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	<id>https://cameo.mfa.org/index.php?action=history&amp;feed=atom&amp;title=Secondary_clay</id>
	<title>Secondary clay - Revision history</title>
	<link rel="self" type="application/atom+xml" href="https://cameo.mfa.org/index.php?action=history&amp;feed=atom&amp;title=Secondary_clay"/>
	<link rel="alternate" type="text/html" href="https://cameo.mfa.org/index.php?title=Secondary_clay&amp;action=history"/>
	<updated>2026-08-29T03:40:41Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
	<generator>MediaWiki 1.39.4</generator>
	<entry>
		<id>https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=88134&amp;oldid=prev</id>
		<title>MDerrick: /* Description */</title>
		<link rel="alternate" type="text/html" href="https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=88134&amp;oldid=prev"/>
		<updated>2022-06-16T17:21:06Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Description&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:21, 16 June 2022&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-l3&quot;&gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;See also [[ball%20clay|ball clay]], [[red%20clay|red clay]], [[calcareous|calcareous clay]], siliceous clay, [[fire%20brick|fire clay]], [[stoneware&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay&lt;/del&gt;|stoneware clay]], &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[fusible%20clay|&lt;/del&gt;fusible clay&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]]&lt;/del&gt;, [[marl|marl]].&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;See also [[ball%20clay|ball clay]], [[red%20clay|red clay]], [[calcareous|calcareous clay]], siliceous clay, [[fire%20brick|fire clay]], [[stoneware|stoneware clay]], fusible clay, [[marl|marl]].&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;== Synonyms and Related Terms ==&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;== Synonyms and Related Terms ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>MDerrick</name></author>
	</entry>
	<entry>
		<id>https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=88133&amp;oldid=prev</id>
		<title>MDerrick at 17:20, 16 June 2022</title>
		<link rel="alternate" type="text/html" href="https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=88133&amp;oldid=prev"/>
		<updated>2022-06-16T17:20:17Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 13:20, 16 June 2022&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-l3&quot;&gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;See also [[ball%20clay|ball clay]], [[red%20clay|red clay]], [[calcareous&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay&lt;/del&gt;|calcareous clay]], &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[siliceous%20clay|&lt;/del&gt;siliceous clay&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]]&lt;/del&gt;, [[fire%&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;20clay&lt;/del&gt;|fire clay]], [[stoneware%20clay|stoneware clay]], [[fusible%20clay|fusible clay]], [[marl|marl]].&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;See also [[ball%20clay|ball clay]], [[red%20clay|red clay]], [[calcareous|calcareous clay]], siliceous clay, [[fire%&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;20brick&lt;/ins&gt;|fire clay]], [[stoneware%20clay|stoneware clay]], [[fusible%20clay|fusible clay]], [[marl|marl]].&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;== Synonyms and Related Terms ==&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;== Synonyms and Related Terms ==&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-l9&quot;&gt;Line 9:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 9:&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;sedimentary clay; ball clay; arcillas secundarias (Esp.); secundaire klei (Ned.); barro secundário (Port.)&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;sedimentary clay; ball clay; arcillas secundarias (Esp.); secundaire klei (Ned.); barro secundário (Port.)&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;== &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Sources Checked for Data in Record &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;==&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Resources and Citations&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;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;* Henry Hodges, &amp;#039;&amp;#039;Artifacts: An Introduction to Early Materials and Technology&amp;#039;&amp;#039;, Ronald P. Frye, Kingston, Canada, 1988&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;* Henry Hodges, &amp;#039;&amp;#039;Artifacts: An Introduction to Early Materials and Technology&amp;#039;&amp;#039;, Ronald P. Frye, Kingston, Canada, 1988&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>MDerrick</name></author>
	</entry>
	<entry>
		<id>https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=54945&amp;oldid=prev</id>
		<title>Jruggiero: Text replace - &quot;\[http:\/\/cameo\.mfa\.org\/materials\/fullrecord\.asp\?name=([^\s]+)\s(.*)\]&quot; to &quot;$2&quot;</title>
		<link rel="alternate" type="text/html" href="https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=54945&amp;oldid=prev"/>
		<updated>2016-05-10T17:08:33Z</updated>

		<summary type="html">&lt;p&gt;Text replace - &amp;quot;\[http:\/\/cameo\.mfa\.org\/materials\/fullrecord\.asp\?name=([^\s]+)\s(.*)\]&amp;quot; to &amp;quot;&lt;a href=&quot;/index.php?title=$1&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;$1 (page does not exist)&quot;&gt;$2&lt;/a&gt;&amp;quot;&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 13:08, 10 May 2016&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-l3&quot;&gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;See also [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;ball%20clay ball clay], [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;red%20clay red clay], [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;calcareous%20clay calcareous clay], [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;siliceous%20clay siliceous clay], [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;fire%20clay fire clay], [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;stoneware%20clay stoneware clay], [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;fusible%20clay fusible clay], [&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;http://cameo.mfa.org/materials/fullrecord.asp?name=&lt;/del&gt;marl marl].&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;See also [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;ball%20clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;ball clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;], [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;red%20clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;red clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;], [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;calcareous%20clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;calcareous clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;], [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;siliceous%20clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;siliceous clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;], [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;fire%20clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;fire clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;], [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;stoneware%20clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;stoneware clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;], [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;fusible%20clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;fusible clay&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;], [&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;marl&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;marl&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&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;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;== Synonyms and Related Terms ==&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;== Synonyms and Related Terms ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jruggiero</name></author>
	</entry>
	<entry>
		<id>https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=52600&amp;oldid=prev</id>
		<title>Jruggiero: Text replace - &quot;== Authority ==&quot; to &quot;== Sources Checked for Data in Record ==&quot;</title>
		<link rel="alternate" type="text/html" href="https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=52600&amp;oldid=prev"/>
		<updated>2016-05-01T23:17:33Z</updated>

		<summary type="html">&lt;p&gt;Text replace - &amp;quot;== Authority ==&amp;quot; to &amp;quot;== Sources Checked for Data in Record ==&amp;quot;&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 19:17, 1 May 2016&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-l9&quot;&gt;Line 9:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 9:&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;sedimentary clay; ball clay; arcillas secundarias (Esp.); secundaire klei (Ned.); barro secundário (Port.)&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;sedimentary clay; ball clay; arcillas secundarias (Esp.); secundaire klei (Ned.); barro secundário (Port.)&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;== &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Authority &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;== &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Sources Checked for Data in Record &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;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;* Henry Hodges, &amp;#039;&amp;#039;Artifacts: An Introduction to Early Materials and Technology&amp;#039;&amp;#039;, Ronald P. Frye, Kingston, Canada, 1988&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;* Henry Hodges, &amp;#039;&amp;#039;Artifacts: An Introduction to Early Materials and Technology&amp;#039;&amp;#039;, Ronald P. Frye, Kingston, Canada, 1988&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Jruggiero</name></author>
	</entry>
	<entry>
		<id>https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=29195&amp;oldid=prev</id>
		<title>Unknown user at 12:39, 24 July 2013</title>
		<link rel="alternate" type="text/html" href="https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=29195&amp;oldid=prev"/>
		<updated>2013-07-24T12:39:38Z</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;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&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 08:39, 24 July 2013&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-l3&quot;&gt;Line 3:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 3:&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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay.  &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;See also [http://cameo.mfa.org/materials/fullrecord.asp?name=ball &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;clay &lt;/del&gt;ball clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=red &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;clay &lt;/del&gt;red clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=calcareous &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;clay &lt;/del&gt;calcareous clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=siliceous &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;clay &lt;/del&gt;siliceous clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=fire &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;clay &lt;/del&gt;fire clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=stoneware &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;clay &lt;/del&gt;stoneware clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=fusible &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;clay &lt;/del&gt;fusible clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=marl marl].&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;See also [http://cameo.mfa.org/materials/fullrecord.asp?name=ball&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay &lt;/ins&gt;ball clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=red&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay &lt;/ins&gt;red clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=calcareous&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay &lt;/ins&gt;calcareous clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=siliceous&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay &lt;/ins&gt;siliceous clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=fire&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay &lt;/ins&gt;fire clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=stoneware&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay &lt;/ins&gt;stoneware clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=fusible&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;%20clay &lt;/ins&gt;fusible clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=marl marl].&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;== Synonyms and Related Terms ==&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;== Synonyms and Related Terms ==&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;sedimentary clay; ball clay; arcillas secundarias (Esp.); secundaire klei (Ned.); barro &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;secundrio &lt;/del&gt;(Port.)&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;sedimentary clay; ball clay; arcillas secundarias (Esp.); secundaire klei (Ned.); barro &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;secundário &lt;/ins&gt;(Port.)&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;== Authority ==&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;== Authority ==&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;* &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Henry Hodges, &lt;/del&gt;Henry Hodges, &amp;#039;&amp;#039;Artifacts: An Introduction to Early Materials and Technology&amp;#039;&amp;#039;, Ronald P. Frye, Kingston, Canada, 1988&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;* Henry Hodges, &amp;#039;&amp;#039;Artifacts: An Introduction to Early Materials and Technology&amp;#039;&amp;#039;, Ronald P. Frye, Kingston, Canada, 1988&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;* &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Robert Fournier, &lt;/del&gt;Robert Fournier, &amp;#039;&amp;#039;Illustrated Dictionary of Practical Pottery&amp;#039;&amp;#039;, Chilton Book Company, Radnor, PA, 1992&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;* Robert Fournier, &amp;#039;&amp;#039;Illustrated Dictionary of Practical Pottery&amp;#039;&amp;#039;, Chilton Book Company, Radnor, PA, 1992&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;* &amp;#039;&amp;#039;The Dictionary of Art&amp;#039;&amp;#039;, Grove&amp;#039;s Dictionaries Inc., New York, 1996  Comment: &amp;quot;Ceramic&amp;quot;&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;* &amp;#039;&amp;#039;The Dictionary of Art&amp;#039;&amp;#039;, Grove&amp;#039;s Dictionaries Inc., New York, 1996  Comment: &amp;quot;Ceramic&amp;quot;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Unknown user</name></author>
	</entry>
	<entry>
		<id>https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=14471&amp;oldid=prev</id>
		<title>Unknown user at 18:17, 27 April 2013</title>
		<link rel="alternate" type="text/html" href="https://cameo.mfa.org/index.php?title=Secondary_clay&amp;diff=14471&amp;oldid=prev"/>
		<updated>2013-04-27T18:17:19Z</updated>

		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;== Description ==&lt;br /&gt;
&lt;br /&gt;
Clay that has been deposited away from the site of the parent feldspathic rock. Secondary clays are often carried downstream by rivers producing a fine particle, highly weathered clay that is deposited along the banks or in estuaries. Secondary clays tend to be very plastic and, without the addition of other materials, may shrink severely when dried. However, in most cases, secondary clays have naturally combined with other other minerals, such as silica, iron oxides and calcium carbonate, that can minimize shrinkage. Additionally, any alkaline oxide impurity can act as a flux when the clay is heated and lower the sintering point of the clay. Iron oxide impurities may add red or yellow color to the clay. &lt;br /&gt;
&lt;br /&gt;
See also [http://cameo.mfa.org/materials/fullrecord.asp?name=ball clay ball clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=red clay red clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=calcareous clay calcareous clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=siliceous clay siliceous clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=fire clay fire clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=stoneware clay stoneware clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=fusible clay fusible clay], [http://cameo.mfa.org/materials/fullrecord.asp?name=marl marl].&lt;br /&gt;
&lt;br /&gt;
== Synonyms and Related Terms ==&lt;br /&gt;
&lt;br /&gt;
sedimentary clay; ball clay; arcillas secundarias (Esp.); secundaire klei (Ned.); barro secundrio (Port.)&lt;br /&gt;
&lt;br /&gt;
== Authority ==&lt;br /&gt;
&lt;br /&gt;
* Henry Hodges, Henry Hodges, &amp;#039;&amp;#039;Artifacts: An Introduction to Early Materials and Technology&amp;#039;&amp;#039;, Ronald P. Frye, Kingston, Canada, 1988&lt;br /&gt;
&lt;br /&gt;
* Robert Fournier, Robert Fournier, &amp;#039;&amp;#039;Illustrated Dictionary of Practical Pottery&amp;#039;&amp;#039;, Chilton Book Company, Radnor, PA, 1992&lt;br /&gt;
&lt;br /&gt;
* &amp;#039;&amp;#039;The Dictionary of Art&amp;#039;&amp;#039;, Grove&amp;#039;s Dictionaries Inc., New York, 1996  Comment: &amp;quot;Ceramic&amp;quot;&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
[[Category:Materials database]]&lt;/div&gt;</summary>
		<author><name>Unknown user</name></author>
	</entry>
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