https://earthwise.bgs.ac.uk/index.php?title=Craig_Rossie_-_an_excursion&feed=atom&action=historyCraig Rossie - an excursion - Revision history2024-03-29T06:23:10ZRevision history for this page on the wikiMediaWiki 1.41.0https://earthwise.bgs.ac.uk/index.php?title=Craig_Rossie_-_an_excursion&diff=41094&oldid=prevScotfot at 12:49, 29 May 20192019-05-29T12:49:26Z<p></p>
<a href="https://earthwise.bgs.ac.uk/index.php?title=Craig_Rossie_-_an_excursion&diff=41094&oldid=41093">Show changes</a>Scotfothttps://earthwise.bgs.ac.uk/index.php?title=Craig_Rossie_-_an_excursion&diff=41093&oldid=prevScotfot: /* Excursion 15 Perth */2019-05-29T12:48:11Z<p><span dir="auto"><span class="autocomment">Excursion 15 Perth</span></span></p>
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<tr><td class="diff-marker"></td><td style="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;"><div>This excursion illustrates the Lower Devonian rocks of the Strathmore basin in the Perth area, which are volcanic rocks of the Ochil Volcanic Formation, overlain by sedimentary strata of the Scone Sandstone Formation. In the Stirling–Perth area, these rocks were folded during the mid-Devonian Acadian orogenic event to form part of the southern limb of the ENE-trending Strathmore Syncline and the northern limb of the Ochil–Sidlaw Anticline. Latest Carboniferous quartz-dolerite dykes intrude both of these formations. The mainly grey, fluviatile, channel sandstone bodies along with reddish-brown overbank or lacustrine silty mudstones are part of the sedimentary pile of the Strathmore basin. Bluck (1990) has expressed the view that this river system drained a mountainous area at some distance away, and since the continent–continent collision between Laurentia and</div></td><td class="diff-marker"></td><td style="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;"><div>This excursion illustrates the Lower Devonian rocks of the Strathmore basin in the Perth area, which are volcanic rocks of the Ochil Volcanic Formation, overlain by sedimentary strata of the Scone Sandstone Formation. In the Stirling–Perth area, these rocks were folded during the mid-Devonian Acadian orogenic event to form part of the southern limb of the ENE-trending Strathmore Syncline and the northern limb of the Ochil–Sidlaw Anticline. Latest Carboniferous quartz-dolerite dykes intrude both of these formations. The mainly grey, fluviatile, channel sandstone bodies along with reddish-brown overbank or lacustrine silty mudstones are part of the sedimentary pile of the Strathmore basin. Bluck (1990) has expressed the view that this river system drained a mountainous area at some distance away, and since the continent–continent collision between Laurentia and</div></td></tr>
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</table>Scotfothttps://earthwise.bgs.ac.uk/index.php?title=Craig_Rossie_-_an_excursion&diff=41092&oldid=prevScotfot: Created page with "{{EGSStirling}} Figure 14.1 Geological map of the area around Craig Rossie, showing localities for Excursion 14. File:EGS_STIRL_PLA..."2019-05-29T12:47:18Z<p>Created page with "{{EGSStirling}} <a href="/index.php/File:EGS_STIRL_FIG_14_01.jpg" title="File:EGS STIRL FIG 14 01.jpg">thumbnail|Figure 14.1 Geological map of the area around Craig Rossie, showing localities for Excursion 14.</a> File:EGS_STIRL_PLA..."</p>
<a href="https://earthwise.bgs.ac.uk/index.php?title=Craig_Rossie_-_an_excursion&diff=41092">Show changes</a>Scotfot