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	<id>https://cornish-semiconductor.com/index.php?action=history&amp;feed=atom&amp;title=Hematite</id>
	<title>Hematite - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://cornish-semiconductor.com/index.php?action=history&amp;feed=atom&amp;title=Hematite"/>
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	<updated>2026-08-24T00:00:36Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>https://cornish-semiconductor.com/index.php?title=Hematite&amp;diff=555&amp;oldid=prev</id>
		<title>Cornish semiconductor at 21:52, 21 July 2026</title>
		<link rel="alternate" type="text/html" href="https://cornish-semiconductor.com/index.php?title=Hematite&amp;diff=555&amp;oldid=prev"/>
		<updated>2026-07-21T21:52:32Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 21:52, 21 July 2026&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l1&quot;&gt;Line 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:Hematite.jpg|thumb|right|frame|Hematite from Tywarnhayle Mine, Porthtowan]]&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;[[File:Hematite.jpg|thumb|right|frame|Hematite from Tywarnhayle Mine, Porthtowan]]&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt; &lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[File:Specularite.jpg|thumb|right|frame|Specularite from Bassett and Grylls Mine, Wendron]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[File:Basset-grylls-spec.png|thumb|right|frame|Curve plot of the specularite shown above from Bassett and Grylls Mine, Wendron]]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Lustre:Metallic, Sub-Metallic, Dull, Earthy&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Lustre:Metallic, Sub-Metallic, Dull, Earthy&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Transparency:Opaque&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Transparency:Opaque&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l15&quot;&gt;Line 15:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 16:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Hematite is an iron ore, and very common in the earths crust - but not that usual to find good crystallised forms of it in Cornish copper and tin mines.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Hematite is an iron ore, and very common in the earths crust - but not that usual to find good crystallised forms of it in Cornish copper and tin mines.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Hematite &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;apparently &lt;/del&gt;is a semiconductor, but &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;trying the specimen &lt;/del&gt;shown here &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;I found at &lt;/del&gt;Tywarnhayle mine near Porthtowan, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;similar to [[wolframite]] it was &lt;/del&gt;unable to carry any current at all. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/del&gt;specularite&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|Specularite]] is &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;different &lt;/del&gt;form of hematite&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, which I will also test&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Hematite is a semiconductor, but &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;it seems to vary depending on where it comes from. The material &lt;/ins&gt;shown here &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;from &lt;/ins&gt;Tywarnhayle mine near Porthtowan, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is &lt;/ins&gt;unable to carry any current at all &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and is an insulator. However material from Bassett and Grylls mine near Wendron seems to provide a voltage drop and a mildly asymmetrical response&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;This second form, although identical in terms of chemistry, is known as &lt;/ins&gt;specularite &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;as &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;more reflective &lt;/ins&gt;form of hematite.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Pages mentioning hematite===&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;===Pages mentioning hematite===&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{Special:WhatLinksHere/Hematite}}&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{Special:WhatLinksHere/Hematite}}&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Cornish semiconductor</name></author>
	</entry>
	<entry>
		<id>https://cornish-semiconductor.com/index.php?title=Hematite&amp;diff=549&amp;oldid=prev</id>
		<title>Cornish semiconductor: Created page with &quot;Hematite from Tywarnhayle Mine, Porthtowan  * Lustre:Metallic, Sub-Metallic, Dull, Earthy * Transparency:Opaque * Colour:Steel-grey to black in crystals and massively crystalline ores, dull to bright &quot;rust-red&quot; in earthy, compact, fine-grained material. * Streak:Reddish brown (&quot;rust-red&quot;); blackish when Ti-bearing * Hardness:5 - 6 on Mohs scale * Tenacity:Brittle * Cleavage:None Observed * Parting:Partings on {0001} and {1011} due...&quot;</title>
		<link rel="alternate" type="text/html" href="https://cornish-semiconductor.com/index.php?title=Hematite&amp;diff=549&amp;oldid=prev"/>
		<updated>2026-07-18T16:49:33Z</updated>

		<summary type="html">&lt;p&gt;Created page with &amp;quot;&lt;a href=&quot;/index.php/File:Hematite.jpg&quot; title=&quot;File:Hematite.jpg&quot;&gt;thumb|right|frame|Hematite from Tywarnhayle Mine, Porthtowan&lt;/a&gt;  * Lustre:Metallic, Sub-Metallic, Dull, Earthy * Transparency:Opaque * Colour:Steel-grey to black in crystals and massively crystalline ores, dull to bright &amp;quot;rust-red&amp;quot; in earthy, compact, fine-grained material. * Streak:Reddish brown (&amp;quot;rust-red&amp;quot;); blackish when Ti-bearing * Hardness:5 - 6 on Mohs scale * Tenacity:Brittle * Cleavage:None Observed * Parting:Partings on {0001} and {1011} due...&amp;quot;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:Hematite.jpg|thumb|right|frame|Hematite from Tywarnhayle Mine, Porthtowan]]&lt;br /&gt;
&lt;br /&gt;
* Lustre:Metallic, Sub-Metallic, Dull, Earthy&lt;br /&gt;
* Transparency:Opaque&lt;br /&gt;
* Colour:Steel-grey to black in crystals and massively crystalline ores, dull to bright &amp;quot;rust-red&amp;quot; in earthy, compact, fine-grained material.&lt;br /&gt;
* Streak:Reddish brown (&amp;quot;rust-red&amp;quot;); blackish when Ti-bearing&lt;br /&gt;
* Hardness:5 - 6 on Mohs scale&lt;br /&gt;
* Tenacity:Brittle&lt;br /&gt;
* Cleavage:None Observed&lt;br /&gt;
* Parting:Partings on {0001} and {1011} due to twinning. Unique cubic parting in masses and grains at Franklin Mine, Franklin, NJ.&lt;br /&gt;
* Fracture:Irregular/Uneven, Sub-Conchoidal&lt;br /&gt;
&lt;br /&gt;
[https://www.mindat.org Data from mindat.org]&lt;br /&gt;
&lt;br /&gt;
Hematite is an iron ore, and very common in the earths crust - but not that usual to find good crystallised forms of it in Cornish copper and tin mines.&lt;br /&gt;
&lt;br /&gt;
Hematite apparently is a semiconductor, but trying the specimen shown here I found at Tywarnhayle mine near Porthtowan, similar to [[wolframite]] it was unable to carry any current at all. [[specularite|Specularite]] is a different form of hematite, which I will also test.&lt;br /&gt;
&lt;br /&gt;
===Pages mentioning hematite===&lt;br /&gt;
&lt;br /&gt;
{{Special:WhatLinksHere/Hematite}}&lt;/div&gt;</summary>
		<author><name>Cornish semiconductor</name></author>
	</entry>
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