File:EGS NWH FIG 072.jpg
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View east from Cnoc an Leathaid Bhig. The low, dark hill slightly right of centre in the image is Cnoc na Stròine, formed of quartz-syenites of the late suite of the Loch Borralan Pluton. The early suite syenites outcrop in the poorly exposed lower ground around Loch Borralan on the right of the photograph. Some of the main thrusts in the area are indicated (BMT= Ben More Thrust). At a large scale these thrusts are cross-cut by the Loch Borralan Pluton; poor exposure obscures the detailed relations between the early suite syenites and the thrusts. (BGS photograph P693885–P693889, © NERC). Figure 72 from: Goodenough, Kathryn M. and Krabbendam, Maartin (Editors) A geological excursion guide to the North-west Highlands of Scotland. Edinburgh : Edinburgh Geological Society in association with NMS Enterprises Limited, 2011.
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|current||19:53, 19 December 2015||1,431 × 539 (333 KB)||Scotfot||View east from Cnoc an Leathaid Bhig. The low, dark hill slightly right of centre in the image is Cnoc na Stròine, formed of quartz-syenites of the late suite of the Loch Borralan Pluton. The early suite syenites outcrop in the poorly exposed lower gr...|
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