Abstract
FEW men have had better opportunities of examining glacial phenomena than Mr. Whymper, and his explanation of the veined structure is certainly an ingenious one. I venture, however, to doubt whether it can be regarded as generally satisfactory, although, possibly, it might explain some isolated cases.
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BONNEY, T. Veined Structure in Ice. Nature 1, 337 (1870). https://doi.org/10.1038/001337b0
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DOI: https://doi.org/10.1038/001337b0
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