&gt;PO&lt;sub&gt;4&lt;/sub&gt;OH.&lt;br /&gt;&lt;br /&gt;This specimen shows the typical triangular crystal cross-section and is from Girilambone, New South Wales. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-107533786890188608?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/107533786890188608'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/107533786890188608'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/libethenite.html' title='⤱ Libethenite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/THZX8N8fUmI/AAAAAAAABF0/_KdsicPj5j8/s72-c/1462-libethenite-girilambone.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-2933274337835364244</id><published>2010-08-26T04:59:00.000-07:00</published><updated>2010-08-26T04:59:49.453-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='sphalerite'/><category scheme='http://www.blogger.com/atom/ns#' term='que river'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='galena'/><title type='text'>⤱ Sphalerite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THZV-kgAM7I/AAAAAAAABFs/WkDJv52Co4w/s1600/1454-sphalerite-que.jpg" imageanchor="1" linkindex="42" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THZV-kgAM7I/AAAAAAAABFs/WkDJv52Co4w/s320/1454-sphalerite-que.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Sphalerite is a zinc sulphide that can have varying amounts of iron, and that forms as crystals that may be almost colourless through orange, red and brown to almost black, and occasionally green. Its formula is ZnS.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Que River Mine, Tasmania and also contains small silver galena.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-2933274337835364244?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2933274337835364244'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2933274337835364244'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/sphalerite.html' title='⤱ Sphalerite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THZV-kgAM7I/AAAAAAAABFs/WkDJv52Co4w/s72-c/1454-sphalerite-que.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-2887907689484356388</id><published>2010-08-26T04:51:00.000-07:00</published><updated>2010-08-26T04:51:30.581-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='pyrite'/><category scheme='http://www.blogger.com/atom/ns#' term='corop'/><title type='text'>⤱ Pyrite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THZUA6auuzI/AAAAAAAABFk/ZlxmKP_qJ7c/s1600/1445-pyrite-corop-4mm.jpg" imageanchor="1" linkindex="199" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THZUA6auuzI/AAAAAAAABFk/ZlxmKP_qJ7c/s320/1445-pyrite-corop-4mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Pyrite is a common mineral and sometimes mistaken for gold (known as "Fool's Gold" and "Iron Pyrites"). It is brassy yellow and metallic and generally forms as cubes. Its formula is FeS&lt;sub&gt;2&lt;/sub&gt;.&lt;br /&gt;&lt;br /&gt;The surface of the cubes on this specimen have tarnished. It comes from Corop, Victoria.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-2887907689484356388?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2887907689484356388'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2887907689484356388'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/pyrite.html' title='⤱ Pyrite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THZUA6auuzI/AAAAAAAABFk/ZlxmKP_qJ7c/s72-c/1445-pyrite-corop-4mm.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-4116508184823024348</id><published>2010-08-26T04:29:00.000-07:00</published><updated>2010-08-26T04:29:53.643-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='corop'/><category scheme='http://www.blogger.com/atom/ns#' term='barite'/><title type='text'>⤱ Barite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THZPxpDPj8I/AAAAAAAABFc/fx9B_N-Vt3I/s1600/1444-barite-corop-9mm.jpg" imageanchor="1" linkindex="81" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THZPxpDPj8I/AAAAAAAABFc/fx9B_N-Vt3I/s320/1444-barite-corop-9mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Barite, also spelled baryte, is a barium sulphate mineral with a formula BaSO&lt;sub&gt;4&lt;/sub&gt;.&amp;nbsp;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a specimen from Corop, Victoria, and is rare at the locality. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-4116508184823024348?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4116508184823024348'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4116508184823024348'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/barite_26.html' title='⤱ Barite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THZPxpDPj8I/AAAAAAAABFc/fx9B_N-Vt3I/s72-c/1444-barite-corop-9mm.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5991418812832631797</id><published>2010-08-26T04:14:00.000-07:00</published><updated>2010-08-26T04:14:27.562-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='dravite'/><category scheme='http://www.blogger.com/atom/ns#' term='western australia'/><category scheme='http://www.blogger.com/atom/ns#' term='tourmaline'/><category scheme='http://www.blogger.com/atom/ns#' term='yinnietharra'/><title type='text'>⤱ Dravite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THZKy2SCoXI/AAAAAAAABFU/uU54E0EIYVw/s1600/1438-dravite-yinnietharra.jpg" imageanchor="1" linkindex="182" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THZKy2SCoXI/AAAAAAAABFU/uU54E0EIYVw/s320/1438-dravite-yinnietharra.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Dravite is one of the tourmaline group of minerals, usually brown in colour, and with a formula of NaMg&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;6&lt;/sub&gt;(BO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;Si&lt;sub&gt;6&lt;/sub&gt;O&lt;sub&gt;18&lt;/sub&gt;(OH)&lt;sub&gt;4&lt;/sub&gt;.&lt;br /&gt;&lt;br /&gt;This specimen is from Yinnitharra in Western Australia and clearly shows an inclusion of another mineral, possibly monazite?&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5991418812832631797?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5991418812832631797'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5991418812832631797'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/dravite.html' title='⤱ Dravite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THZKy2SCoXI/AAAAAAAABFU/uU54E0EIYVw/s72-c/1438-dravite-yinnietharra.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-2484576901138540281</id><published>2010-08-26T04:01:00.000-07:00</published><updated>2010-08-26T04:01:52.899-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='mt moliagul'/><category scheme='http://www.blogger.com/atom/ns#' term='ferrimolybdite'/><title type='text'>⤱ Ferrimolybdite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THZIUTbPL6I/AAAAAAAABFM/gQhKMDIG6h0/s1600/1436-ferrimolybdite-mtmoliagul-01.jpg" imageanchor="1" linkindex="26" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THZIUTbPL6I/AAAAAAAABFM/gQhKMDIG6h0/s320/1436-ferrimolybdite-mtmoliagul-01.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Ferrimolybdite is a fibrous yellow alteration product of molybdenite. Its formula is Fe&lt;sub&gt;2&lt;/sub&gt;(MoO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;.nH&lt;sub&gt;2&lt;/sub&gt;0.&lt;br /&gt;&lt;br /&gt;This specimen is from Mt Moliagul, Victoria. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-2484576901138540281?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2484576901138540281'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2484576901138540281'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/ferrimolybdite.html' title='⤱ Ferrimolybdite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THZIUTbPL6I/AAAAAAAABFM/gQhKMDIG6h0/s72-c/1436-ferrimolybdite-mtmoliagul-01.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6876778327725523102</id><published>2010-08-26T03:52:00.000-07:00</published><updated>2010-08-26T03:59:09.464-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='calcite'/><category scheme='http://www.blogger.com/atom/ns#' term='phillip island'/><category scheme='http://www.blogger.com/atom/ns#' term='kitty miller bay'/><title type='text'>⤱ Calcite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THZGKpFElcI/AAAAAAAABFE/cUf4oqrR5lY/s1600/1424-calcite-kittymiller.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THZGKpFElcI/AAAAAAAABFE/cUf4oqrR5lY/s320/1424-calcite-kittymiller.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Calcite is a calcium carbonate mineral and has more crystal forms than any other mineral species. Its formula is CaCO&lt;sub&gt;3&lt;/sub&gt;.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a specimen of 'agate-patterned calcite'&amp;nbsp; locally called 'eye agates' that forms as infillings of vescicles in basalt, and is from Kitty Miller Bay, Phillip Island, Victoria. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6876778327725523102?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6876778327725523102'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6876778327725523102'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/calcite.html' title='⤱ Calcite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THZGKpFElcI/AAAAAAAABFE/cUf4oqrR5lY/s72-c/1424-calcite-kittymiller.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7902371328509887993</id><published>2010-08-26T03:43:00.000-07:00</published><updated>2010-08-26T03:43:40.622-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='yowah'/><category scheme='http://www.blogger.com/atom/ns#' term='queensland'/><category scheme='http://www.blogger.com/atom/ns#' term='opal'/><title type='text'>⤱ Opal ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THZDXXU7VAI/AAAAAAAABE8/krl1oTjSZ8Y/s1600/1400-opal-yowah-1.jpg" imageanchor="1" linkindex="51" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THZDXXU7VAI/AAAAAAAABE8/krl1oTjSZ8Y/s320/1400-opal-yowah-1.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Opal is an amorphous form of silica with a formula of SiO&lt;sub&gt;2&lt;/sub&gt;.nH&lt;sub&gt;2&lt;/sub&gt;O. Opal without 'fire' is usually referred to as potch. Colourless opal that forms as spheres is known as hyalite, and this form is often fluorescent under UV light. The form that has 'fire' or a play of colour is known as precious opal.&lt;br /&gt;&lt;br /&gt;This specimen is boulder opal (Yowah Nut) from Yowah, Queensland.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7902371328509887993?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7902371328509887993'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7902371328509887993'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/opal.html' title='⤱ Opal ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THZDXXU7VAI/AAAAAAAABE8/krl1oTjSZ8Y/s72-c/1400-opal-yowah-1.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6669808324691477753</id><published>2010-08-26T03:32:00.000-07:00</published><updated>2010-08-26T03:32:59.847-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='copper'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Copper ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THZBxnJXV6I/AAAAAAAABE0/CuDzFB9NUEs/s1600/1381-copper-brokenhill-39mm-1-2009-04-04.jpg" imageanchor="1" linkindex="4" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THZBxnJXV6I/AAAAAAAABE0/CuDzFB9NUEs/s320/1381-copper-brokenhill-39mm-1-2009-04-04.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;Copper is one of the native elements, formula Cu. It has been known, mined and used for thousands of years. It often forms as crystals or groups of crystals, sometimes forming branching or dendritic groups.&lt;br /&gt;&lt;br /&gt;This unusual specimen is from Broken Hill, New South Wales.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6669808324691477753?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6669808324691477753'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6669808324691477753'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/copper.html' title='⤱ Copper ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THZBxnJXV6I/AAAAAAAABE0/CuDzFB9NUEs/s72-c/1381-copper-brokenhill-39mm-1-2009-04-04.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-877187794501835841</id><published>2010-08-26T03:25:00.001-07:00</published><updated>2010-08-26T03:25:53.267-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='kintore'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='smithsonite'/><title type='text'>⤱ Smithsonite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THZBB9oGQYI/AAAAAAAABEs/OufIfyu7XYw/s1600/1380-smithsonite-kintore.jpg" imageanchor="1" linkindex="201" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THZBB9oGQYI/AAAAAAAABEs/OufIfyu7XYw/s320/1380-smithsonite-kintore.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Smithsonite is a zinc carbonate mineral with a formula of ZnCO&lt;sub&gt;3&lt;/sub&gt;. It is common in the oxidised zone of zinc ore deposits. Smithsonite can occur as individual rhombohedral crystals, or more commonly, aggregates that form spherical groups.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Kintore Open Cut, Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-877187794501835841?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/877187794501835841'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/877187794501835841'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/smithsonite_26.html' title='⤱ Smithsonite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THZBB9oGQYI/AAAAAAAABEs/OufIfyu7XYw/s72-c/1380-smithsonite-kintore.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7116974332179813936</id><published>2010-08-26T03:22:00.000-07:00</published><updated>2010-08-26T03:22:13.438-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='block 14'/><category scheme='http://www.blogger.com/atom/ns#' term='cerussite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Cerussite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/THY_P98MrQI/AAAAAAAABEk/wU0IQ3fwTWI/s1600/1377-cerussite-block14.jpg" imageanchor="1" linkindex="77" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/THY_P98MrQI/AAAAAAAABEk/wU0IQ3fwTWI/s320/1377-cerussite-block14.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Cerussite is a lead carbonate mineral with a formula of PbCO&lt;sub&gt;3&lt;/sub&gt;. It is common in the oxidised zone of lead ore deposits. Most crystals are colourless, white or cream.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Block 14 Open Cut, Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7116974332179813936?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7116974332179813936'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7116974332179813936'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/cerussite_26.html' title='⤱ Cerussite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/THY_P98MrQI/AAAAAAAABEk/wU0IQ3fwTWI/s72-c/1377-cerussite-block14.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-2019450412036937934</id><published>2010-08-26T03:15:00.000-07:00</published><updated>2010-08-26T03:15:45.896-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='kintore'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='smithsonite'/><title type='text'>⤱ Smithsonite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THY8sQeXDdI/AAAAAAAABEc/byTtIT05qH0/s1600/1368-smithsonite-kintore.jpg" imageanchor="1" linkindex="200" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THY8sQeXDdI/AAAAAAAABEc/byTtIT05qH0/s320/1368-smithsonite-kintore.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Smithsonite is a zinc carbonate mineral with a formula of ZnCO&lt;sub&gt;3&lt;/sub&gt;. It is common in the oxidised zone of zinc ore deposits. Smithsonite can occur as individual rhombohedral crystals, or more commonly, aggregates that form spherical groups.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Kintore Open Cut, Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-2019450412036937934?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2019450412036937934'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2019450412036937934'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/smithsonite.html' title='⤱ Smithsonite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THY8sQeXDdI/AAAAAAAABEc/byTtIT05qH0/s72-c/1368-smithsonite-kintore.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7531129230218420701</id><published>2010-08-25T05:12:00.000-07:00</published><updated>2010-08-25T05:12:04.484-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='coolac'/><category scheme='http://www.blogger.com/atom/ns#' term='chlorite'/><category scheme='http://www.blogger.com/atom/ns#' term='clinochlore'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='mt lightning'/><title type='text'>⤱ Clinochlore ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/THUHDLP4jaI/AAAAAAAABEU/diOoNBWj3vQ/s1600/1357-clinochlore-coolac-1.jpg" imageanchor="1" linkindex="350" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/THUHDLP4jaI/AAAAAAAABEU/diOoNBWj3vQ/s320/1357-clinochlore-coolac-1.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Clinochlore is one of the chlorite group of minerals with a formula of (MgFe)5Al(Si3Al)O10(OH)8 and is usually green.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;This specimen is unusual in that it is colourless. It comes from Mt Lightning, near Coolac, New South Wales.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7531129230218420701?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7531129230218420701'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7531129230218420701'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/clinochlore.html' title='⤱ Clinochlore ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/THUHDLP4jaI/AAAAAAAABEU/diOoNBWj3vQ/s72-c/1357-clinochlore-coolac-1.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7609817011168339450</id><published>2010-08-25T05:01:00.000-07:00</published><updated>2010-08-25T05:01:22.678-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='cerussite'/><category scheme='http://www.blogger.com/atom/ns#' term='magnet mine'/><title type='text'>⤱ Cerussite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THUEZL-yeYI/AAAAAAAABEM/ClOKMkSdE8s/s1600/1352-cerussite-magnet-4mm.jpg" imageanchor="1" linkindex="30" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THUEZL-yeYI/AAAAAAAABEM/ClOKMkSdE8s/s320/1352-cerussite-magnet-4mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Cerussite is a lead carbonate mineral with a formula of PbCO&lt;sub&gt;3&lt;/sub&gt;. It is common in the oxidised zone of lead ore deposits. Most crystals are colourless, white or cream. So-called 'chrome' cerussite is a yellow form.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Magnet Mine, near Waratah, Tasmania, the Type Locality for 'chrome' cerussite.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7609817011168339450?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7609817011168339450'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7609817011168339450'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/cerussite.html' title='⤱ Cerussite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THUEZL-yeYI/AAAAAAAABEM/ClOKMkSdE8s/s72-c/1352-cerussite-magnet-4mm.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7653301858131016970</id><published>2010-08-25T04:50:00.000-07:00</published><updated>2010-08-25T04:50:11.314-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='spessartine'/><category scheme='http://www.blogger.com/atom/ns#' term='kintore'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Spessartine ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THUCpvY8uiI/AAAAAAAABEE/rvwxXnJtYTM/s1600/1351-spessartine-kintore.jpg" imageanchor="1" linkindex="102" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THUCpvY8uiI/AAAAAAAABEE/rvwxXnJtYTM/s320/1351-spessartine-kintore.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Spessartine is one of the garnet group minerals and has a formula of Mn&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;(SiO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;. It is usually red or orange in colour, and occurs as transparent to translucent distinct crystals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen has formed as a sharp crystal and is from the Kintore Open Cut, Broken Hill, New South Wales. Spessartine is common, even characteristic, at this locality.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7653301858131016970?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7653301858131016970'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7653301858131016970'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/spessartine_25.html' title='⤱ Spessartine ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THUCpvY8uiI/AAAAAAAABEE/rvwxXnJtYTM/s72-c/1351-spessartine-kintore.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3700812078251396029</id><published>2010-08-25T04:25:00.000-07:00</published><updated>2010-08-25T04:25:50.741-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='auckland'/><category scheme='http://www.blogger.com/atom/ns#' term='thomsonite-ca'/><category scheme='http://www.blogger.com/atom/ns#' term='new zealand'/><category scheme='http://www.blogger.com/atom/ns#' term='thomsonite'/><category scheme='http://www.blogger.com/atom/ns#' term='waitakere'/><title type='text'>⤱ Thomsonite-Ca ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THT6cFJEc6I/AAAAAAAABD8/AdxHili5h9w/s1600/1284-thomsonite-auckland-1.jpg" imageanchor="1" linkindex="146" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THT6cFJEc6I/AAAAAAAABD8/AdxHili5h9w/s320/1284-thomsonite-auckland-1.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Thomsonite is one of the zeolite group of minerals and occurs as colourless thin prismatic crystals with a rectangular cross-section, or else as white fibrous masses or hemispheres. Its formula is NaCa&lt;sub&gt;2&lt;/sub&gt;Al&lt;sub&gt;5&lt;/sub&gt;Si&lt;sub&gt;5&lt;/sub&gt;O&lt;sub&gt;20&lt;/sub&gt;.6H&lt;sub&gt;2&lt;/sub&gt;O.&lt;/div&gt;&lt;br /&gt;This specimen is from the Waitakere Volcanics, West Auckland, North Island, New Zealand.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3700812078251396029?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3700812078251396029'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3700812078251396029'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/thomsonite-ca.html' title='⤱ Thomsonite-Ca ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THT6cFJEc6I/AAAAAAAABD8/AdxHili5h9w/s72-c/1284-thomsonite-auckland-1.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7015330080500790405</id><published>2010-08-25T04:06:00.000-07:00</published><updated>2010-08-25T04:06:22.248-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='siderite'/><category scheme='http://www.blogger.com/atom/ns#' term='new zealand'/><category scheme='http://www.blogger.com/atom/ns#' term='bickers quarry'/><title type='text'>⤱ Siderite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/THT4DhvPfaI/AAAAAAAABD0/zqTcoORduxc/s1600/1278-siderite-bickers-1.jpg" imageanchor="1" linkindex="160" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/THT4DhvPfaI/AAAAAAAABD0/zqTcoORduxc/s320/1278-siderite-bickers-1.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Siderite is a common iron carbonate that is usually brown in colour and often forms rhombohedral crystals. Its formula is FeCO&lt;sub&gt;3&lt;/sub&gt;.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from Bicker's Quarry, a basalt quarry near Tokatoka, Northland, North Island, New Zealand.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7015330080500790405?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7015330080500790405'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7015330080500790405'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/siderite.html' title='⤱ Siderite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/THT4DhvPfaI/AAAAAAAABD0/zqTcoORduxc/s72-c/1278-siderite-bickers-1.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5182412095149869740</id><published>2010-08-24T05:35:00.000-07:00</published><updated>2010-08-24T05:35:13.616-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='new zealand'/><category scheme='http://www.blogger.com/atom/ns#' term='analcime'/><category scheme='http://www.blogger.com/atom/ns#' term='bickers quarry'/><title type='text'>⤱ Analcime ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THO8JGgfGTI/AAAAAAAABDs/CwSqgkh7Pr8/s1600/1273-analcime-bickers-2.jpg" imageanchor="1" linkindex="69" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THO8JGgfGTI/AAAAAAAABDs/CwSqgkh7Pr8/s320/1273-analcime-bickers-2.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Analcime (sometimes known as 'analcite') is a common member of the zeolite group of minerals with a formula of Na&lt;sub&gt;2&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;4&lt;/sub&gt;O&lt;sub&gt;12&lt;/sub&gt;.2H&lt;sub&gt;2&lt;/sub&gt;O&lt;span style="font-family: &amp;quot;Calibri&amp;quot;,&amp;quot;sans-serif&amp;quot;; font-size: 11pt; line-height: 115%;"&gt;&lt;/span&gt; and occurs as colourless trapezohedral crystals in cavities in volcanic basalt rocks. Often, these crystals 'craze' and turn white after being exposed. Crystals may also appear to be the same colour as the underlying matrix, they are so transparent.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from Bicker's Quarry, a basalt quarry near Tokatoka, Northland, North Island, New Zealand. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5182412095149869740?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5182412095149869740'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5182412095149869740'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/analcime_24.html' title='⤱ Analcime ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THO8JGgfGTI/AAAAAAAABDs/CwSqgkh7Pr8/s72-c/1273-analcime-bickers-2.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-1565747122453139635</id><published>2010-08-24T05:25:00.000-07:00</published><updated>2010-08-24T05:25:50.553-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='gypsum'/><category scheme='http://www.blogger.com/atom/ns#' term='new zealand'/><category scheme='http://www.blogger.com/atom/ns#' term='bickers quarry'/><title type='text'>⤱ Gypsum ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THO4qqhttSI/AAAAAAAABDk/E0DcsV0e4Y8/s1600/1272-gypsum-bickers-1.jpg" imageanchor="1" linkindex="72" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THO4qqhttSI/AAAAAAAABDk/E0DcsV0e4Y8/s320/1272-gypsum-bickers-1.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Gypsum is a very soft calcium sulphate mineral that can be scratched with a fingernail, and is also water-soluble. It may occur as colourless transparent crystals with a high lustre, "rams's horn" curved crystals, and fishtail twins. It has a formula of Ca(SO&lt;sub&gt;4&lt;/sub&gt;).2H&lt;sub&gt;2&lt;/sub&gt;O.&lt;br /&gt;&lt;br /&gt;This specimen is from Bicker's Quarry, a basalt quarry near Tokatoka, Northland, North Island, New Zealand.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-1565747122453139635?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1565747122453139635'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1565747122453139635'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/gypsum.html' title='⤱ Gypsum ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THO4qqhttSI/AAAAAAAABDk/E0DcsV0e4Y8/s72-c/1272-gypsum-bickers-1.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7780581136429431657</id><published>2010-08-24T05:07:00.000-07:00</published><updated>2010-08-24T05:10:10.433-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='axinite-fe'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='colebrook hill'/><category scheme='http://www.blogger.com/atom/ns#' term='axinite'/><title type='text'>⤱ Axinite-(Fe) ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THOzKxNBFFI/AAAAAAAABDc/hg89VAEC0k4/s1600/1263-ferroaxinite-colebrookhill-4mm.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THOzKxNBFFI/AAAAAAAABDc/hg89VAEC0k4/s320/1263-ferroaxinite-colebrookhill-4mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;span style="font-size: small;"&gt;Axinite-(Fe) or ferroaxinite is the iron-rich member of the axinite group of borosilicates, and forms brownish crystals.&lt;/span&gt; Its formula is Ca&lt;sub&gt;2&lt;/sub&gt;FeAl&lt;sub&gt;2&lt;/sub&gt;BO&lt;sub&gt;3&lt;/sub&gt;Si&lt;sub&gt;4&lt;/sub&gt;O&lt;sub&gt;12&lt;/sub&gt;OH.&lt;br /&gt;&lt;br /&gt;This specimen is a single crystal from Colebrook Hill, near Rosebery, Tasmania.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7780581136429431657?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7780581136429431657'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7780581136429431657'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/axinite-fe.html' title='⤱ Axinite-(Fe) ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THOzKxNBFFI/AAAAAAAABDc/hg89VAEC0k4/s72-c/1263-ferroaxinite-colebrookhill-4mm.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5851144396583677341</id><published>2010-08-24T04:43:00.000-07:00</published><updated>2010-08-24T04:43:00.493-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='heulandite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='garawilla'/><title type='text'>⤱ Heulandite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THOu4CfZWtI/AAAAAAAABDU/tnFYZFO4OKw/s1600/1257-heulandite-garawilla.jpg" imageanchor="1" linkindex="124" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THOu4CfZWtI/AAAAAAAABDU/tnFYZFO4OKw/s320/1257-heulandite-garawilla.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Heulandite is the name given to a series of zeolite minerals and characteristically have a coffin-shaped habit. They are usually colourless, but can be orange to red.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Garawilla Volcanics in New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5851144396583677341?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5851144396583677341'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5851144396583677341'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/heulandite.html' title='⤱ Heulandite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THOu4CfZWtI/AAAAAAAABDU/tnFYZFO4OKw/s72-c/1257-heulandite-garawilla.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-1252699579590909924</id><published>2010-08-24T02:56:00.000-07:00</published><updated>2010-08-24T02:56:24.286-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='arsenopyrite'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='dolomite'/><category scheme='http://www.blogger.com/atom/ns#' term='renison'/><title type='text'>⤱ Dolomite, Arsenopyrite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THOV-nJPZEI/AAAAAAAABDM/n0YycQSbq7o/s1600/1256-dolomite-arsenopyrite-renison-8mm.jpg" imageanchor="1" linkindex="35" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THOV-nJPZEI/AAAAAAAABDM/n0YycQSbq7o/s320/1256-dolomite-arsenopyrite-renison-8mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;span style="font-size: small;"&gt;Dolomite is a magnesium-bearing carbonate mineral, formula CaMg(CO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;, and often occurs as saddle-shaped crystals. Arsenopyrite is an iron arsenic sulphide mineral that occurs as silver crystals. It's formula is FeAsS.&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;&lt;span style="font-size: small;"&gt;This specimen has spherical aggregates of dolomite crystals with well-formed arsenopyrite crystals from the Renison Mine, Tasmania.&lt;/span&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-1252699579590909924?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1252699579590909924'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1252699579590909924'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/dolomite-arsenopyrite.html' title='⤱ Dolomite, Arsenopyrite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THOV-nJPZEI/AAAAAAAABDM/n0YycQSbq7o/s72-c/1256-dolomite-arsenopyrite-renison-8mm.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-4925005230922079544</id><published>2010-08-23T05:55:00.000-07:00</published><updated>2010-08-23T05:55:05.430-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='calcite'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='marrawah'/><category scheme='http://www.blogger.com/atom/ns#' term='natrolite'/><title type='text'>⤱ Natrolite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THJuh3JjkII/AAAAAAAABDE/b-rfNQZh-Mk/s1600/1209-calcite-marrawah-9mm.jpg" imageanchor="1" linkindex="120" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THJuh3JjkII/AAAAAAAABDE/b-rfNQZh-Mk/s320/1209-calcite-marrawah-9mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Natrolite is a colourless prismatic zeolite mineral that has a characteristic square cross-section. It's formula is Na&lt;sub&gt;2&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;10&lt;/sub&gt;.2H&lt;sub&gt;2&lt;/sub&gt;O.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen from Marrawah, Tasmania, has a small calcite crystal attached to one of the prisms. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-4925005230922079544?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4925005230922079544'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4925005230922079544'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/natrolite.html' title='⤱ Natrolite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THJuh3JjkII/AAAAAAAABDE/b-rfNQZh-Mk/s72-c/1209-calcite-marrawah-9mm.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3068550722051719292</id><published>2010-08-23T05:46:00.000-07:00</published><updated>2010-08-23T05:46:38.277-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='spessartine'/><category scheme='http://www.blogger.com/atom/ns#' term='kintore'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Spessartine ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THJtSlvIqTI/AAAAAAAABC8/IzjEIvPVkB4/s1600/1173-spessartine-kintore.jpg" imageanchor="1" linkindex="64" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THJtSlvIqTI/AAAAAAAABC8/IzjEIvPVkB4/s320/1173-spessartine-kintore.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Spessartine is one of the garnet group minerals and has a formula of Mn&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;(SiO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;. It is usually red or orange in colour, and occurs as transparent to translucent distinct crystals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen has formed as a sharp deep red crystal and is from the Kintore Open Cut, Broken Hill, New South Wales. Spessartine is common, even characteristic, at this locality.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3068550722051719292?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3068550722051719292'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3068550722051719292'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/spessartine_23.html' title='⤱ Spessartine ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THJtSlvIqTI/AAAAAAAABC8/IzjEIvPVkB4/s72-c/1173-spessartine-kintore.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6085503027955245455</id><published>2010-08-23T05:38:00.000-07:00</published><updated>2010-08-23T05:41:14.055-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='mesolite'/><category scheme='http://www.blogger.com/atom/ns#' term='lévyne'/><category scheme='http://www.blogger.com/atom/ns#' term='phillip island'/><category scheme='http://www.blogger.com/atom/ns#' term='sunderland bluff'/><title type='text'>⤱ Mesolite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/THJqVgPx9WI/AAAAAAAABC0/PMl1bBaBfXU/s1600/1146-mesolite-sunderlandbluff.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/THJqVgPx9WI/AAAAAAAABC0/PMl1bBaBfXU/s320/1146-mesolite-sunderlandbluff.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;Mesolite is a white fibrous zeolite mineral with a formula of Na&lt;sub&gt;2&lt;/sub&gt;Ca&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;9&lt;/sub&gt;Al&lt;sub&gt;6&lt;/sub&gt;O&lt;sub&gt;30&lt;/sub&gt;.8H&lt;sub&gt;2&lt;/sub&gt;0.&lt;br /&gt;&lt;br /&gt;This specimen has mesolite with minor lévyne infilling a cavity in basalt from Sunderland Bluff, south coast of Phillip Island, Victoria.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6085503027955245455?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6085503027955245455'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6085503027955245455'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/mesolite.html' title='⤱ Mesolite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/THJqVgPx9WI/AAAAAAAABC0/PMl1bBaBfXU/s72-c/1146-mesolite-sunderlandbluff.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-4282014560364677389</id><published>2010-08-23T05:23:00.000-07:00</published><updated>2010-08-23T05:23:21.536-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='browns prospect'/><category scheme='http://www.blogger.com/atom/ns#' term='rum jungle'/><category scheme='http://www.blogger.com/atom/ns#' term='pyromorphite'/><category scheme='http://www.blogger.com/atom/ns#' term='northern territory'/><title type='text'>⤱ Pyromorphite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THJnxgPWLeI/AAAAAAAABCs/lVnlxLcUfDk/s1600/1129-pyromorphite-brownsprospect.jpg" imageanchor="1" linkindex="19" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THJnxgPWLeI/AAAAAAAABCs/lVnlxLcUfDk/s320/1129-pyromorphite-brownsprospect.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Pyromorphite is a common secondary lead phosphate mineral that occurs in lead ore deposits. It's formula is Pb&lt;sub&gt;5&lt;/sub&gt;(PO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;Cl and it occurs generally as prismatic, sometimes tabular, green or brown hexagonal crystals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is an unusual branching group from Brown's Prospect, Rum Jungle, Northern Territory.&lt;br /&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-4282014560364677389?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4282014560364677389'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/4282014560364677389'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/pyromorphite_23.html' title='⤱ Pyromorphite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THJnxgPWLeI/AAAAAAAABCs/lVnlxLcUfDk/s72-c/1129-pyromorphite-brownsprospect.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6437437364241559521</id><published>2010-08-23T05:17:00.000-07:00</published><updated>2010-08-23T05:17:29.648-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='block 14'/><category scheme='http://www.blogger.com/atom/ns#' term='pyromorphite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Pyromorphite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THJlyYtHBlI/AAAAAAAABCk/aOxXYbKppLw/s1600/1125-pyromorphite-block14-2.jpg" imageanchor="1" linkindex="168" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THJlyYtHBlI/AAAAAAAABCk/aOxXYbKppLw/s320/1125-pyromorphite-block14-2.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Pyromorphite is a common secondary lead phosphate mineral that occurs in lead ore deposits. It's formula is Pb&lt;sub&gt;5&lt;/sub&gt;(PO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;Cl and it occurs generally as prismatic, sometimes tabular, green or brown hexagonal crystals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Block 14 Open Cut, Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6437437364241559521?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6437437364241559521'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6437437364241559521'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/pyromorphite.html' title='⤱ Pyromorphite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THJlyYtHBlI/AAAAAAAABCk/aOxXYbKppLw/s72-c/1125-pyromorphite-block14-2.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-1354820860248729519</id><published>2010-08-23T05:05:00.000-07:00</published><updated>2010-08-23T05:05:17.525-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='stolzite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Stolzite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THJi9k57RtI/AAAAAAAABCc/cTOC_UvRx7c/s1600/1108-stolzite-proprietary.jpg" imageanchor="1" linkindex="272" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THJi9k57RtI/AAAAAAAABCc/cTOC_UvRx7c/s320/1108-stolzite-proprietary.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;Stolzite is a lead tungstate mineral, formula Pb(WO4), and occurs as tabular or bipyramidal crystals that are commonly yellow, orange or red.&lt;br /&gt;&lt;br /&gt;This specimen is from Broken Hill, New South Wales, a locality well-known for excellent specimens in the earlier days of mining.&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-1354820860248729519?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1354820860248729519'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1354820860248729519'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/stolzite.html' title='⤱ Stolzite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THJi9k57RtI/AAAAAAAABCc/cTOC_UvRx7c/s72-c/1108-stolzite-proprietary.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-209469872848939776</id><published>2010-08-23T04:55:00.000-07:00</published><updated>2010-08-23T04:55:33.147-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='spessartine'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='löllingite'/><title type='text'>⤱ Löllingite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/THJel5tKH8I/AAAAAAAABCM/h7EIOaTj0UU/s1600/1107-lollingite-brokenhill-01.jpg" imageanchor="1" linkindex="34" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/THJel5tKH8I/AAAAAAAABCM/h7EIOaTj0UU/s320/1107-lollingite-brokenhill-01.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;span style="font-size: small;"&gt;Löllingite is an iron arsenic sulphide mineral that occurs as silver crystals or masses and can be easily confused with arsenopyrite. It's formula is FeAs&lt;sub&gt;2&lt;/sub&gt;.&lt;/span&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is embedded in the typical garnet sandstone from Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-209469872848939776?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/209469872848939776'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/209469872848939776'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/lollingite.html' title='⤱ Löllingite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/THJel5tKH8I/AAAAAAAABCM/h7EIOaTj0UU/s72-c/1107-lollingite-brokenhill-01.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6791461709499176825</id><published>2010-08-23T04:35:00.000-07:00</published><updated>2010-08-23T04:35:35.502-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='pyromorphite'/><category scheme='http://www.blogger.com/atom/ns#' term='kintore'/><category scheme='http://www.blogger.com/atom/ns#' term='sulphur'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='galena'/><title type='text'>⤱ Sulphur ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/THJbi-N3mSI/AAAAAAAABCE/5oAALtFZz6Q/s1600/1100-sulphur-kintore.jpg" imageanchor="1" linkindex="342" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/THJbi-N3mSI/AAAAAAAABCE/5oAALtFZz6Q/s320/1100-sulphur-kintore.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Sulphur is a native element, formula S, that normally occurs as transparent or translucent yellow crystals. It occurs in areas of active volcanism, particularly around fumeroles or volcanic vents, and in orebodies as a result of the breakdown of sulphide minerals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen has a tiny but very bright crystal of sulphur sitting alonside brown pyromorphite in cavities in galena. It is from the Kintore Open Cut, Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6791461709499176825?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6791461709499176825'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6791461709499176825'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/sulphur.html' title='⤱ Sulphur ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/THJbi-N3mSI/AAAAAAAABCE/5oAALtFZz6Q/s72-c/1100-sulphur-kintore.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3303255468642854742</id><published>2010-08-23T04:23:00.000-07:00</published><updated>2010-08-23T04:23:38.913-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='spessartine'/><category scheme='http://www.blogger.com/atom/ns#' term='kintore'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Spessartine ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/THJWXx7JbqI/AAAAAAAABB8/OJ18VUAinAU/s1600/1094-spessartine-kintore.jpg" imageanchor="1" linkindex="93" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/THJWXx7JbqI/AAAAAAAABB8/OJ18VUAinAU/s320/1094-spessartine-kintore.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Spessartine is one of the garnet group minerals and has a formula of Mn&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;(SiO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;3&lt;/sub&gt;. It is usually red or orange in colour, and occurs as transparent to translucent distinct crystals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen has formed as a rounded crystal and is from the Kintore Open Cut, Broken Hill, New South Wales. Spessartine is common, even characteristic, at this locality.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3303255468642854742?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3303255468642854742'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3303255468642854742'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/spessartine.html' title='⤱ Spessartine ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/THJWXx7JbqI/AAAAAAAABB8/OJ18VUAinAU/s72-c/1094-spessartine-kintore.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-8372849020586458835</id><published>2010-08-21T06:43:00.000-07:00</published><updated>2010-08-21T06:43:17.703-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='olympic dam'/><category scheme='http://www.blogger.com/atom/ns#' term='south australia'/><category scheme='http://www.blogger.com/atom/ns#' term='roxby downs'/><category scheme='http://www.blogger.com/atom/ns#' term='dolomite'/><category scheme='http://www.blogger.com/atom/ns#' term='hematite'/><title type='text'>⤱ Dolomite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/TG_W-xKb_VI/AAAAAAAABB0/hr3Rsli7Fy0/s1600/1080-dolomite-roxbydowns-01.jpg" imageanchor="1" linkindex="163" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/TG_W-xKb_VI/AAAAAAAABB0/hr3Rsli7Fy0/s320/1080-dolomite-roxbydowns-01.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Dolomite is a magnesium-bearing carbonate mineral, formula CaMg(CO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;, and often occurs as saddle-shaped crystals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen comes from the Olympic Dam deposit, Roxby Downs, South Australia, and there are small hemispheres of hematite present. &lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-8372849020586458835?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/8372849020586458835'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/8372849020586458835'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/dolomite.html' title='⤱ Dolomite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/TG_W-xKb_VI/AAAAAAAABB0/hr3Rsli7Fy0/s72-c/1080-dolomite-roxbydowns-01.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5699212343134611401</id><published>2010-08-21T06:34:00.000-07:00</published><updated>2010-08-21T06:34:35.640-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='oakleigh creek'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='fluorite'/><category scheme='http://www.blogger.com/atom/ns#' term='pelion mine'/><title type='text'>⤱ Fluorite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/TG_U8ESo5ZI/AAAAAAAABBs/vP1KokBVOTE/s1600/1069-fluorite-pelionmine-9mm.jpg" imageanchor="1" linkindex="19" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/TG_U8ESo5ZI/AAAAAAAABBs/vP1KokBVOTE/s320/1069-fluorite-pelionmine-9mm.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Fluorite is a halide, formula CaF&lt;sub&gt;2&lt;/sub&gt;, that occurs as cubic crystals, or more rarely as octahedral crystals.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the Pelion Mine, Oakleigh Creek, Tasmania, an area now included as part of the South West Wilderness area. The cube faces have been etched by geological processes.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5699212343134611401?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5699212343134611401'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5699212343134611401'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/fluorite.html' title='⤱ Fluorite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/TG_U8ESo5ZI/AAAAAAAABBs/vP1KokBVOTE/s72-c/1069-fluorite-pelionmine-9mm.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-2390934174335514058</id><published>2010-08-21T06:24:00.000-07:00</published><updated>2010-08-21T06:24:56.349-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='northern territory'/><category scheme='http://www.blogger.com/atom/ns#' term='harts range'/><category scheme='http://www.blogger.com/atom/ns#' term='albite'/><title type='text'>⤱ Albite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/TG_SngsXTMI/AAAAAAAABBk/I6Xy_eeLCek/s1600/1055-albite-hartsrange.jpg" imageanchor="1" linkindex="9" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/TG_SngsXTMI/AAAAAAAABBk/I6Xy_eeLCek/s320/1055-albite-hartsrange.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Albite is one of the feldspars with a formula of NaAlSi&lt;sub&gt;3&lt;/sub&gt;O&lt;sub&gt;8&lt;/sub&gt;. The "sunstone" variety, such as the one shown here from the Harts Range, Northern Territory, gets its name from the platelets inside the crystal.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-2390934174335514058?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2390934174335514058'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2390934174335514058'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/albite_21.html' title='⤱ Albite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/TG_SngsXTMI/AAAAAAAABBk/I6Xy_eeLCek/s72-c/1055-albite-hartsrange.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3535028083683418683</id><published>2010-08-21T06:16:00.000-07:00</published><updated>2010-08-21T06:16:33.164-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='gartrellite'/><category scheme='http://www.blogger.com/atom/ns#' term='western australia'/><category scheme='http://www.blogger.com/atom/ns#' term='ashburton downs'/><title type='text'>⤱ Gartrellite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/TG_QYbEufnI/AAAAAAAABBc/8-yJFidMDvU/s1600/1048-gartrellite-ashburtondowns-01.jpg" imageanchor="1" linkindex="137" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/TG_QYbEufnI/AAAAAAAABBc/8-yJFidMDvU/s320/1048-gartrellite-ashburtondowns-01.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Gartrellite is a lead copper iron arsenate mineral with a long formula - Pb(CuFeZn)&lt;sub&gt;2&lt;/sub&gt;[AsO&lt;sub&gt;4&lt;/sub&gt;,SO&lt;sub&gt;4&lt;/sub&gt;]&lt;sub&gt;2&lt;/sub&gt;.2(H&lt;sub&gt;2&lt;/sub&gt;O,OH). It usually occurs as earthy green masses such as this one from Ashburton Downs in Western Australia.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3535028083683418683?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3535028083683418683'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3535028083683418683'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/gartrellite.html' title='⤱ Gartrellite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/TG_QYbEufnI/AAAAAAAABBc/8-yJFidMDvU/s72-c/1048-gartrellite-ashburtondowns-01.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-831832696639799057</id><published>2010-08-21T06:06:00.000-07:00</published><updated>2010-08-21T06:06:07.579-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='bismuth'/><category scheme='http://www.blogger.com/atom/ns#' term='wolfram camp'/><category scheme='http://www.blogger.com/atom/ns#' term='queensland'/><category scheme='http://www.blogger.com/atom/ns#' term='bismuthinite'/><title type='text'>⤱ Bismuth ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/TG_OAPf8w0I/AAAAAAAABBU/ozKKAVb4mD8/s1600/1040-bismuth-wolframcamp.jpg" imageanchor="1" linkindex="314" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/TG_OAPf8w0I/AAAAAAAABBU/ozKKAVb4mD8/s320/1040-bismuth-wolframcamp.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;The element bismuth sometimes occurs as a whitish silver native metal, often tarnished (formula Bi), or may be a constituent of another mineral.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;In this specimen from Wolfram Camp in Queensland, native bismuth occurs with bismuthinite wires.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-831832696639799057?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/831832696639799057'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/831832696639799057'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/bismuth.html' title='⤱ Bismuth ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/TG_OAPf8w0I/AAAAAAAABBU/ozKKAVb4mD8/s72-c/1040-bismuth-wolframcamp.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-517541280774313670</id><published>2010-08-21T01:16:00.000-07:00</published><updated>2010-08-21T01:16:33.842-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='rosebery'/><category scheme='http://www.blogger.com/atom/ns#' term='alstonite'/><title type='text'>⤱ Alstonite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://www.crocoite.com/imagebrowser/ib_p021_1_1.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="240" src="http://www.crocoite.com/imagebrowser/ib_p021_1_1.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Alstonite, Rosebery, Tasmania.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-517541280774313670?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/517541280774313670'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/517541280774313670'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/alstonite.html' title='⤱ Alstonite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5746907551611238835</id><published>2010-08-21T01:13:00.000-07:00</published><updated>2010-08-21T01:13:32.239-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='feldspar'/><category scheme='http://www.blogger.com/atom/ns#' term='tulendeena'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='quartz'/><category scheme='http://www.blogger.com/atom/ns#' term='albite'/><title type='text'>⤱ Albite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://www.crocoite.com/imagebrowser/ib_p020_0_2.jpg" imageanchor="1" linkindex="17" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="240" src="http://www.crocoite.com/imagebrowser/ib_p020_0_2.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Albite with smoky quartz and feldspar, Tulendeena, Tasmania.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5746907551611238835?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5746907551611238835'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5746907551611238835'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/albite.html' title='⤱ Albite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-2009841315778901606</id><published>2010-08-21T01:10:00.000-07:00</published><updated>2010-08-24T05:13:38.668-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='agardite'/><category scheme='http://www.blogger.com/atom/ns#' term='south australia'/><category scheme='http://www.blogger.com/atom/ns#' term='dome rock'/><category scheme='http://www.blogger.com/atom/ns#' term='agardite-y'/><title type='text'>⤱ Agardite-(Y) ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://www.crocoite.com/imagebrowser/ib_p019_0_1.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="240" src="http://www.crocoite.com/imagebrowser/ib_p019_0_1.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Agardite-(Y) from Dome Rock, South Australia.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-2009841315778901606?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2009841315778901606'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/2009841315778901606'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/agardite-y.html' title='⤱ Agardite-(Y) ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-103232792334188942</id><published>2010-08-21T01:06:00.000-07:00</published><updated>2010-08-21T01:06:53.729-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='adamite'/><category scheme='http://www.blogger.com/atom/ns#' term='puttapa'/><category scheme='http://www.blogger.com/atom/ns#' term='south australia'/><title type='text'>⤱ Adamite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://www.crocoite.com/imagebrowser/ib_p018_1_2.jpg" imageanchor="1" linkindex="17" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="240" src="http://www.crocoite.com/imagebrowser/ib_p018_1_2.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Adamite from the Puttapa Zinc Deposit, South Australia.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-103232792334188942?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/103232792334188942'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/103232792334188942'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/adamite_21.html' title='⤱ Adamite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5544586616352510166</id><published>2010-08-21T01:05:00.000-07:00</published><updated>2010-08-21T01:05:14.804-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='adamite'/><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='kintore'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Adamite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://www.crocoite.com/imagebrowser/ib_p018_1_1.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="240" src="http://www.crocoite.com/imagebrowser/ib_p018_1_1.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Cuprian adamite from the Kintore Open Cut, Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5544586616352510166?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5544586616352510166'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5544586616352510166'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/adamite.html' title='⤱ Adamite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-8459848599674416001</id><published>2010-08-21T01:01:00.000-07:00</published><updated>2010-08-21T01:01:45.468-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='acanthite'/><category scheme='http://www.blogger.com/atom/ns#' term='magnet mine'/><title type='text'>⤱ Acanthite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://www.crocoite.com/imagebrowser/ib_p017_0_2.jpg" imageanchor="1" linkindex="19" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="240" src="http://www.crocoite.com/imagebrowser/ib_p017_0_2.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Acanthite from the Magnet Mine near Waratah, Tasmania. Photo width 2mm. Brian Carney specimen.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-8459848599674416001?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/8459848599674416001'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/8459848599674416001'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/acanthite_21.html' title='⤱ Acanthite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5281995251827266146</id><published>2010-08-21T00:59:00.000-07:00</published><updated>2010-08-21T00:59:39.592-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='minium'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='acanthite'/><title type='text'>⤱ Acanthite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://www.crocoite.com/imagebrowser/ib_p017_0_1.jpg" imageanchor="1" linkindex="20" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" height="240" src="http://www.crocoite.com/imagebrowser/ib_p017_0_1.jpg" width="320" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Acanthite on minium from Broken Hill, New South Wales. Photo width 2mm.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5281995251827266146?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5281995251827266146'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5281995251827266146'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/acanthite.html' title='⤱ Acanthite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6786786111114343152</id><published>2010-08-20T22:51:00.000-07:00</published><updated>2010-08-20T22:51:57.904-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='glendonite'/><category scheme='http://www.blogger.com/atom/ns#' term='calcite'/><category scheme='http://www.blogger.com/atom/ns#' term='hunter valley'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><category scheme='http://www.blogger.com/atom/ns#' term='ikaite'/><title type='text'>⤱ Glendonite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/TG9nxAHn7lI/AAAAAAAABBM/wscIon7jiho/s1600/glendonite-huntervalley.jpg" imageanchor="1" linkindex="82" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/TG9nxAHn7lI/AAAAAAAABBM/wscIon7jiho/s320/glendonite-huntervalley.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Glendonites are a pseudomorph of calcite, formula CaCO&lt;sub&gt;3&lt;/sub&gt;, after the mineral ikaite, formula CaCO&lt;sub&gt;3&lt;/sub&gt;.6H&lt;sub&gt;2&lt;/sub&gt;O. They are thought to have formed in glacial conditions. More information on glendonites can be found &lt;a href="http://www.glendonite.com/" linkindex="83"&gt;here&lt;/a&gt;.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a particularly large specimen (albeit repaired) from the Hunter Valley in New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6786786111114343152?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6786786111114343152'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6786786111114343152'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/glendonite.html' title='⤱ Glendonite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/TG9nxAHn7lI/AAAAAAAABBM/wscIon7jiho/s72-c/glendonite-huntervalley.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7983671140058139445</id><published>2010-08-20T22:43:00.000-07:00</published><updated>2010-08-20T22:44:03.351-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='coulsellite'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='mt cleveland'/><category scheme='http://www.blogger.com/atom/ns#' term='luina'/><title type='text'>⤱ Coulsellite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/TG9mNC6BGgI/AAAAAAAABBE/D6NWjbXGZQY/s1600/coulsellite-luina.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/TG9mNC6BGgI/AAAAAAAABBE/D6NWjbXGZQY/s320/coulsellite-luina.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Coulsellite is a newly-described halide, previously known as calcian ralstonite. It has a formula of CaNa&lt;sub&gt;3&lt;/sub&gt;AlMg&lt;sub&gt;3&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt; and was named after the late Victorian mineral collector, Ruth Coulsell.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from the type locality, the Mt Cleveland Mine, Luina, Tasmania.&lt;/div&gt;&lt;table class="ft2"&gt;&lt;tbody&gt;  &lt;/tbody&gt;&lt;/table&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7983671140058139445?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7983671140058139445'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7983671140058139445'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/coulsellite.html' title='⤱ Coulsellite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/TG9mNC6BGgI/AAAAAAAABBE/D6NWjbXGZQY/s72-c/coulsellite-luina.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-6408897807792075924</id><published>2010-08-20T22:36:00.000-07:00</published><updated>2010-08-20T22:36:49.950-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='chlorargyrite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Chlorargyrite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/TG9ks_HZmiI/AAAAAAAABA8/tzltf_D_rYY/s1600/chlorargyrite-brokenhill.jpg" imageanchor="1" linkindex="219" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/TG9ks_HZmiI/AAAAAAAABA8/tzltf_D_rYY/s320/chlorargyrite-brokenhill.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Chlorargyrite is a silver halide, formula AgCl, that occurs as cubes, or modified cubes, in the gossans of silver-lead orebodies. Specimens such as this one are often called embolite, or more correctly, bromian chlorargyrite, Ag(ClBr). Chlorargyrite, as with many silver-bearing minerals, is affected by light.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is from Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-6408897807792075924?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6408897807792075924'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/6408897807792075924'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/chlorargyrite.html' title='⤱ Chlorargyrite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/TG9ks_HZmiI/AAAAAAAABA8/tzltf_D_rYY/s72-c/chlorargyrite-brokenhill.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3953937632191685260</id><published>2010-08-20T21:58:00.000-07:00</published><updated>2010-08-20T21:58:05.413-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='crocoite'/><category scheme='http://www.blogger.com/atom/ns#' term='adelaide mine'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='hisingerite'/><category scheme='http://www.blogger.com/atom/ns#' term='dundas'/><category scheme='http://www.blogger.com/atom/ns#' term='gibbsite'/><category scheme='http://www.blogger.com/atom/ns#' term='coronadite'/><title type='text'>⤱ Crocoite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/TG9XLVDxTPI/AAAAAAAABA0/XkbRT9YArvs/s1600/blackcrocoite-dundas.jpg" imageanchor="1" linkindex="105" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/TG9XLVDxTPI/AAAAAAAABA0/XkbRT9YArvs/s320/blackcrocoite-dundas.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Crocoite is a red to orange lead chromate, formula PB(CrO&lt;sub&gt;4&lt;/sub&gt;), and occurs generally as thin prismatic interlocking crystals. The Dundas region of Tasmania is a world-famous locality for crocoite.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This specimen is coated by a number of black minerals that are apparently made up of a banded mixture of coronadite, gibbsite and manganoan hisingerite, replacing the crocoite, and comes from the Adelaide Mine, Dundas, Tasmania.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3953937632191685260?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3953937632191685260'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3953937632191685260'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/crocoite.html' title='⤱ Crocoite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/TG9XLVDxTPI/AAAAAAAABA0/XkbRT9YArvs/s72-c/blackcrocoite-dundas.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-1060013571922542248</id><published>2010-08-20T21:32:00.000-07:00</published><updated>2010-08-20T21:33:04.466-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='tabba tabba'/><category scheme='http://www.blogger.com/atom/ns#' term='western australia'/><category scheme='http://www.blogger.com/atom/ns#' term='beryl'/><title type='text'>⤱ Beryl ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/TG9VUNl6q5I/AAAAAAAABAs/6KcV8OV91XU/s1600/beryl-tabbatabba.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/TG9VUNl6q5I/AAAAAAAABAs/6KcV8OV91XU/s320/beryl-tabbatabba.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Beryl is a beryllium silicate, formula Be&lt;sub&gt;3&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;6&lt;/sub&gt;O&lt;sub&gt;18&lt;/sub&gt;, and provides us with a number of gem varieties such as emerald (green), aquamarine (blue) and morganite (pink). It often occurs as prismatic crystals embedded in the surrounding matrix and can be difficult to extract without damage.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a specimen of opaque white beryl from the Tabba Tabba pegmatite in Western Australia.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-1060013571922542248?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1060013571922542248'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/1060013571922542248'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/beryl.html' title='⤱ Beryl ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/TG9VUNl6q5I/AAAAAAAABAs/6KcV8OV91XU/s72-c/beryl-tabbatabba.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-7731233317429886821</id><published>2010-08-20T21:23:00.000-07:00</published><updated>2010-08-20T21:34:20.637-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='broken hill'/><category scheme='http://www.blogger.com/atom/ns#' term='barite'/><category scheme='http://www.blogger.com/atom/ns#' term='new south wales'/><title type='text'>⤱ Barite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/TG9UGENxa9I/AAAAAAAABAk/Pd1ab6RfQFg/s1600/barite-brokenhill.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/TG9UGENxa9I/AAAAAAAABAk/Pd1ab6RfQFg/s320/barite-brokenhill.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Barite, also spelled baryte, is a barium sulphate mineral with a formula BaSO&lt;sub&gt;4&lt;/sub&gt;. &lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a nice specimen of orange bladed barite from Broken Hill, New South Wales.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-7731233317429886821?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7731233317429886821'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/7731233317429886821'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/barite.html' title='⤱ Barite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/TG9UGENxa9I/AAAAAAAABAk/Pd1ab6RfQFg/s72-c/barite-brokenhill.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-5885942552666725598</id><published>2010-08-19T06:01:00.000-07:00</published><updated>2010-08-20T21:32:49.893-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='lake boga'/><category scheme='http://www.blogger.com/atom/ns#' term='anatase'/><category scheme='http://www.blogger.com/atom/ns#' term='muscovite'/><title type='text'>⤱ Anatase ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://1.bp.blogspot.com/_q-eiBrUv--k/TG0nOa6gQPI/AAAAAAAABAI/7CigzzzB3zw/s1600/anatase-lakeboga.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://1.bp.blogspot.com/_q-eiBrUv--k/TG0nOa6gQPI/AAAAAAAABAI/7CigzzzB3zw/s320/anatase-lakeboga.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Anatase is one of three naturally occurring forms of titanium oxide - TiO&lt;sub&gt;2&lt;/sub&gt;, the others being rutile and brookite. It often occurs as bipyramidal crystals that may be blue, black, or other colours.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a photo of a single anatase crystal with muscovite mica in a miarolitic cavity, image width about 4mm.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-5885942552666725598?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5885942552666725598'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/5885942552666725598'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/anatase.html' title='⤱ Anatase ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_q-eiBrUv--k/TG0nOa6gQPI/AAAAAAAABAI/7CigzzzB3zw/s72-c/anatase-lakeboga.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3774984949055202531</id><published>2010-08-19T05:37:00.000-07:00</published><updated>2010-08-21T03:42:48.711-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='mt bischoff'/><category scheme='http://www.blogger.com/atom/ns#' term='tasmania'/><category scheme='http://www.blogger.com/atom/ns#' term='fluorite'/><category scheme='http://www.blogger.com/atom/ns#' term='vivianite'/><title type='text'>⤱ Vivianite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://3.bp.blogspot.com/_q-eiBrUv--k/TG0mYhM9miI/AAAAAAAABAA/dAOFYVI0jdk/s1600/vivianite-mtbischoff.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://3.bp.blogspot.com/_q-eiBrUv--k/TG0mYhM9miI/AAAAAAAABAA/dAOFYVI0jdk/s320/vivianite-mtbischoff.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Vivianite is an iron phosphate mineral that can be found as earthy masses as well as blue or green crystals. Its formula is Fe&lt;sub&gt;3&lt;/sub&gt;(PO&lt;sub&gt;4&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;.8H&lt;sub&gt;2&lt;/sub&gt;O.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a vivianite on fluorite specimen from the Mt Bischoff Mine, Waratah, Tasmania, and the crystal group is about 6 or 7mm across.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3774984949055202531?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3774984949055202531'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3774984949055202531'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/vivianite.html' title='⤱ Vivianite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_q-eiBrUv--k/TG0mYhM9miI/AAAAAAAABAA/dAOFYVI0jdk/s72-c/vivianite-mtbischoff.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3745310186234069486</id><published>2010-08-19T05:02:00.000-07:00</published><updated>2010-08-19T05:58:20.854-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='western australia'/><category scheme='http://www.blogger.com/atom/ns#' term='wulfenite'/><category scheme='http://www.blogger.com/atom/ns#' term='whim creek'/><title type='text'>⤱ Wulfenite ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: center;"&gt;&lt;a href="http://4.bp.blogspot.com/_q-eiBrUv--k/TG0dNvZKTJI/AAAAAAAAA_4/tF7LbdizuWs/s1600/wulfenite-whimcreek.jpg" imageanchor="1" linkindex="16" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://4.bp.blogspot.com/_q-eiBrUv--k/TG0dNvZKTJI/AAAAAAAAA_4/tF7LbdizuWs/s320/wulfenite-whimcreek.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Wulfenite is a lead molybdate mineral with a formula of Pb(MoO&lt;span style="font-family: &amp;quot;Calibri&amp;quot;,&amp;quot;sans-serif&amp;quot;; font-size: 11pt; line-height: 115%;"&gt;&lt;sub&gt;4&lt;/sub&gt;&lt;/span&gt;). It occurs generally as tabular or bipyramidal crystals that may be yellow, red, colourless, even blue.&lt;/div&gt;&lt;div style="text-align: justify;"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;This is a nice yellow wulfenite from the now-closed locality of Whim Creek in Western Australia. The crystal is approximately 1.2mm across.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3745310186234069486?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3745310186234069486'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3745310186234069486'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/wulfenite.html' title='⤱ Wulfenite ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_q-eiBrUv--k/TG0dNvZKTJI/AAAAAAAAA_4/tF7LbdizuWs/s72-c/wulfenite-whimcreek.jpg' height='72' width='72'/></entry><entry><id>tag:blogger.com,1999:blog-5614200336220321753.post-3634247381944252861</id><published>2010-08-19T04:44:00.000-07:00</published><updated>2010-08-19T05:56:39.117-07:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='victoria'/><category scheme='http://www.blogger.com/atom/ns#' term='analcime'/><category scheme='http://www.blogger.com/atom/ns#' term='flinders'/><title type='text'>⤱ Analcime ⤱</title><content type='html'>&lt;div class="separator" style="clear: both; text-align: justify;"&gt;&lt;a href="http://2.bp.blogspot.com/_q-eiBrUv--k/TG0KXyq7KKI/AAAAAAAAA_w/J1B-OTCl84M/s1600/analcime-flinders.jpg" imageanchor="1" linkindex="134" style="clear: left; float: left; margin-bottom: 1em; margin-right: 1em;"&gt;&lt;img border="0" src="http://2.bp.blogspot.com/_q-eiBrUv--k/TG0KXyq7KKI/AAAAAAAAA_w/J1B-OTCl84M/s320/analcime-flinders.jpg" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div style="text-align: justify;"&gt;Analcime (sometimes known as 'analcite') is a common member of the zeolite group of minerals with a formula of Na&lt;sub&gt;2&lt;/sub&gt;Al&lt;sub&gt;2&lt;/sub&gt;Si&lt;sub&gt;4&lt;/sub&gt;O&lt;sub&gt;12&lt;/sub&gt;.2H&lt;sub&gt;2&lt;/sub&gt;O&lt;span style="font-family: &amp;quot;Calibri&amp;quot;,&amp;quot;sans-serif&amp;quot;; font-size: 11pt; line-height: 115%;"&gt;&lt;/span&gt; and occurs as colourless trapezohedral crystals in cavities in volcanic basalt rocks. Often, these crystals 'craze' and turn white after being exposed. Crystals may also appear to be the same colour as the underlying matrix, they are so transparent.&lt;br /&gt;&lt;br /&gt;This particular specimen is from Cairns Bay, Flinders, Victoria.&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/5614200336220321753-3634247381944252861?l=mineral-spot.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3634247381944252861'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/5614200336220321753/posts/default/3634247381944252861'/><link rel='alternate' type='text/html' href='http://mineral-spot.blogspot.com/2010/08/analcime.html' title='⤱ Analcime ⤱'/><author><name>crocoite</name><uri>http://www.blogger.com/profile/13085042174191275031</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='31' height='32' src='http://www.crocoite.com/blogspot/me.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_q-eiBrUv--k/TG0KXyq7KKI/AAAAAAAAA_w/J1B-OTCl84M/s72-c/analcime-flinders.jpg' height='72' width='72'/></entry></feed>
