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- W2011998472 abstract "Last summer (1934) I found several pieces of a brownish-red, brick-like rock in an inter-Glacial moraine deposit in Iceland. This find, it is believed, furnishes evidence for a Pleistocene thermal activity in that island. The present-day thermal activity in Iceland is unequalled in intensity and extent. On the accompanying map (Fig. 1) all known localities of hot springs have been plotted, and in order to give a better idea of the proportions, the little square in which the legend of the map is printed has been drawn so as to represent the area of Yellowstone National Park on exactly the same scale. Since the intensity of the thermal activity is not less in Iceland than in Yellowstone, it is readily understood that the hot springs of Iceland are of great geologic importance. They are responsible for a large number of extensive deposits of chlorides, sulfates, and of native sulfur, as well as silica sinter, and last but not least, they have over large areas acted on the adjacent rocks and transformed them into clay-like substances. A question immediately presenting itself to the geologist is therefore the antiquity of this impressive thermal activity. Can it be traced farther back than those thousand and some years constituting the written history of Iceland? We do know that the lifetime of the individual springs varies considerably. Several of the voluminous alkaline springs are at least 1000 years old, but several examples are also known of springs which came into existence and entirely disappeared in less than one year." @default.
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- W2011998472 date "1935-01-01" @default.
- W2011998472 modified "2023-10-05" @default.
- W2011998472 title "Vestige of a Pleistocene thermal activity in Iceland" @default.
- W2011998472 doi "https://doi.org/10.1029/tr016i001p00284-2" @default.
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