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	<title>Kirkwood Formation - Revision history</title>
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	<updated>2026-04-17T19:05:11Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Kirkwood_Formation&amp;diff=52687&amp;oldid=prev</id>
		<title>Dbk: 1 revision imported</title>
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		<updated>2021-07-26T14:53:54Z</updated>

		<summary type="html">&lt;p&gt;1 revision imported&lt;/p&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 15:53, 26 July 2021&lt;/td&gt;
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		<author><name>Dbk</name></author>
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	<entry>
		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Kirkwood_Formation&amp;diff=52686&amp;oldid=prev</id>
		<title>Geosource&gt;Volunteer 01: /* Kirkwood Formation (KRW), Carboniferous, Midland Valley of Scotland */</title>
		<link rel="alternate" type="text/html" href="http://earthwise-staging.bgs.ac.uk/index.php?title=Kirkwood_Formation&amp;diff=52686&amp;oldid=prev"/>
		<updated>2015-10-27T11:55:59Z</updated>

		<summary type="html">&lt;p&gt;&lt;span dir=&quot;auto&quot;&gt;&lt;span class=&quot;autocomment&quot;&gt;Kirkwood Formation (KRW), Carboniferous, Midland Valley of Scotland&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;==Kirkwood Formation [http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=KRW (KRW)], Carboniferous, Midland Valley of Scotland ==&lt;br /&gt;
Kirkwood Formation is part of the [[Strathclyde Group]].&lt;br /&gt;
=== Name ===&lt;br /&gt;
Taken from Kirkwood Farm, Strathclyde Region. The name was introduced by Monro (1982)&amp;lt;ref name=&amp;quot;Monro82&amp;quot;&amp;gt;Monro, S K. 1982. Stratigraphy, sedimentation and tectonics in the Dalry Basin, Ayrshire. Unpublished PhD Thesis, University of Edinburgh&amp;lt;/ref&amp;gt;.&lt;br /&gt;
&lt;br /&gt;
=== Lithology ===&lt;br /&gt;
The Kirkwood Formation consists of tuffaceous mudstones and tuffs, locally intercalated with non-tuffaceous sedimentary rocks, with some marine horizons developed. The tuffaceous mudstones and tuffs vary in colour from dark reddish brown to greenish grey. Non-tuffaceous sedimentary rocks, sandstones, siltstones and limestones, generally grey in colour, also occur within a restricted area intercalated with volcaniclastic rocks.&lt;br /&gt;
&lt;br /&gt;
=== Genetic interpretation ===&lt;br /&gt;
The strata were largely formed by the reworking of materials derived from the underlying volcanic rocks but some primary ash-fall tuffs may be present. The formation shows extensive lateritisation, the product of a period of intense subaerial tropical weathering. There are some marine incursions.&lt;br /&gt;
&lt;br /&gt;
=== Stratotype ===&lt;br /&gt;
The type section of the Kirkwood Formation occurs between 38.9 and 75.45 m depth in the Kirkwood Borehole (BGS Registration Number NS34NE/11) (NS 3885 4716), near Kilmarnock (Monro, 1999)&amp;lt;ref name=&amp;quot;Monro99&amp;quot;&amp;gt;Monro, S K. 1999. Geology of the Irvine district. &amp;#039;&amp;#039;Memoir of the British Geological Survey&amp;#039;&amp;#039;, Sheet 22W, part 21E (Scotland)&amp;lt;/ref&amp;gt;. This is the complete thickness of the formation at this locality.&lt;br /&gt;
&lt;br /&gt;
=== Lower and upper boundaries ===&lt;br /&gt;
The base of the formation is taken at the lithological change from the underlying lavas of the [[Clyde Plateau Volcanic Formation]] into volcaniclastic sedimentary rocks (Figure 6, Column 4A).&lt;br /&gt;
&lt;br /&gt;
The top is generally taken at the base of the overlying mudstones, siltstones and sandstones of the [[Lawmuir Formation]] or the cyclical limestones and clastic lithologies of the [[Lower Limestone Formation]] ([[Clackmannan Group]]). This boundary is commonly irregular and transitional with an interdigitation of lithologies.&lt;br /&gt;
&lt;br /&gt;
=== Thickness ===&lt;br /&gt;
The Kirkwood Formation varies in thickness, from about 6 to more than 41 m (Monro, 1999, fig. 9)&amp;lt;ref name=&amp;quot;Monro99&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt; with thinning generally taking place towards the areas where the [[Clyde Plateau Volcanic Formation]] is thick. In the Irvine district, Monro (1999, p. 35, fig. 11)&amp;lt;ref name=&amp;quot;Monro99&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt; recorded a thickness of 41.39 m encountered in the Coalhill No. 2 Borehole (BGS Registration Number NS24NW/20) (NS 2432 4653) (a minimum thickness since the borehole did not reach the [[Clyde Plateau Volcanic Formation]]), and referred to localised thinning in boreholes close to the Dusk Water Fault. In the Kilmarnock district MacPherson et al. (2000, p.9)&amp;lt;ref&amp;gt;MacPherson, K A T, Smith, R A, and Akhurst, M C. 2000. Geology of the Kilmarnock district. &amp;#039;&amp;#039;Sheet description of the British Geological Survey&amp;#039;&amp;#039;, Sheet 22E (Scotland)&amp;lt;/ref&amp;gt; stated that the thickness of the formation averages around 15 m. BGS (1996)&amp;lt;ref&amp;gt;British Geological Survey. 1996. Campbeltown. Scotland Sheet 12, Provisional Series. Solid and Drift 1:50.000. (Keyworth, Nottingham: British Geological Survey.)&amp;lt;/ref&amp;gt; gave a generalised thickness of 18.75 m for the formation in the main coalfield area at Machrihanish.&lt;br /&gt;
&lt;br /&gt;
=== Distribution and regional correlation ===&lt;br /&gt;
Western Midland Valley and Machrihanish.&lt;br /&gt;
&lt;br /&gt;
=== Age ===&lt;br /&gt;
Visean (Asbian to early Brigantian) (Monro, 1999&amp;lt;ref name=&amp;quot;Monro99&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt;; Browne et al., 1999&amp;lt;ref&amp;gt;Browne, M A E, Dean, M T, Hall, I H S, McAdam, A D, Monro, S K, and Chisholm, J I. 1999. A lithostratigraphical framework for the Carboniferous rocks of the Midland Valley of Scotland. &amp;#039;&amp;#039;British Geological Survey Research Report&amp;#039;&amp;#039;, RR/99/07&amp;lt;/ref&amp;gt;)&lt;br /&gt;
&lt;br /&gt;
== References ==&lt;br /&gt;
&amp;lt;references/&amp;gt;&lt;br /&gt;
[[Category:Carboniferous lithostratigraphical nomenclature]]&lt;/div&gt;</summary>
		<author><name>Geosource&gt;Volunteer 01</name></author>
	</entry>
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