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	<title>Langness Conglomerate Formation - Revision history</title>
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		<id>http://earthwise-staging.bgs.ac.uk/index.php?title=Langness_Conglomerate_Formation&amp;diff=52782&amp;oldid=prev</id>
		<title>Geosource&gt;Volunteer 01 at 11:11, 8 July 2015</title>
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&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;==Langness Conglomerate Formation [http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=LNCO (LNCO)], Carboniferous, Isle of Man==&lt;br /&gt;
Langness Conglomerate Formation is part of the [[Ravenstonedale Group]]&lt;br /&gt;
=== Name ===&lt;br /&gt;
The name is derived from Langness, south Isle of Man, and was given by Dickson et al. (1987)&amp;lt;ref name=&amp;quot;Dickson&amp;quot;&amp;gt;Dickson, J A D, Ford, T D, and Swift, A.1987.The strati-graphy of the Carboniferous rocks around Castletown, Isle of Man.&amp;#039;&amp;#039;Proceedings of the Yorkshire Geological Society&amp;#039;&amp;#039;, Vol. 46, 203–229&amp;lt;/ref&amp;gt;.&lt;br /&gt;
&lt;br /&gt;
=== Lithology ===&lt;br /&gt;
The formation comprises reddish brown, generally poorly sorted, typically clast-supported conglomerate with subordinate interbedded sandstone. Sedimentary structures include crude stratification and rare cross-bedding. See Chadwick et al. (2001)&amp;lt;ref name=&amp;quot;Chadwick01&amp;quot;&amp;gt;Chadwick, R A, Jackson, D I, Barnes, R P, Kimbell, G S, Johnson, H, Chiverrell, R C, Thomas, G S P, Jones, N S, Riley, N J, Pickett, E A, Young, B, Holliday, D W, Ball, D F, Molyneux, S G, Long, D, Power, G M, and Roberts, D H.2001.The geology of the Isle of Man and its offshore area.&amp;#039;&amp;#039;British Geological Survey Research Report&amp;#039;&amp;#039;, RR/01/06&amp;lt;/ref&amp;gt;.&lt;br /&gt;
&lt;br /&gt;
=== Genetic interpretation ===&lt;br /&gt;
The formation is an alluvial fan deposit, transported by debris flow and streamflow processes.&lt;br /&gt;
&lt;br /&gt;
=== Stratotype ===&lt;br /&gt;
A partial type section includes foreshore exposures along the Langness Peninsula (SC 2819 6604 to 2854 6661) where an estimated 30 m of coarse clastic sedimentary rocks are present (see Dickson et al., 1987, p. 205&amp;lt;ref name=&amp;quot;Dickson&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt;).&lt;br /&gt;
&lt;br /&gt;
=== Lower and upper boundaries ===&lt;br /&gt;
The formation is unconformable on the underlying, steeper-dipping, Ordovician Lonan Formation (see Chadwick et al., 2001&amp;lt;ref name=&amp;quot;Chadwick01&amp;quot;&amp;gt;&amp;lt;/ref&amp;gt;).&lt;br /&gt;
&lt;br /&gt;
The limestones of the Turkeyland Member, Derbyhaven Formation, Great Scar Limestone Group (Figure.8, Column.8) overlie the apparently partly reworked sandstone top to the Langness Conglomerate Formation.&lt;br /&gt;
&lt;br /&gt;
=== Thickness ===&lt;br /&gt;
The formation is about 30 m thick.&lt;br /&gt;
&lt;br /&gt;
=== Distribution and regional correlation ===&lt;br /&gt;
The formation occurs in the south Isle of Man.&lt;br /&gt;
&lt;br /&gt;
=== Age ===&lt;br /&gt;
Devonian to Courceyan (Chadwick et al., 2001, p. 59&amp;lt;ref name=&amp;quot;Chadwick01&amp;quot;&amp;gt;&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>
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