landscapes of assynt
TRANSCRIPT
Landscapes of Assynt
Assynt Geology in a nutshell at Knockan Crag
Moine rocks
Durness Limestone
Salterella GritFucoid Beds
Pipe Rock
Basal QuartziteTorridonian SandstoneLewisian Gneiss
Knockan Crag
The Moine Thrust
Moine Schist
Cambrian Limestone
Mylonite
View from the top of Knockan Crag
Suliven
The Torridonian Sandstone peak of Suliven
Stac Pollaidh
Composed of Torridonian Sandstone and Conglomerate deposited in rivers 1000 million years ago
The Quartzite capped nunatak of Quinag
Quinag and Loch Assynt
Conival from Inchnadamph
The Traligill Valley
A dry valley. (Unless heavy rain). Dark grey limestone cliff to the north gently sloping pale limestone to the south with limestone pavement. The slope is a thrust plane, the older dark grey limestone has been thrust over the younger paler limestone. The river follows the line of this weakness even underground.
Dry Waterfall in the Traligill
Achmelvich Beach