Abstract
REFERRING to the map in Croll's “Climate and Time,” which is reproduced in his “Climate and Cosmology” (p. 133), and which traces the ice-flows of the Glacial period from the two sides of the Scandinavian peninsula, it will be seen that the said flow bifurcates in the North Sea, and that the bifurcation is at the position of the Dogger bank. I should be glad to be informed whether this fact has been observed or commented upon in any geological work.
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HOOKER, J. Scandinavian Ice-Flows. Nature 33, 79 (1885). https://doi.org/10.1038/033079c0
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DOI: https://doi.org/10.1038/033079c0
