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Arthur's Seat in Edinburgh
Arthur's Seat in Edinburgh
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View along the Highland Boundary Fault from Conic Hill – the topographic ridge is mainly due to the presence of Devonian age conglomerates on the sout
View along the Highland Boundary Fault from Conic Hill – the topographic ridge is mainly due to the presence of Devonian age conglomerates on the southwestern side of the fault and can be traced across Loch Lomond on the islands of Inchcailloch, Torrinch, Creinch and Inchmurrin, to Ben Bowie on the western shore
Altered serpentinite and associated sediments of the Highland Border Complex caught up in the fault zone – exposed on Druim nam Buraich, near Balmaha
Altered serpentinite and associated sediments of the Highland Border Complex caught up in the fault zone – exposed on Druim nam Buraich, near Balmaha
Lower Devonian sandstones and conglomerates of the Inchmurrin Member dipping steeply to the southeast close to the Highland Boundary Fault trace near
Lower Devonian sandstones and conglomerates of the Inchmurrin Member dipping steeply to the southeast close to the Highland Boundary Fault trace near Balmaha