The Geology of the Carboniferous Limestone, Yoredale Rocks, and Millstone Grit of North Derbyshire: (Parts of Sheets 88 S. E., 81 N. E., 81 S. E., 72 N. E., 82 N. W., 82 S. W., and 71 N. W.)H.M. Stationery Office, 1887 - 212 pagina's |
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Pagina xiv
... Section across Harthili and Stanton Moors 20. Diagram to explain the Change in the Direction of the throw of a Fault 65 2 A ***** 2016 & 20 69 3 21 25 28 29 36 38 42 44 47 50 54 55 56 64 Page Fig . 21. Section along Wood Brook , near xiv.
... Section across Harthili and Stanton Moors 20. Diagram to explain the Change in the Direction of the throw of a Fault 65 2 A ***** 2016 & 20 69 3 21 25 28 29 36 38 42 44 47 50 54 55 56 64 Page Fig . 21. Section along Wood Brook , near xiv.
Pagina 2
... direction being much more gentle . The upheaval has been greatest in the north of Derbyshire , where a large dome - shaped mass of Moun- tain Limestone has been brought to the surface , from which the beds slope away , gently to the ...
... direction being much more gentle . The upheaval has been greatest in the north of Derbyshire , where a large dome - shaped mass of Moun- tain Limestone has been brought to the surface , from which the beds slope away , gently to the ...
Pagina 3
... direction of the dip , and often at nearly the same angle , and ending on the other side in a sharp cliff or " edge , " below which is a broad valley hollowed out in the underlying beds of softer shale . The stream at the bottom of this ...
... direction of the dip , and often at nearly the same angle , and ending on the other side in a sharp cliff or " edge , " below which is a broad valley hollowed out in the underlying beds of softer shale . The stream at the bottom of this ...
Pagina 12
... direction from the centre of the mass , and pass out of sight on all sides beneath the Yoredale Rocks ; these latter are overlaid by the Millstone Grit , but the belt of them , which parts the limestone from the Grits , varies very much ...
... direction from the centre of the mass , and pass out of sight on all sides beneath the Yoredale Rocks ; these latter are overlaid by the Millstone Grit , but the belt of them , which parts the limestone from the Grits , varies very much ...
Pagina 13
... direction till we reach a long line of fault , also ranging north and south by Marple , Disley , Jenkin Chapel , Forest Chapel down to Wetley Rocks , which has been named " The Anticlinal Fault " ( see Section , Sheet 18 ) . Crossing ...
... direction till we reach a long line of fault , also ranging north and south by Marple , Disley , Jenkin Chapel , Forest Chapel down to Wetley Rocks , which has been named " The Anticlinal Fault " ( see Section , Sheet 18 ) . Crossing ...
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Overige edities - Alles bekijken
The Geology of the Carboniferous Limestone, Yoredale Rocks, and Millstone ... Alexander Henry Green Volledige weergave - 1887 |
Veelvoorkomende woorden en zinsdelen
50 fathoms Alport anticlinal Ashover Bakewell Bamford Edge black shales Boulder brook Carboniferous Castleton caulk Chatsworth Grit chert Chrome Hill clay cliff Clough coal coarse Crich Cromford crosses Dale Derbyshire Derwent district Drift east Edale Edge escarpment Eyam Farey fathoms depth fault feet thick formed FOSSILS galena Geology gritstone ground Hathersage Hill Hucklow junction Kinder Grit Kinder Scout Grit lode Longshaw Grit M'Coy mass massive Matlock Matlock Bank Memoir mile Millstone Grit mineral mines Moor Mountain Limestone nearly north-east north-west outcrop outlier pebbles Penine Phil Pilkington pipe PROF quarry Rake ranging river Rough Rock Rowsley sandstone scrins seen shaft Shale Grit side Sough south-east Staffordshire stone Stoney Middleton stream thickly bedded thin Tideswell toadstone traced valley white limestone Wirksworth yards Yoredale Rocks Yoredale Sandstones Yoredale Shale دو وو
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