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V.—On the Climate of the Loess Period in Central Europe and the Cause which Produced it

Published online by Cambridge University Press:  01 May 2009

T. F. Jamieson
T. F. Jamieson
Affiliation:
Ellon, Aberdeenshire.
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Extract

Under the name of “Loess” there has been confounded two kinds of deposit which are due to entirely distinct and different causes. One is the fine-grained sediment left by the muddy water of flooded rivers and streams of all sorts; the other is the powdery dust and sand carried by wind, which in dry regions often produces large accumulations of this nature.

Type
Original Articles
Information
Geological Magazine , Volume 7 , Issue 2 , February 1890 , pp. 70 - 73
Copyright
Copyright © Cambridge University Press 1890

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References

page 70 note 1 See Report on Buried Cliff at Sewerby, British Association for 1888 (p. 335).

page 71 note 1 Geol. Mag. Feb. 1883; also, Neues Jahrbuch für Mineralogie, etc., 1889, p. 66.

page 72 note 1 Journ. Geol. Soc. vol. xx. p. 192, 18

page 73 note 1 Quart. Journ. Sci. Jan. 1887, “On the Loess of the Ehine and the Danube.”