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 3
... bank at the top of each ridge , as at A ; the steep hill - side below is formed of shale , and at the bottom of the valley we have a brook at B running on the top of the grit next below . To this general type all the main ridges and the ...
... bank at the top of each ridge , as at A ; the steep hill - side below is formed of shale , and at the bottom of the valley we have a brook at B running on the top of the grit next below . To this general type all the main ridges and the ...
Pagina 27
... Banks . " A capital summary is given in Conybeare and Phillips ' " Outlines of the Geology of England and Wales , " p . 450. We also gave our reasons for suspecting some such fault in the Memoir on the adjoining Quarter - sheet 81 S.W. ...
... Banks . " A capital summary is given in Conybeare and Phillips ' " Outlines of the Geology of England and Wales , " p . 450. We also gave our reasons for suspecting some such fault in the Memoir on the adjoining Quarter - sheet 81 S.W. ...
Pagina 29
... bank , unless a fault ran between . Fig . 5 . Plan of the Limestone Boundary at Ludwell . Ludwell Mill 60 25 30 * In Map 81 S.E. Black shale . Upper limestone with chert . Lower white limestone . Faults . Bank Top . From Bank Top * to ...
... bank , unless a fault ran between . Fig . 5 . Plan of the Limestone Boundary at Ludwell . Ludwell Mill 60 25 30 * In Map 81 S.E. Black shale . Upper limestone with chert . Lower white limestone . Faults . Bank Top . From Bank Top * to ...
Pagina 30
... Bank Top * to Hartington * there runs a clear line of crags of white limestone , dipping east at 25 ° , and with black shale abutting against them on the west ; the boundary , therefore , for two reasons , must be a fault . This clear ...
... Bank Top * to Hartington * there runs a clear line of crags of white limestone , dipping east at 25 ° , and with black shale abutting against them on the west ; the boundary , therefore , for two reasons , must be a fault . This clear ...
Pagina 42
... bank begins to be covered with huge landslips formed of masses of the Shale Grit which have slid down from the hill top above . They strew the hill - side in vast numbers for the whole distance that the river runs through the shale ...
... bank begins to be covered with huge landslips formed of masses of the Shale Grit which have slid down from the hill top above . They strew the hill - side in vast numbers for the whole distance that the river runs through the shale ...
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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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