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A president of the Geological Society from 1815 to 1817, he is best remembered for producing the first geological map of Scotland, published in 1836. 'MacCulloch's Tree', a 40-foot (12 m) high fossil conifer in the Mull lava flows, is named after him. [57] [58] Charles Lyell
Column 4 indicates on which sheet, if any, of the British Geological Survey's 1:50,000 / 1" scale geological map series of Scotland, the fault is shown and named (either on map/s or cross-section/s or both). A handful of BGS maps at other scales are listed too.
Map of the Great Glen Fault and other late Caledonian strike-slip faults in Scotland and northwestern Ireland. The Great Glen Fault is a strike-slip fault that runs through the Great Glen in Scotland. Occasional moderate tremors have been recorded over the past 150 years.
New Geological Map of Scotland. Edinburgh: W. & A.K. Johnston: Blackwood & Sons. Nicol, James (1861). "On the Structure of the North-western Highlands, and the Relation of the Gneiss, Red Sandstone, and Quartzite of Sutherland and Ross-shire". The Quarterly Journal of the Geological Society of London. 17 (1– 2): 85– 113.
The geology of the Isle of Skye in Scotland is highly varied and the island's landscape reflects changes in the underlying nature of the rocks. A wide range of rock types are exposed on the island, sedimentary , metamorphic and igneous , ranging in age from the Archaean through to the Quaternary .
The main geographical divisions of Scotland. The Central Lowlands, sometimes called the Midland Valley or Central Valley, [1] is a geologically defined area of relatively low-lying land in southern Scotland. It consists of a rift valley between the Highland Boundary Fault to the north and the Southern Uplands Fault to the south. [2]
Sketch geological map of Orkney. The geology of the Orkney islands in northern Scotland is dominated by the Devonian Old Red Sandstone (ORS). In the southwestern part of Mainland, this sequence can be seen to rest unconformably on a Moinian type metamorphic basement.
Geological map of the Hebridean terrane showing distribution of Torridonian sediments. The Torridonian is the informal name given to a sequence of Mesoproterozoic to Neoproterozoic sedimentary rocks that outcrop in a strip along the northwestern coast of Scotland and some parts of the Inner Hebrides from the Isle of Mull in the southwest to Cape Wrath in the northeast.