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Mid Pleistocene Transition caused by decline in atmospheric CO2
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Nature, 1941
THE year 1840 will always be remembered as one of outstanding importance in the annals of geology. So far as Great Britain is concerned, glacial geology was born in 1840 with the visit to this country of Louis Agassiz. Glasgow will always be associated with this event, for Agassiz attended the tenth meeting of the British Association which was held ...
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THE year 1840 will always be remembered as one of outstanding importance in the annals of geology. So far as Great Britain is concerned, glacial geology was born in 1840 with the visit to this country of Louis Agassiz. Glasgow will always be associated with this event, for Agassiz attended the tenth meeting of the British Association which was held ...
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1958
Contained within the 3rd Edition (1957) of the Atlas of Canada is a map that shows the locations of glacial materials, circa mid-1950s. The extents of existing glaciers and ice caps are shown. The direction of ice movement is illustrated by denoting the trends of drumlins (elongated or oval hills of glacial drift), drumlinoid ridges, flutings, glacial ...
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Contained within the 3rd Edition (1957) of the Atlas of Canada is a map that shows the locations of glacial materials, circa mid-1950s. The extents of existing glaciers and ice caps are shown. The direction of ice movement is illustrated by denoting the trends of drumlins (elongated or oval hills of glacial drift), drumlinoid ridges, flutings, glacial ...
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History of Kansas Glacial Geology
Earth Sciences History, 1984The glacial features of northeastern Kansas have been investigated scientifically for more than a century; out of this study has come the concept of the "Kansan glaciation," which is recognized as an important stage of continental glaciation during the Pleistocene Epoch.
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New York glacial geology, U.S.A.
2004Publisher Summary This chapter reviews that the limit of glaciation in the north-eastern United States lies in Pennsylvania beyond New York's southern border except along the coast of Long Island, in eastern New York, and in the Salamanca Re-entrant, in western New York, where relief is high and the southern limit of glaciation has its most northerly
Donald H. Cadwell, Ernest H. Muller
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Glacial Geology in Northeastern Newfoundland
Geologiska Föreningen i Stockholm Förhandlingar, 1965Abstract In connection with prospecting work the author has investigated glacial striae in northeastern Newfoundland. The striae indicate that the Labrador ice sheet probably affected Newfoundland in early Wisconsin Time. After that the island supported its own ice cap.
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2000
This field guide and proceedings of the seventeenth annual meeting of the Geological Association of New Jersey contains the following papers: Investigations of New Jersey's glacial deposits, 1840-2000 by David P. Harper; Overview of the glacial geology of New Jersey by Scott D.
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This field guide and proceedings of the seventeenth annual meeting of the Geological Association of New Jersey contains the following papers: Investigations of New Jersey's glacial deposits, 1840-2000 by David P. Harper; Overview of the glacial geology of New Jersey by Scott D.
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THE GLACIAL GEOLOGY OF NIDDERDALE
Proceedings of the Yorkshire Geological Society, 1933Introduction. The catchment basin of the River Nidd, from its source on Great Whernside to its termination at Nun Monkton, approximately forty-five miles in length and covering an area of about 450 square miles, presents interesting features of superficial geology which will be considered in some detail.
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Glacial Geology and the Pleistocene Epoch
Nature, 1949PROF. R. F. FLINT'S distinguished work in the broad field of glacial geology has been prominent for a generation, and his book is important for that and for other reasons. It deals with the Pleistocene period from the points of view of a geologist and of glaciologist.
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