Proceedings of the Yorkshire Geological Society, Volume 16Yorkshire Geological Society, 1909 Includes list of members in each vol. |
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Pagina 3
... thickness of 1,000 feet , though here sand dominates over pebbles , are about 300 feet thick in the neigh- bourhood of Trentham and on Cannock Chase , but die out along a line drawn south - east through Leicester . But they appear in ...
... thickness of 1,000 feet , though here sand dominates over pebbles , are about 300 feet thick in the neigh- bourhood of Trentham and on Cannock Chase , but die out along a line drawn south - east through Leicester . But they appear in ...
Pagina 4
... thickness of about 100 feet , the Lower Sandstone is apparently wanting , and the Upper is represented by a soft sandstone measuring about 450 feet . Some differences of opinion exist about its exact limits , but into these we need not ...
... thickness of about 100 feet , the Lower Sandstone is apparently wanting , and the Upper is represented by a soft sandstone measuring about 450 feet . Some differences of opinion exist about its exact limits , but into these we need not ...
Pagina 5
... thickness , so far as I can ascertain , is about 300 feet , but it seldom exceeds half that amount and is often thinner , so that , as it is obviously a transitional formation , we may pass on to the Red Marl . This overlaps even the ...
... thickness , so far as I can ascertain , is about 300 feet , but it seldom exceeds half that amount and is often thinner , so that , as it is obviously a transitional formation , we may pass on to the Red Marl . This overlaps even the ...
Pagina 40
... thickness exposed at Gisburn clearly amounts to over 2,800 feet approximately . The dip is almost constant in direction for about one and a quarter miles and averages 25 ° . There seems to be no chance of repetition of beds . Hence the ...
... thickness exposed at Gisburn clearly amounts to over 2,800 feet approximately . The dip is almost constant in direction for about one and a quarter miles and averages 25 ° . There seems to be no chance of repetition of beds . Hence the ...
Pagina 43
... thickness exposed is about 800 feet , and the shales with limestones are at the base . Further N. there are exposures on the S.W. side of Swinden Moor , where the strata dip E. , N.E. , and almost due N. At Swinden Moor Head there are ...
... thickness exposed is about 800 feet , and the shales with limestones are at the base . Further N. there are exposures on the S.W. side of Swinden Moor , where the strata dip E. , N.E. , and almost due N. At Swinden Moor Head there are ...
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Overige edities - Alles bekijken
Proceedings of the Yorkshire Geological Society, Volume 20 Yorkshire Geological Society Volledige weergave - 1926 |
Proceedings of the Yorkshire Geological Society, Volume 11 Yorkshire Geological Society Volledige weergave - 1891 |
Proceedings of the Yorkshire Geological Society, Volume 18 Yorkshire Geological Society Volledige weergave - 1915 |
Veelvoorkomende woorden en zinsdelen
abundant Ammonites anticlinal Austwick B.Sc Bala bands base Basement Bed black shales Brachiopods Bradford breccia Bunter calcareous Carboniferous Limestone Carboniferous rocks Castletown Chapel-le-Dale character characterised Chonetes Clitheroe Colne corals Craven crinoidal Cyathophyllum Dale deposits Derbyhaven Dibunophyllum district drift DWERRYHOUSE examined Excursion exposed exposures faults fauna feet flaggy fold fossiliferous fossils fragments Genus Geol giganteus Gill glacial Graptolitic gravel Halifax Hall Headingley Hill horizon Horton Flags Ingleborough Ingleton Ingletonian Kendall Keuper knolls Lamplugh Leeds lime limestones and shales Lithostrotion Lower Carter masses Millstone Grit Mountain Limestone Mudstone occur Pateley Bridge pebbles Pendle Pendleside series Plate Poolvash Posidonomya Becheri Proc Productus Professor quarry quartz quartzite Road sand Sandstone Scarlet seen shales Sheffield shell side Silurian species specimens Speeton stones strata Studfold Syringopora thickness thin upper valley well-bedded Wheelton Hind Wolds Worsaw York Yorkshire Geological Society Zaphrentis Enniskilleni zone