Hostname: page-component-848d4c4894-m9kch Total loading time: 0 Render date: 2024-06-09T15:52:25.452Z Has data issue: false hasContentIssue false
  • English
  • Français

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.
Get access Rights & Permissions [Opens in a new window]

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

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

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.”