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GLACIAL GEOLOGY AND THE PLEISTOCENE EPOCH
New Zealand Geographer, 1948D. S. F., Richard Foster Flint
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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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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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Contributions to the Glacial Geology of Spitsbergen
Quarterly Journal of the Geological Society of London, 1898On June 17th, 1896, the tercentenary of the discovery of Spitsbergen by Barentz, we first sighted the western coast of the great island, the unknown interior of which Sir Martin Conway's expedition had been organized to explore. The sea was strewn with floes, which barred direct approach to the shore, and the incidents of the passage through the ice ...
E. J. Garwood, J. W. Gregory
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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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A Contribution to the Glacial Geology of Tasmania
Quarterly Journal of the Geological Society of London, 1904I. Introduction. The existence of Pleistocene glaciation in Southern Australia has been so often affirmed on unsatisfactory evidence, that the assertion of a recent glaciation in Tasmania has been received with doubt. Two years ago I read through the literature on the glaciation of Tasmania, and came to the conclusion that, except for such ...
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