https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&feed=atom&action=history
Foreland succession of the Loch Assynt roadside, North-west Highlands - an excursion - Revision history
2024-03-28T23:05:09Z
Revision history for this page on the wiki
MediaWiki 1.41.0
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24064&oldid=prev
Scotfot: /* Locality 1.6 Typical outcrops of Applecross Formation. [NC 2248 2479] */
2015-12-19T08:32:36Z
<p><span dir="auto"><span class="autocomment">Locality 1.6 Typical outcrops of Applecross Formation. [NC 2248 2479]</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:32, 19 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l37">Line 37:</td>
<td colspan="2" class="diff-lineno">Line 37:</td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.6 Typical outcrops of Applecross Formation. [NC 2248 2479] ==</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>== Locality 1.6 Typical outcrops of Applecross Formation. [NC 2248 2479] ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Continuing eastwards, just beyond an old road sign and set back 20m from the road next to a small holly is an easily accessible outcrop of typical Applecross Formation. The grain size varies from very coarse sand to granule and the clasts are angular to sub-angular; there is very little silt or clay, in common with most of the Applecross Formation. Compositionally, the sediment contains a high proportion of terracotta-coloured feldspar and lithic clasts in addition to vein and polycrystalline quartz. Trough cross-bedding is common throughout, with sets varying from 10–20cm. On the upper surface of the outcrop, sets can be seen clearly in 3D with current directions towards 100˚. The sediments were deposited by deep, perennial braided rivers that formed a very large-scale braidplain, with a mean current direction of 123˚ (Stewart, 2002).</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Continuing eastwards, just beyond an old road sign and set back 20m from the road next to a small holly is an easily accessible outcrop of typical Applecross Formation. The grain size varies from very coarse sand to granule and the clasts are angular to sub-angular; there is very little silt or clay, in common with most of the Applecross Formation. Compositionally, the sediment contains a high proportion of terracotta-coloured feldspar and lithic clasts in addition to vein and polycrystalline quartz. Trough cross-bedding is common throughout, with sets varying from 10–20cm<ins style="font-weight: bold; text-decoration: none;">[[Media:EGS_NWH_FIG_014.jpg| (See image)]]</ins>. On the upper surface of the outcrop, sets can be seen clearly in 3D with current directions towards 100˚. The sediments were deposited by deep, perennial braided rivers that formed a very large-scale braidplain, with a mean current direction of 123˚ (Stewart, 2002).</div></td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.7 The basal Cambrian unconformity. [NC 2273 2470] ==</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>== Locality 1.7 The basal Cambrian unconformity. [NC 2273 2470] ==</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24063&oldid=prev
Scotfot at 08:31, 19 December 2015
2015-12-19T08:31:05Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:31, 19 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l31">Line 31:</td>
<td colspan="2" class="diff-lineno">Line 31:</td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.4 Base of the Applecross Formation. [NC 2194 2497] ==</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>== Locality 1.4 Base of the Applecross Formation. [NC 2194 2497] ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Thirty metres before the end of the roadside safety barrier, the character of the road-cut changes and thick, trough cross-bedded sandstones of the Applecross Formation (Torridon Group) can be seen to conformably overlie the thinly bedded, poorly sorted, laminated granulestones of the Diabaig Formation. The lithology of the Applecross Formation will be examined at Locality</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Thirty metres before the end of the roadside safety barrier, the character of the road-cut changes and thick, trough cross-bedded sandstones of the Applecross Formation (Torridon Group) can be seen to conformably overlie the thinly bedded, poorly sorted, laminated granulestones of the Diabaig Formation<ins style="font-weight: bold; text-decoration: none;">[[Media:P506431.jpg| (P506431)]]</ins>. The lithology of the Applecross Formation will be examined at Locality</div></td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.5 Glacial striae. [NC 2225 2489] ==</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>== Locality 1.5 Glacial striae. [NC 2225 2489] ==</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24062&oldid=prev
Scotfot at 08:27, 19 December 2015
2015-12-19T08:27:13Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:27, 19 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l16">Line 16:</td>
<td colspan="2" class="diff-lineno">Line 16:</td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507] ==</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>== Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507] ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Park in the lay-by [NC 212 251] alongside the A837 to Lochinver from Skiag Bridge (second lay-by on the left). From the lay-by, walk down to a small east-facing bay on the shore of Loch Assynt, adjacent to an island with two large Scots Pines and many dead trees. The bay [NC 2125 2507] contains a 9m-wide, ESE-trending ultramafic Scourie Dyke, intruded into Lewisian orthogneisses with a westward dipping foliation[[Media:P531871.jpg| P531871]]. The core of the dyke is a fairly fresh, olivine-rich metaclinopyroxene-norite (Tarney, 1973). The host rocks are chiefly pyroxene-bearing felsic gneisses, consisting of quartz, feldspar and hypersthene, with hornblende and biotite also present. Lenses, pods and bands of both mafic and ultramafic rock are common and are generally unfoliated.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Park in the lay-by [NC 212 251] alongside the A837 to Lochinver from Skiag Bridge (second lay-by on the left). From the lay-by, walk down to a small east-facing bay on the shore of Loch Assynt<ins style="font-weight: bold; text-decoration: none;">[[Media:EGS_NWH_FIG_011.jpg| (See image)]]</ins>, adjacent to an island with two large Scots Pines and many dead trees. The bay [NC 2125 2507] contains a 9m-wide, ESE-trending ultramafic Scourie Dyke, intruded into Lewisian orthogneisses with a westward dipping foliation[[Media:P531871.jpg| P531871]]. The core of the dyke is a fairly fresh, olivine-rich metaclinopyroxene-norite (Tarney, 1973). The host rocks are chiefly pyroxene-bearing felsic gneisses, consisting of quartz, feldspar and hypersthene, with hornblende and biotite also present. Lenses, pods and bands of both mafic and ultramafic rock are common and are generally unfoliated.</div></td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.2 Basal unconformity of the Torridon Group. [NC 2134 2516] ==</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>== Locality 1.2 Basal unconformity of the Torridon Group. [NC 2134 2516] ==</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24061&oldid=prev
Scotfot at 08:25, 19 December 2015
2015-12-19T08:25:51Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:25, 19 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l16">Line 16:</td>
<td colspan="2" class="diff-lineno">Line 16:</td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507] ==</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>== Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507] ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Park in the lay-by [NC 212 251] alongside the A837 to Lochinver from Skiag Bridge (second lay-by on the left). From the lay-by, walk down to a small east-facing bay on the shore of Loch Assynt, adjacent to an island with two large Scots Pines and many dead trees. The bay [NC 2125 2507] contains a 9m-wide, ESE-trending ultramafic Scourie Dyke, intruded into Lewisian orthogneisses with a westward dipping foliation[[Media:P531871.jpg|P531871]]. The core of the dyke is a fairly fresh, olivine-rich metaclinopyroxene-norite (Tarney, 1973). The host rocks are chiefly pyroxene-bearing felsic gneisses, consisting of quartz, feldspar and hypersthene, with hornblende and biotite also present. Lenses, pods and bands of both mafic and ultramafic rock are common and are generally unfoliated.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Park in the lay-by [NC 212 251] alongside the A837 to Lochinver from Skiag Bridge (second lay-by on the left). From the lay-by, walk down to a small east-facing bay on the shore of Loch Assynt, adjacent to an island with two large Scots Pines and many dead trees. The bay [NC 2125 2507] contains a 9m-wide, ESE-trending ultramafic Scourie Dyke, intruded into Lewisian orthogneisses with a westward dipping foliation[[Media:P531871.jpg| P531871]]. The core of the dyke is a fairly fresh, olivine-rich metaclinopyroxene-norite (Tarney, 1973). The host rocks are chiefly pyroxene-bearing felsic gneisses, consisting of quartz, feldspar and hypersthene, with hornblende and biotite also present. Lenses, pods and bands of both mafic and ultramafic rock are common and are generally unfoliated.</div></td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.2 Basal unconformity of the Torridon Group. [NC 2134 2516] ==</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>== Locality 1.2 Basal unconformity of the Torridon Group. [NC 2134 2516] ==</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24060&oldid=prev
Scotfot: /* Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507] */
2015-12-19T08:25:03Z
<p><span dir="auto"><span class="autocomment">Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507]</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 08:25, 19 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l16">Line 16:</td>
<td colspan="2" class="diff-lineno">Line 16:</td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507] ==</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>== Locality 1.1 Lewisian outcrops, Loch Assynt. [NC 2125 2507] ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Park in the lay-by [NC 212 251] alongside the A837 to Lochinver from Skiag Bridge (second lay-by on the left). From the lay-by, walk down to a small east-facing bay on the shore of Loch Assynt, adjacent to an island with two large Scots Pines and many dead trees. The bay [NC 2125 2507] contains a 9m-wide, ESE-trending ultramafic Scourie Dyke, intruded into Lewisian orthogneisses with a westward dipping foliation. The core of the dyke is a fairly fresh, olivine-rich metaclinopyroxene-norite (Tarney, 1973). The host rocks are chiefly pyroxene-bearing felsic gneisses, consisting of quartz, feldspar and hypersthene, with hornblende and biotite also present. Lenses, pods and bands of both mafic and ultramafic rock are common and are generally unfoliated.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Park in the lay-by [NC 212 251] alongside the A837 to Lochinver from Skiag Bridge (second lay-by on the left). From the lay-by, walk down to a small east-facing bay on the shore of Loch Assynt, adjacent to an island with two large Scots Pines and many dead trees. The bay [NC 2125 2507] contains a 9m-wide, ESE-trending ultramafic Scourie Dyke, intruded into Lewisian orthogneisses with a westward dipping foliation<ins style="font-weight: bold; text-decoration: none;">[[Media:P531871.jpg|P531871]]</ins>. The core of the dyke is a fairly fresh, olivine-rich metaclinopyroxene-norite (Tarney, 1973). The host rocks are chiefly pyroxene-bearing felsic gneisses, consisting of quartz, feldspar and hypersthene, with hornblende and biotite also present. Lenses, pods and bands of both mafic and ultramafic rock are common and are generally unfoliated.</div></td></tr>
<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;"><br></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;"><br></td></tr>
<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>== Locality 1.2 Basal unconformity of the Torridon Group. [NC 2134 2516] ==</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>== Locality 1.2 Basal unconformity of the Torridon Group. [NC 2134 2516] ==</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24049&oldid=prev
Scotfot at 22:52, 18 December 2015
2015-12-18T22:52:52Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:52, 18 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l69">Line 69:</td>
<td colspan="2" class="diff-lineno">Line 69:</td></tr>
<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;"><br></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;"><br></td></tr>
<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>==[[References - Geological excursion guide to the North-west Highlands of Scotland|References]] ==</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>==[[References - Geological excursion guide to the North-west Highlands of Scotland|References]] ==</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">{{EGwalks}}</ins></div></td></tr>
<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;"><br></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;"><br></td></tr>
<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>[[Category:2. Northern Highlands]]</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>[[Category:2. Northern Highlands]]</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24045&oldid=prev
Scotfot: /* Locality 1.12 [NC 2372 2408] Outcrops of the Salterella Grit Member and Ghrudaidh Formation. */
2015-12-18T22:30:53Z
<p><span dir="auto"><span class="autocomment">Locality 1.12 [NC 2372 2408] Outcrops of the Salterella Grit Member and Ghrudaidh Formation.</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:30, 18 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l60">Line 60:</td>
<td colspan="2" class="diff-lineno">Line 60:</td></tr>
<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>The less abundant lithofacies comprises distinctive 10–30cm beds of dolomitic grainstones in which the dominant allochems are echinoderm fragments. McKie and Donovan (1992) identified eocrinoid fragments amongst the debris. The grainstones are cross-bedded with E-to NE-directed palaeocurrents and are interpreted as storm event beds.</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>The less abundant lithofacies comprises distinctive 10–30cm beds of dolomitic grainstones in which the dominant allochems are echinoderm fragments. McKie and Donovan (1992) identified eocrinoid fragments amongst the debris. The grainstones are cross-bedded with E-to NE-directed palaeocurrents and are interpreted as storm event beds.</div></td></tr>
<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;"><br></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;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>== Locality 1.12 <del style="font-weight: bold; text-decoration: none;">[NC 2372 2408] </del>Outcrops of the Salterella Grit Member and Ghrudaidh Formation. <del style="font-weight: bold; text-decoration: none;"> </del>==</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>== Locality 1.12 Outcrops of the Salterella Grit Member and Ghrudaidh Formation. <ins style="font-weight: bold; text-decoration: none;">[NC 2372 2408] </ins>==</div></td></tr>
<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>The Fucoid Beds Member is conformably overlain by the Salterella Grit Member, which forms the upper part of the An t-Sròn Formation and marks a return to cross-bedded quartz arenite deposition. The roadside outcrop contains prominent ''Skolithos ''and less conspicuous examples of the body fossil ''Salterella''. The latter is an organism of unknown affinity, but may be a primitive mollusc that produced an agglutinated rather than microcrystalline shell. In hand specimen, it appears as a cone a few milli-metres long that produces dark, circular or v-shaped profiles depending on the section; very occasional 3D specimens are white or black, but the shell is frequently dissolved out leaving distinctive mouldic cavities. ''Salterella ''occurs from the upper part of the Pipe Rock Member through to the base of the Ghrudaidh Formation, but is particularly abundant in the epony-mous member. The genus is stratigraphically restricted to the ''Bonnia– Olenellus ''Biozone. Other shell material is present as small fragments.</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>The Fucoid Beds Member is conformably overlain by the Salterella Grit Member, which forms the upper part of the An t-Sròn Formation and marks a return to cross-bedded quartz arenite deposition. The roadside outcrop contains prominent ''Skolithos ''and less conspicuous examples of the body fossil ''Salterella''. The latter is an organism of unknown affinity, but may be a primitive mollusc that produced an agglutinated rather than microcrystalline shell. In hand specimen, it appears as a cone a few milli-metres long that produces dark, circular or v-shaped profiles depending on the section; very occasional 3D specimens are white or black, but the shell is frequently dissolved out leaving distinctive mouldic cavities. ''Salterella ''occurs from the upper part of the Pipe Rock Member through to the base of the Ghrudaidh Formation, but is particularly abundant in the epony-mous member. The genus is stratigraphically restricted to the ''Bonnia– Olenellus ''Biozone. Other shell material is present as small fragments.</div></td></tr>
<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;"><br></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;"><br></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24042&oldid=prev
Scotfot: /* ==References == */
2015-12-18T22:25:52Z
<p><span dir="auto"><span class="autocomment">==References ==</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:25, 18 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l68">Line 68:</td>
<td colspan="2" class="diff-lineno">Line 68:</td></tr>
<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>Beyond the end of the lay-by, the top of a vogesite (hornblende lamprophyre) sill that intrudes the Ghrudaidh Formation is seen by a culvert. Ten metres farther east is a 5m-thick vogesite sill with a rubbly base, which has been interpreted as the floor thrust of the Achmore Duplex, and the lowest thrust (Sole Thrust) of the Moine Thrust Zone in this area.</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>Beyond the end of the lay-by, the top of a vogesite (hornblende lamprophyre) sill that intrudes the Ghrudaidh Formation is seen by a culvert. Ten metres farther east is a 5m-thick vogesite sill with a rubbly base, which has been interpreted as the floor thrust of the Achmore Duplex, and the lowest thrust (Sole Thrust) of the Moine Thrust Zone in this area.</div></td></tr>
<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;"><br></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;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">== </del>==[[References - Geological excursion guide to the North-west Highlands of Scotland|References]] <del style="font-weight: bold; text-decoration: none;">== </del>==</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>==[[References - Geological excursion guide to the North-west Highlands of Scotland|References]] ==</div></td></tr>
<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;"><br></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;"><br></td></tr>
<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;"><br></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;"><br></td></tr>
<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>[[Category:2. Northern Highlands]]</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>[[Category:2. Northern Highlands]]</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24041&oldid=prev
Scotfot: /* References */
2015-12-18T22:25:25Z
<p><span dir="auto"><span class="autocomment">References</span></span></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:25, 18 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l68">Line 68:</td>
<td colspan="2" class="diff-lineno">Line 68:</td></tr>
<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>Beyond the end of the lay-by, the top of a vogesite (hornblende lamprophyre) sill that intrudes the Ghrudaidh Formation is seen by a culvert. Ten metres farther east is a 5m-thick vogesite sill with a rubbly base, which has been interpreted as the floor thrust of the Achmore Duplex, and the lowest thrust (Sole Thrust) of the Moine Thrust Zone in this area.</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>Beyond the end of the lay-by, the top of a vogesite (hornblende lamprophyre) sill that intrudes the Ghrudaidh Formation is seen by a culvert. Ten metres farther east is a 5m-thick vogesite sill with a rubbly base, which has been interpreted as the floor thrust of the Achmore Duplex, and the lowest thrust (Sole Thrust) of the Moine Thrust Zone in this area.</div></td></tr>
<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;"><br></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;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>== References ==</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>== <ins style="font-weight: bold; text-decoration: none;">==[[</ins>References <ins style="font-weight: bold; text-decoration: none;">- Geological excursion guide to the North-west Highlands of Scotland|References]] == </ins>==</div></td></tr>
<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;"><br></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;"><br></td></tr>
<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;"><br></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;"><br></td></tr>
<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>[[Category:2. Northern Highlands]]</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>[[Category:2. Northern Highlands]]</div></td></tr>
</table>
Scotfot
https://earthwise.bgs.ac.uk/index.php?title=Foreland_succession_of_the_Loch_Assynt_roadside,_North-west_Highlands_-_an_excursion&diff=24040&oldid=prev
Scotfot at 22:12, 18 December 2015
2015-12-18T22:12:30Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
<col class="diff-marker" />
<col class="diff-content" />
<col class="diff-marker" />
<col class="diff-content" />
<tr class="diff-title" lang="en-GB">
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:12, 18 December 2015</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td>
<td colspan="2" class="diff-lineno">Line 1:</td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[File:EGS NWH Cover.jpg|thumbnail|'''Buy the book''' [https://www.edinburghgeolsoc.org/p_sales.html#nwh '''EGS''']. Also available from Amazon]]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[File:EGS NWH Cover.jpg<ins style="font-weight: bold; text-decoration: none;">|200px</ins>|thumbnail|'''Buy the book''' [https://www.edinburghgeolsoc.org/p_sales.html#nwh '''EGS''']. Also available from Amazon]]</div></td></tr>
<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>[[File:EGS_NWH_FIG_011.jpg|thumbnail|Geological map of the Loch Assynt area, after British Geological Survey (2007), showing the localities described in Excursion 1.]]</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>[[File:EGS_NWH_FIG_011.jpg|thumbnail|Geological map of the Loch Assynt area, after British Geological Survey (2007), showing the localities described in Excursion 1.]]</div></td></tr>
<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>[[File:P531871.jpg|thumbnail|Outcrops of Lewisian gneiss on the shore of Loch Assynt at Locality 1.1. (BGS photograph P531871, © NERC)]]</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>[[File:P531871.jpg|thumbnail|Outcrops of Lewisian gneiss on the shore of Loch Assynt at Locality 1.1. (BGS photograph P531871, © NERC)]]</div></td></tr>
</table>
Scotfot