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<channel>
	<title>Mineralogy</title>
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	<link>http://www.mineralogy.com</link>
	<description></description>
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		<title>Internship Information</title>
		<link>http://www.mineralogy.com/2010/09/internship-information/</link>
		<comments>http://www.mineralogy.com/2010/09/internship-information/#comments</comments>
		<pubDate>Sun, 05 Sep 2010 09:44:59 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[Jobs]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=662</guid>
		<description><![CDATA[Each semester, the faculty, staff, and students of the Georgia Museum of Natural History welcome undergraduates as Natural History Interns to enjoy a hands-on course with the Museum. Interns receive supervised experience working directly with the faculty, staff, and other students curating one of the natural history collections affiliated with the Georgia Museum of Natural [...]]]></description>
			<content:encoded><![CDATA[<p>Each semester, the faculty, staff, and students of the Georgia Museum of Natural History welcome undergraduates as Natural History Interns to enjoy a hands-on course with the Museum. Interns receive supervised experience working directly with the faculty, staff, and other students curating one of the natural history collections affiliated with the Georgia Museum of Natural History or with education and outreach programs.</p>
<p>The course objective is for Interns to learn about museums of natural history and natural history collections by working closely with collection staff collecting, accessioning, preparing, cataloging, and curating natural history collections or with education staff interpretating natural history to the public. Students will practice techniques and methods for curating materials in one or more collections under the direction of collection personnel. Routine curatorial practices such as identification and preparation of specimens and data management will be part of the Internship. In addition, Interns may participate in tours, outreach presentations at area schools, special events, preparation of displays, and occasional weekend field trips.</p>
<p>For further information please visit <a title="Internship Information" href="http://museum.nhm.uga.edu/index.php?page=content/academics/internship" target="_blank">http://museum.nhm.uga.edu/</a></p>
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		<title>Gem &amp; Mineral Council Coordinator</title>
		<link>http://www.mineralogy.com/2010/09/gem-mineral-council-coordinator/</link>
		<comments>http://www.mineralogy.com/2010/09/gem-mineral-council-coordinator/#comments</comments>
		<pubDate>Sat, 04 Sep 2010 12:07:41 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[Jobs]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=653</guid>
		<description><![CDATA[The Natural History Museum of Los Angeles County seeks a Gem &#38; Mineral Council Coordinator to work with our Research and Collections department. The Gem &#38; Mineral Council Coordinator handles day-to-day operations of The Gem &#38; Mineral Council including implementing, facilitating, and following-up on Council projects and activities prescribed by The Gem &#38; Mineral Council [...]]]></description>
			<content:encoded><![CDATA[<p>The Natural History Museum of Los Angeles County seeks a Gem &amp; Mineral Council Coordinator to work with our Research and Collections department. The Gem &amp; Mineral Council Coordinator handles day-to-day operations of The Gem &amp; Mineral Council including implementing, facilitating, and following-up on Council projects and activities prescribed by The Gem &amp; Mineral Council Board of Directors and the Mineral Science Curator. Primary responsibilities include but are not limited to working on the planning and staging of all Council activities (meetings, events, programs, field trips, etc.) including tracking, scheduling and deadlines, preparing memos and work orders, reserving venues, arranging for catering equipment and support personnel, preparing and mailing program flyers, newsletter, roster, minutes, agendas, etc., and taking reservations.</p>
<p>For further information please visit <a title="Jobs at NHM" href="http://www.nhm.org/site/about-our-museums/working-at-nhm/jobs-nhm" target="_blank">http://www.nhm.org</a></p>
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		<title>American Manganese Inc</title>
		<link>http://www.mineralogy.com/2010/09/american-manganese-inc/</link>
		<comments>http://www.mineralogy.com/2010/09/american-manganese-inc/#comments</comments>
		<pubDate>Thu, 02 Sep 2010 20:40:58 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[drilling program]]></category>
		<category><![CDATA[manganese]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=646</guid>
		<description><![CDATA[Mr. Larry W. Reaugh, President and Chief Executive Officer of American Manganese Inc.(“American Manganese” or the “Company”), (TSX.V:  AMY; Pink Sheets:  AMYZF), is pleased to announce the Company has received results from its on going Artillery Peak drilling program for drill hole numbers 49 – 53 located on the South Maggie zone of the Manganese Mesa [...]]]></description>
			<content:encoded><![CDATA[<p><strong>Mr. Larry W. Reaugh</strong>, President and Chief Executive Officer of <strong>American Manganese Inc.</strong>(“American Manganese” or the “Company”), (TSX.V:  AMY; Pink Sheets:  AMYZF), is pleased to announce the Company has received results from its on going Artillery Peak drilling program for drill hole numbers 49 – 53 located on the South Maggie zone of the Manganese Mesa from its on going Artillery Peak drilling program.  Results for drill holes 1 through 48 have been announced previously.</p>
<p>“The Artillery Peak manganese mineralization is located within basin filling alluvial fan/playa deposit which typically exhibit large thickness and lateral continuity” says Mr. Reaugh.  He goes on to say:  “According to the US Geological Survey, Bulletin 961, the bedded deposits of the Chapin Wash formation have the potential for hosting immense tonnage of prospective manganese mineralization.  The success of this drilling program demonstrates that character and continuity.”</p>
<div class="wp-caption aligncenter" style="width: 410px"><a rel="http://www.americanmanganeseinc.com/wp-content/uploads/2010/07/7-21-2010-3-11-58-PM.jpg" href="http://www.americanmanganeseinc.com/wp-content/uploads/2010/07/7-21-2010-3-11-58-PM.jpg" target="_blank"><img class="     " title="drill plan " src="http://www.americanmanganeseinc.com/wp-content/uploads/2010/07/7-21-2010-3-11-58-PM.jpg" alt="" width="400" height="286" /></a><p class="wp-caption-text">www.americanmanganeseinc.com</p></div>
<p>For further information please visit <a href="http://www.americanmanganeseinc.com/">http://www.americanmanganeseinc.com</a></p>
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		<title>The Summit Mine</title>
		<link>http://www.mineralogy.com/2010/08/the-summit-mine-4/</link>
		<comments>http://www.mineralogy.com/2010/08/the-summit-mine-4/#comments</comments>
		<pubDate>Sun, 29 Aug 2010 08:39:16 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[Mines]]></category>
		<category><![CDATA[hemimorphite]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=638</guid>
		<description><![CDATA[The Summit Mine Source of the finest hemimorphite specimens in the United States © Copyright 2005-2010 Chris Tucker All rights reserved. www.christuckerminerals.com The Minerals Descloizite Descloizite occurs throughout the mine and is locally plentiful.  The crystals are generally sharp and vary in color from red to green to black, larger crystals tend to be distorted. Sharp rosettes [...]]]></description>
			<content:encoded><![CDATA[<h2 style="text-align: center;">The Summit Mine</h2>
<h3 style="text-align: center;">Source of the finest hemimorphite specimens in the United States</h3>
<p style="text-align: center;">© Copyright 2005-2010 <a href="mailto:chris@christuckerminerals.com">Chris Tucker</a> All rights reserved.</p>
<p style="text-align: center;"><a href="http://www.christuckerminerals.com/">www.christuckerminerals.com</a></p>
<p style="text-align: center;">The Minerals</p>
<p style="text-align: center;">
<p style="text-align: center;"><strong>Descloizite</strong><br />
Descloizite occurs throughout the mine and is locally plentiful.  The crystals are generally sharp and vary in color from red to green to black, larger crystals tend to be distorted.</p>
<p style="text-align: center;">Sharp rosettes of blood-red descloizite make striking specimens.</p>
<p style="text-align: center;">
<div class="wp-caption aligncenter" style="width: 360px"><img class=" " title="Descloizite crystals, the largest is 2mm long." src="http://www.christuckerminerals.com/mine%20summit%20descloizite.jpg" alt="" width="350" height="357" /><p class="wp-caption-text">© Copyright 2005-2010 Chris Tucker - All Rights Reserved  www.christuckerminerals.com</p></div>
<div class="wp-caption aligncenter" style="width: 360px"><img class=" " title="Descloizite, 9 cm across." src="http://www.christuckerminerals.com/mine%20summit%20descloizite2.jpg" alt="" width="350" height="319" /><p class="wp-caption-text">© Copyright 2005-2010 Chris Tucker - All Rights Reserved  www.christuckerminerals.com</p></div>
<p style="text-align: center;"><strong>Fluorite</strong><br />
Fluorite is rarely found and is one of the earliest minerals to have formed and is always massive.  In the back of one small stope several tons of massive purple fluorite occurs with secondary copper minerals.</p>
<p style="text-align: center;"><span id="more-638"></span></p>
<p style="text-align: center;"><strong>Galena</strong><br />
Galena has been found as residual pieces and occasionally forms the matrix for secondary lead minerals.</p>
<p style="text-align: center;"><strong>Gold</strong><br />
Historic documents report a small quantity of gold being present in the ore.  Likely, if a sizable ore sample was to be crushed and panned, free gold would be obtained.</p>
<p>To be continued&#8230; Part 2: The Minerals</p>
<p>Courtesy: Mr. Chris Tucker</p>
<p>All text, images, and design © Copyright 2005-2010 <a href="mailto:chris@christuckerminerals.com">Chris Tucker</a> All rights reserved.</p>
<p><a href="http://www.christuckerminerals.com/">http://www.christuckerminerals.com</a></p>
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		<title>Imperial Metals Corporation</title>
		<link>http://www.mineralogy.com/2010/08/imperial-metals-corporation/</link>
		<comments>http://www.mineralogy.com/2010/08/imperial-metals-corporation/#comments</comments>
		<pubDate>Mon, 23 Aug 2010 16:32:27 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[metals]]></category>
		<category><![CDATA[gold]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=628</guid>
		<description><![CDATA[Red Chris Exploration Program Continues to Expand Deep Deposit Vancouver, BC &#8211; August 5, 2010 - Imperial Metals Corporation (TSX:III) reports assay results from ongoing exploration drilling at its Red Chris property. Results from drill hole RC10-393 include 317.5 metres grading 1.08% copper, 1.46 g/t gold and 4.28 g/t silver within a 1,112.5 metre mineralized section [...]]]></description>
			<content:encoded><![CDATA[<p><strong><big>Red Chris Exploration Program Continues to Expand Deep Deposit</big></strong></p>
<p>Vancouver, BC &#8211; August 5, 2010 -<span style="color: #000000;"> </span><span style="color: #333333;">Imperial</span><span style="color: #333333;"> </span><span style="color: #333333;">Metals</span><span style="color: #333333;"> </span><span style="color: #333333;">Corporation</span> (TSX:III) reports assay results from ongoing exploration drilling at its Red Chris property. Results from drill hole RC10-393 include 317.5 metres grading 1.08% copper, 1.46 g/t gold and 4.28 g/t silver within a 1,112.5 metre mineralized section grading 0.54% copper, 0.61 g/t gold and 1.96 g/t silver. This is one of the longest mineralized intercepts obtained to date at Red Chris. RC10-388, one of the first holes in the deep Main zone since 2007, tested the western edge of the known Main zone and intersected five intervals of copper/gold mineralization including 380.0 metres grading 0.34% copper and 0.50 g/t gold.<br />
Final results from RC10-360* have extended the length of the previously reported high grade interval to 671.2 metres grading 1.03% copper and 1.65 g/t gold. This intercept strengthens confidence in high grade mineralization observed to the west in RC07-338 and to the east in RC09-350. More drilling will be required to fully define the geometry of the high gold to copper ratio mineralization in this area. (*partial results were released April 12, 2010)</p>
<p><span id="more-628"></span></p>
<p>The East zone mineralization has been extended with RC10-375 intersecting 861.7 metres grading 0.41% copper and 0.38 g/t gold including a 302.5 metre section grading 0.56% copper and 0.54 g/t gold. This step out is the most easterly deep drill hole in the East zone. Mineralization at depth in this area is still open to the east. Also drilled in the East zone, RC10-391, located 125 metres northeast of RC10-393, returned 1,002.5 metres grading 0.50% copper and 0.38 g/t gold while nearby RC10-393 returned 1,107.5 metres grading 0.54% copper and 0.61 g/t gold. RC10-391 and 393 were drilled in an area to the east of RC07-335 where previous attempts to drill deep had been unsuccessful.</p>
<p>for further information please visit <a title="imperial metals" href="http://www.imperialmetals.com/s/News-2010.asp?ReportID=413243&amp;_Type=&amp;_Title=Red-Chris-Exploration-Program-Continues-to-Expand-Deep-Deposit" target="_blank">http://www.imperialmetals.com</a></p>
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		<title>University of Western Ontario</title>
		<link>http://www.mineralogy.com/2010/08/university-of-western-ontario/</link>
		<comments>http://www.mineralogy.com/2010/08/university-of-western-ontario/#comments</comments>
		<pubDate>Sun, 22 Aug 2010 12:47:10 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[Jobs]]></category>
		<category><![CDATA[jobs]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=624</guid>
		<description><![CDATA[Dr. Roberta Flemming at the Department of Earth Sciences at University of Western Ontario has openings for M.Sc. or Ph.D. candidates interested in pursuing fundamental or applied studies of minerals in the following areas: Fundamental understanding and quantification of mineral behavior as a function of pressure (P), temperature (T) and composition (X). Projects involve mineral [...]]]></description>
			<content:encoded><![CDATA[<p><a id="aptureLink_crYJzLFwlQ" style="margin-top: 0px; margin-right: auto; margin-bottom: 0px; margin-left: auto; text-align: center; display: block; padding-top: 0px; padding-right: 6px; padding-bottom: 0px; padding-left: 6px;" href="http://www.flickr.com/photos/criminalintent/2508784649/"><img style="border: 0px initial initial;" title="University of Western Ontario 1991" src="http://static.flickr.com/2252/2508784649_616d7a79e2.jpg" alt="" width="350" height="228" /></a></p>
<p>Dr. Roberta Flemming at the Department of Earth Sciences at University of Western Ontario has openings for M.Sc. or Ph.D. candidates interested in pursuing fundamental or applied studies of minerals in the following areas:</p>
<ol>
<li>Fundamental understanding and quantification of mineral behavior as a function of pressure (P), temperature (T) and composition (X). Projects involve mineral synthesis (at controlled P-T), and determination of crystal structure (by X-ray diffraction/Rietveld refinement), crystal chemistry (by EPMA), and cation order-disorder (by Nuclear Magnetic Resonance (NMR) spectroscopy (e.g. 29 Si NMR provides a measure of Si/Al order in aluminosilicates). These data have application in geothermobarometry.<span id="more-624"></span></li>
</ol>
<ol>
<li>Systematic investigation of Kimberlite Indicator Minerals (KIM) (e.g. chromite, Cr-diopside). Variation in unit cell parameters (measured by µXRD) is correlated to geochemical data (by EPMA), on a grain-by-grain basis, with the aim of developing µXRD as a tool for diamond exploration. Inclusions and strain, observed by µXRD, give additional clues to origin.</li>
<li>Systematic mineralogical investigation of meteorites. In situ µXRD provides rapid mineral ID for meteorite classification, as well as unit cell parameters for addition to our growing database of unit cell parameters for meteorite minerals. Unit cell parameters can be correlated to geochemical information, and in some cases (e.g. clinopyroxene and olivine in basaltic meteorites) this may be correlated to planetary origin. Rietveld refinement of powder XRD data provides modal mineral analysis of bulk sample, and enables crystal structural study of selected phases.</li>
<li>Development of micro X-ray diffraction (µXRD) as a tool for geologists. Micro XRD provides a unique opportunity to correlate crystal structural information with other microanalytical data on the microscopic scale (50-500 µm) not previously available routinely. Furthermore, minerals can be examined in situ, preserving orientational information. Projects include:
<ol>
<li>Quantification of strain-related mosaicity in minerals in meteorites, impact structures, and other rocks, with an aim toward development of a µXRD strain index and calibration using existing strain indices.</li>
<li>Development of µXRD for exsolution geothermometry. (e.g. two pyroxenes). GADDS image provides simultaneous unit cell information for both phases, as well as their T-dependent orientational relationship.</li>
</ol>
</li>
</ol>
<p>Facilities at UWO include a Bruker D8 Discover micro X-ray diffractometer, High-T and High-P laboratories, EPMA, SEM, FTIR, Raman, and XRF facilities (Earth Sciences), 400 and 600 MHz solid-state NMRs (Chemistry), XPS and SIMS facilities (Surface Science Western).</p>
<p>If you wish to obtain more information about these projects, or other possible projects, please contact <a href="http://www.uwo.ca/earth/people/faculty/flemming.html">Dr. Roberta Flemming</a> (519-661-3143, <a href="mailto:rflemmin@uwo.ca">rflemmin@uwo.ca</a>). Collaborative projects with other faculty are also possible. Research and teaching assistantships are guaranteed for all qualified students.</p>
<p>for further information please visit <a title="Western Ontario" href="http://www.uwo.ca/earth/graduate/StudentOpportunities.html" target="_blank">http://www.uwo.ca</a></p>
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		<title>Canada Lithium Corp.</title>
		<link>http://www.mineralogy.com/2010/08/canada-lithium-corp/</link>
		<comments>http://www.mineralogy.com/2010/08/canada-lithium-corp/#comments</comments>
		<pubDate>Sat, 21 Aug 2010 17:46:28 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[metals]]></category>
		<category><![CDATA[Lithium]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=610</guid>
		<description><![CDATA[Canada Lithium Corp. Project Update; Drilling Intersects 66.3 Metres Grading 1.29% Li2O Toronto, July 5, 2010 &#8212; Canada Lithium Corp. (TSX: CLQ; U.S. OTCQX: CLQMF) announced today that the major components of the definitive Feasibility Study (FS) for the re-development of the Quebec Lithium mine are now under way and on schedule for completion in [...]]]></description>
			<content:encoded><![CDATA[<p><strong><big>Canada Lithium Corp. Project Update; Drilling Intersects 66.3 Metres Grading 1.29% Li<sub>2</sub>O</big></strong></p>
<p>Toronto, July 5, 2010 &#8212; Canada Lithium Corp. (TSX: CLQ; U.S. OTCQX: CLQMF) announced today that the major components of the definitive Feasibility Study (FS) for the re-development of the Quebec Lithium mine are now under way and on schedule for completion in the First Quarter 2011.</p>
<p>The major components of the FS are as follows:</p>
<p>Resource Drilling Program:<br />
The program, aimed primarily at testing extensions of the known resource both at depth and along strike, also includes some infill drilling for increased resource definition within the initial pit design. The program was initiated in late April and 49 holes totalling 6,724 meters have been completed to date. The assay results for the program will be completed by August 2010 and an updated NI-43-101 resource report will be available in October 2010.</p>
<p>Some highlights of the assay results received to date are as follows: <a title="canadalithium" href="http://www.canadalithium.com/s/NewsReleases.asp?ReportID=409021&amp;_Type=News-Releases&amp;_Title=Canada-Lithium-Corp.-Project-Update-Drilling-Intersects-66.3-Metres-Grading..." target="_blank">http://www.canadalithium.com/</a></p>
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		<title>The Summit Mine</title>
		<link>http://www.mineralogy.com/2010/08/the-summit-mine-3/</link>
		<comments>http://www.mineralogy.com/2010/08/the-summit-mine-3/#comments</comments>
		<pubDate>Fri, 20 Aug 2010 09:09:58 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[Mines]]></category>
		<category><![CDATA[hemimorphite]]></category>
		<category><![CDATA[Montana]]></category>

		<guid isPermaLink="false">http://www.mineralogy.com/?p=599</guid>
		<description><![CDATA[The Summit Mine Source of the finest hemimorphite specimens in the United States © Copyright 2005-2010 Chris Tucker All rights reserved. www.christuckerminerals.com The Minerals Aragonite Colorless crystals of aragonite are fairly common and widespread throughout the mine.  The crystals rarely exceed 1cm in length. Aurichalcite Pale tufts of aurichalcite have been found with wulfenite and hemimorphite in [...]]]></description>
			<content:encoded><![CDATA[<h2 style="text-align: center;">The Summit Mine</h2>
<h3 style="text-align: center;">Source of the finest hemimorphite specimens in the United States</h3>
<p style="text-align: center;">© Copyright 2005-2010 <a href="mailto:chris@christuckerminerals.com">Chris Tucker</a> All rights reserved.</p>
<p style="text-align: center;"><a href="http://www.christuckerminerals.com/">www.christuckerminerals.com</a></p>
<p style="text-align: center;"><strong>The Minerals</strong></p>
<p style="text-align: center;"><strong>Aragonite</strong></p>
<p style="text-align: center;"><span style="color: #333333;">Colorless crystals of aragonite are fairly common and widespread throughout the mine.  The crystals</span><strong><span style="color: #333333;"> </span></strong><span style="color: #333333;">rarely exceed 1cm in length.</span></p>
<p style="text-align: center;"><strong>Aurichalcite</strong></p>
<p style="text-align: center;"><span style="color: #333333;">Pale tufts of aurichalcite have been found with wulfenite and hemimorphite in a narrow fracture about half way to the bottom of the mine.  The aurichalcite crystals reach a few millimeters in size.</span></p>
<p style="text-align: center;">
<div class="wp-caption aligncenter" style="width: 430px"><img class="  " title="Aurichalcite, 2 mm across." src="http://www.christuckerminerals.com/mine%20summit%20surichalcite.jpg" alt="" width="420" height="416" /><p class="wp-caption-text">© Copyright 2005-2010 Chris Tucker - All Rights Reserved  www.christuckerminerals.com</p></div>
<p style="text-align: center;"><strong>Barite</strong></p>
<p style="text-align: center;"><span style="color: #333333;">Massive white barite is locally present; the barite is coarsely crystalline and occasionally forms the matrix of specimens.</span></p>
<p style="text-align: center;"><span style="color: #333333;"><span id="more-599"></span></span></p>
<p style="text-align: center;"><strong>Calcite</strong></p>
<p style="text-align: center;"><strong><span style="color: #ff0000; font-size: large;"><span style="color: #333333;"><br />
</span></span><span style="color: #ffffff;"><span style="color: #333333;"><span style="font-weight: normal;"><span style="color: #333333;">Calcite is widespread throughout the mine.  Colorless to white calcite crystals can be found lining vugs and fractures.  Calcite is commonly the last mineral to have formed.</span></span></span></span></strong></p>
<p style="text-align: center;"><strong><span style="color: #ffffff;"><span style="color: #333333;"><span style="color: #000000;">Cerussite</span></span></span></strong></p>
<p style="text-align: center;"><span style="color: #ffffff;"><span style="color: #333333;"><span style="color: #333333;">Colorless to grey cerussite crystals to 6cm have been found in localized areas.  The crystals are generally crude and rounded although sharp colorless microcrystals have been found.</span></span></span></p>
<p style="text-align: center;"><span style="color: #ffffff;"><span style="color: #333333;"><span style="color: #000000;"> </span></span></span></p>
<p style="text-align: center;">
<p><span style="color: #ffffff;"> </span></p>
<div class="wp-caption aligncenter" style="width: 430px"><img class="   " title="Cerussite, 3 mm across." src="http://www.christuckerminerals.com/mine%20summit%20cerussite.jpg" alt="" width="420" height="388" /><p class="wp-caption-text">© Copyright 2005-2010 Chris Tucker - All Rights Reserved  www.christuckerminerals.com</p></div>
<p style="text-align: center;"><span style="color: #000000;"><strong>Chalcopyrite</strong></span></p>
<p style="text-align: center;"><span style="color: #333333;">A single chalcopyrite crystal was found in massive galena.</span></p>
<p style="text-align: center;"><span style="color: #000000;"><strong>Chlorargyrite</strong></span></p>
<p style="text-align: center;"><span style="color: #333333;">Crude crystals of yellow-green chlorargyrite have been recovered from the lower reaches of the mine.  The crystals rarely exceed 4mm and generally have a &#8220;melted&#8221; appearance.  Chlorargyrite has been found with both residual sulfides and hemimorphite.</span></p>
<p style="text-align: center;"><span style="color: #000000;"> </span></p>
<div class="wp-caption aligncenter" style="width: 430px"><img class="  " title="Chlorargyrite with hemimorphite, 4 mm across." src="http://www.christuckerminerals.com/mine%20summit%20chlorargyrite.jpg" alt="" width="420" height="382" /><p class="wp-caption-text">© Copyright 2005-2010 Chris Tucker - All Rights Reserved  www.christuckerminerals.com</p></div>
<p><span style="color: #333333;">To be continued&#8230; Part 2: The Minerals</span></p>
<p><span style="color: #333333;">Courtesy: Mr. Chris Tucker</span></p>
<p><span style="color: #333333;">All text, images, and design © Copyright 2005-2010</span> <a href="mailto:chris@christuckerminerals.com">Chris Tucker</a> <span style="color: #333333;">All rights reserved.</span></p>
<p><a href="http://www.christuckerminerals.com/">http://www.christuckerminerals.com</a></p>
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		<title>Sunridge Gold</title>
		<link>http://www.mineralogy.com/2010/08/sunridge-gold/</link>
		<comments>http://www.mineralogy.com/2010/08/sunridge-gold/#comments</comments>
		<pubDate>Wed, 18 Aug 2010 15:47:09 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[drilling program]]></category>
		<category><![CDATA[gold]]></category>

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		<description><![CDATA[Sunridge Gold Corp. (SGC/TSX.V) (&#8220;Sunridge&#8221;) is pleased to report important new gold and copper assay results from the Company&#8217;s phase one diamond drill program at the Adi Rassi copper&#8211;gold prospect, part of the Asmara Project in Eritrea. These results indicate that a potentially large new copper and gold zone has been discovered at Adi Rassi. These assay results, combined with recently re-assayed [...]]]></description>
			<content:encoded><![CDATA[<p>Sunridge Gold Corp. (SGC/TSX.V) (&#8220;Sunridge&#8221;) is pleased to report important new gold and copper assay results from the Company&#8217;s phase one diamond drill program at the Adi Rassi copper&#8211;gold prospect, part of the Asmara Project in Eritrea. These results indicate that a potentially large new copper and gold zone has been discovered at Adi Rassi. These assay results, combined with recently re-assayed core, now show a drilled strike length of over 500 metres (see maps and cross-section at the end of this news release).</p>
<p>These results from ongoing exploration programs further demonstrate that the Asmara Project remains wide open for additional discoveries. There are still many untested anomalies and drill targets within the Asmara Project.</p>
<p>Drill Highlights include:</p>
<ul>
<li>AR-002D: 84 metres grading      1.32 g/t gold and      0.84% copper</li>
<li>AR-003D: 25       metres grading 0.75 g/t gold and 0.54% copper</li>
<li>AR-004D: 78       metres grading 0.22 g/t gold and 1.0% copper</li>
</ul>
<p><em>for further information</em>, <em>please visit <a title="sunridgegold" href="http://www.sunridgegold.com/s/PressReleases.asp?ReportID=411847" target="_blank">http://www.sunridgegold.com</a> </em></p>
<p><em>Thu Jul 29, 2010</em></p>
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		<title>Osisko Mining Corporation</title>
		<link>http://www.mineralogy.com/2010/08/osisko-mining-corporation/</link>
		<comments>http://www.mineralogy.com/2010/08/osisko-mining-corporation/#comments</comments>
		<pubDate>Mon, 16 Aug 2010 23:11:03 +0000</pubDate>
		<dc:creator>Mineralogy</dc:creator>
				<category><![CDATA[drilling program]]></category>
		<category><![CDATA[gold]]></category>

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		<description><![CDATA[Osiko Discovers new high-grade extensions in step-out drilling at hammond reef. DDH 368 intersects 9 metres averaging 17.3 g/t Au included within 84 metres averaging 2.78 g/t Au Osisko Mining Corporation (“Osisko”, OSK – TSX; EWX – Deutsche Boerse) and Brett Resources Inc. (&#8220;Brett&#8221;, BBR &#8211; TSX.V) are pleased to announce results from two exploratory [...]]]></description>
			<content:encoded><![CDATA[<p>Osiko Discovers new high-grade extensions in step-out drilling at hammond reef.</p>
<p>DDH 368 intersects 9 metres averaging 17.3 g/t Au included within 84 metres averaging 2.78 g/t Au</p>
<p>Osisko Mining Corporation (“Osisko”, OSK – TSX; EWX – Deutsche Boerse) and Brett Resources Inc. (&#8220;Brett&#8221;, BBR &#8211; TSX.V) are pleased to announce results from two exploratory step-out holes at the ongoing drilling program at Hammond Reef, located in western Ontario. Highlight drill hole BR-368 intersected <strong>9 metres averaging 17.36 g/t Au</strong>, included in a larger intercept of <strong>84 metres averaging 2.78 g/t Au</strong>. The Hammond Reef project is 100 percent owned by Brett, which is currently 77.2% held by Osisko and being fully acquired as a result of the recent all-stock bid.</p>
<p>Results from the two new holes are presented in the table below. These holes were designed to explore the down-dip extension of the deposit in an area formerly known as the Gap Zone between sections 2525E and 2725E.</p>
<p>Fur further information please visit <a title="osiko" href="http://www.osisko.com/en/press/2010/08/12/534/osisko-discovers-new-high-grade-extension-in-step-out-drilling-at-hammond-reef.html" target="_blank">www.osisko.com</a></p>
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