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		<updated>2015-05-06T20:49:38Z</updated>

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{{Information&lt;br /&gt;
|description={{en|1=Stratigraphic column at Port nan Clach Cruinn. Key &lt;br /&gt;
&lt;br /&gt;
1 Vesicular lava with basal pipe amygdales. Load structures cause sediment to be squeezed upwards into lava. Toes of lava project downwards and northwards into the sediment causing minor fold disturbances. &lt;br /&gt;
2 Interbedded cream limestone (1-3 cm) and cream calcareous phyllite (0.5-1 cm). &lt;br /&gt;
3 Channel filled by limestone containing boulders of grey limestone in a matrix charged with angular fragments of quartz. Whole unit is cross-bedded, indicating derivation from south. &lt;br /&gt;
4 Pure grey limestone with beds 1-10 cm thick. &lt;br /&gt;
5 Parallel laminated (0.5-1 cm) limestone. &lt;br /&gt;
6 Graded limestone with fragments of quartz (1-1.5 cm) and black calcareous slate. Channelled base trending 110°. Intruded from below by a sedimentary dyke of 7. &lt;br /&gt;
7 Laminated (0.2-2 cm) limestone with sand-sized quartz fragments. &lt;br /&gt;
8 Conglomerate with boulders of dark grey limestone. &lt;br /&gt;
9 As 7. &lt;br /&gt;
10 Conglomerate of rusty weathering black limestone with largest fragments measuring 100 X 50 cm. &lt;br /&gt;
11 As 7. &lt;br /&gt;
12 Grey limestone with fragments (0.5-1 cm) of malachite and quartz. &lt;br /&gt;
13 As 7 with ripple marked base. &lt;br /&gt;
14 Massive limestone with quartz (0.5-1.5 cm) and black slaty limestone (1-3 cm) fragments. Flute casts at base indicate current from south-east.  From: P. J. Gower 1977. 3: The Dalradian rocks of the west coast of the Tayvallich peninsula. Scottish Journal of Geology v 13. p125-133.}}&lt;br /&gt;
|date=2015-05-06 21:32:18&lt;br /&gt;
|source=Dalradian rocks of the South-west Highlands. Scottish Journal of Geology 13 (2) 1977&lt;br /&gt;
|author=Edinburgh Geological Society&lt;br /&gt;
|permission=&lt;br /&gt;
|other versions=&lt;br /&gt;
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		<author><name>Scotfot</name></author>
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