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	<id>http://earthwise-staging.bgs.ac.uk/index.php?action=history&amp;feed=atom&amp;title=OR%2F13%2F013_Glossary</id>
	<title>OR/13/013 Glossary - Revision history</title>
	<link rel="self" type="application/atom+xml" href="http://earthwise-staging.bgs.ac.uk/index.php?action=history&amp;feed=atom&amp;title=OR%2F13%2F013_Glossary"/>
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	<updated>2026-04-16T12:14:07Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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	<entry>
		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=OR/13/013_Glossary&amp;diff=30165&amp;oldid=prev</id>
		<title>Dbk: 1 revision imported</title>
		<link rel="alternate" type="text/html" href="http://earthwise-staging.bgs.ac.uk/index.php?title=OR/13/013_Glossary&amp;diff=30165&amp;oldid=prev"/>
		<updated>2016-11-10T12:17:48Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;1&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 13:17, 10 November 2016&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-notice&quot; lang=&quot;en&quot;&gt;&lt;div class=&quot;mw-diff-empty&quot;&gt;(No difference)&lt;/div&gt;
&lt;/td&gt;&lt;/tr&gt;&lt;/table&gt;</summary>
		<author><name>Dbk</name></author>
	</entry>
	<entry>
		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=OR/13/013_Glossary&amp;diff=30164&amp;oldid=prev</id>
		<title>Ajhil at 08:52, 27 October 2016</title>
		<link rel="alternate" type="text/html" href="http://earthwise-staging.bgs.ac.uk/index.php?title=OR/13/013_Glossary&amp;diff=30164&amp;oldid=prev"/>
		<updated>2016-10-27T08:52:41Z</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;__NOTOC__&lt;br /&gt;
{{OR/13/013}}&lt;br /&gt;
&lt;br /&gt;
{|&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| ! scope=&amp;quot;col&amp;quot; style=&amp;quot;width: 140px;&amp;quot; | &amp;#039;&amp;#039;&amp;#039;Aggregate:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| ! scope=&amp;quot;col&amp;quot; style=&amp;quot;width: 700px;&amp;quot; | Particles of rock which, when brought together in a bound or unbound condition, form part or whole of a building or civil engineering structure.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Biogenic:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A material formed by organisms or biological activity.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Carboniferous:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A period of geological time from 359 to 318 million years ago.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Clast:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A rock fragment; commonly applied to a fragment of pre-existing rock included in a younger sediment.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Evaporite:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A mineral formed from precipitation from concentrated brine.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Flint:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Variety of chert occurring in the Chalk of northern Europe.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Fluvial:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Relating to a river; a deposit produced by the action of a river.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Glaciofluvial:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| May be applied to sediment transported and deposited by running water discharged from an ice mass.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Glacial deposits:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Heterogeneous material transported by glaciers or icebergs and deposited directly on land or in the sea. Often poorly sorted.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Gravel:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Granular material in clasts between 4 and 80 millimetres; coarse aggregate.&lt;br /&gt;
Used for general and concrete applications.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Holocene:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| The youngest epoch of the Quaternary period from 0.01 million years to present.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Mineral:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A naturally formed chemical element or compound and normally having a characteristic crystal form and a distinct composition.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Moraine:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A landform deposited directly by a glacier.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Permian:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A period of geological time from 299 to 251 million years ago.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Placer:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A deposit of economic minerals formed by natural (often gravity driven) processes.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Periglacial:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Cold, dry climatic conditions occurring away from glacial ice.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Pleistocene:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| An epoch of the Quaternary period from 2.58 to 0.01 million years ago.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Quartz:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Crystalline silica; an important durable rock-forming mineral.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Quaternary:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| An era of geological time from 2.58 million years ago to present.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Reserve:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| That part of a mineral resource that is economical to work and has been fully evaluated on a systematic basis by drilling and sampling and is free from legal or other obstruction that might inhibit extraction.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Resource:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| Natural accumulations of minerals, or bodies of rock, that are, or may become, of potential economic interest as a basis for the extraction of a commodity.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Sand:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A granular material that is finer than 4&amp;amp;nbsp;mm, but coarser than 0.063&amp;amp;nbsp;mm.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Sandstone:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A sedimentary rock made of abundant fragments of sand size set in a fine-grained matrix or cementing material. The sand particles are usually of quartz.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Siliclastic:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| a clastic sediment predominantly (over 50%) composed of silicate minerals&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Till:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| glacial sediments, often unsorted clay and boulders deposited directly from glaciers.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Triassic:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A Period of geological time from 250 to 200 million years ago.&lt;br /&gt;
|- style=&amp;quot;vertical-align:top;&amp;quot;&lt;br /&gt;
| &amp;#039;&amp;#039;&amp;#039;Westphalian:&amp;#039;&amp;#039;&amp;#039;&lt;br /&gt;
| A Period of geological time during the late Carboniferous.&lt;br /&gt;
|}&lt;br /&gt;
[[Category: OR/13/013 The mineral resources of Scottish waters and the Central North Sea | 08]]&lt;/div&gt;</summary>
		<author><name>Ajhil</name></author>
	</entry>
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