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 2
... deep dales or ravines , some of which are of great beauty , specially where the stream has worked its way through the thickly bedded part of the formation , and has eaten out a narrow road bounded on either side by steep and in some ...
... deep dales or ravines , some of which are of great beauty , specially where the stream has worked its way through the thickly bedded part of the formation , and has eaten out a narrow road bounded on either side by steep and in some ...
Pagina 3
... deep pool below . The moisture and spray are ever wearing away the shale at the base of the cliff , and masses of sand- stone from time to time lose their support and tumble over , and the valley is thus gradually worked farther and ...
... deep pool below . The moisture and spray are ever wearing away the shale at the base of the cliff , and masses of sand- stone from time to time lose their support and tumble over , and the valley is thus gradually worked farther and ...
Pagina 11
... deep below the waters , into which finely divided mud was carried and settled down gently , forming a mass of thinly bedded shale . And when this had gone on for some time the bottom would again begin to rise , and when the water had ...
... deep below the waters , into which finely divided mud was carried and settled down gently , forming a mass of thinly bedded shale . And when this had gone on for some time the bottom would again begin to rise , and when the water had ...
Pagina 28
... deep , narrow , steep - sided limestone gorge , then winding across the flat , and escaping through another narrow cleft in the western limestone wall into the Dove . And here the same explanation applies . The amphitheatre is occupied ...
... deep , narrow , steep - sided limestone gorge , then winding across the flat , and escaping through another narrow cleft in the western limestone wall into the Dove . And here the same explanation applies . The amphitheatre is occupied ...
Pagina 30
... , mostly at high angles , beneath the shales ; the boundary being broken by faults at Deep Dalet and Waterhouses . † * In Map 81 S.E. † In Map 72 N.E. W. Fig . 6 . Section at Apes Tor , 30 THE CARBONIFEROUS LIMESTONE . Page.
... , mostly at high angles , beneath the shales ; the boundary being broken by faults at Deep Dalet and Waterhouses . † * In Map 81 S.E. † In Map 72 N.E. W. Fig . 6 . Section at Apes Tor , 30 THE CARBONIFEROUS LIMESTONE . Page.
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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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