Abstract
THERE is in the Astronomical theory of the Ice Age a point of some importance, not mentioned by Sir Robert Ball in his interesting work on this subject, to which I invite the reader's attention. I mean the slowness with which the difference between the length of summer and that of winter is varying in the neighbourhood of its maximum.
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GRAVELAAR, N. The Great Ice Age. Nature 47, 200 (1892). https://doi.org/10.1038/047200a0
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DOI: https://doi.org/10.1038/047200a0
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