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Facies Changes versus Sliding: Loch Leven, Argyll
Copyright policy )As is well known the northern face of Garbh Bheinn, which rises from Loch Leven east of Caolasnacon farm, is occupied by a “very obvious asymmetric downfold” of inversion Eilde Quartzite (Hardie, 1952, p. 273; Bailey, 1934, p. 485). The inversion is established by current bedding and is unquestioned. The Eilde Quartzite here floats on Eilde Schist, younger than itself. The occurrence marks the western end of the Kinlochleven Inversion, one of the most remarkable geological structures known to science.
Microsoft Academic Graph classification: Facies Geological structure Paleontology Geomorphology Inversion (geology) Geology Schist Bedding
Geology
Geology
Microsoft Academic Graph classification: Facies Geological structure Paleontology Geomorphology Inversion (geology) Geology Schist Bedding
As is well known the northern face of Garbh Bheinn, which rises from Loch Leven east of Caolasnacon farm, is occupied by a “very obvious asymmetric downfold” of inversion Eilde Quartzite (Hardie, 1952, p. 273; Bailey, 1934, p. 485). The inversion is established by current bedding and is unquestioned. The Eilde Quartzite here floats on Eilde Schist, younger than itself. The occurrence marks the western end of the Kinlochleven Inversion, one of the most remarkable geological structures known to science.