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Klippe

For the style of coin, see Klippe (coin).
Schematic overview of a thrust system. The shaded material is called a nappe. The erosional hole is called a window or fenster. The klippe is the isolated block of the nappe overlying autochthonous material.

A klippe (German for cliff or crag; plural klippen or klippes[1]) is a geological feature of thrust fault terrains. The klippe is the remnant portion of a nappe after erosion has removed connecting portions of the nappe. This process results in an outlier of exotic, often nearly horizontally translated strata overlying autochthonous strata.[2]

  1. ^ Plašienka, D. (2018). "The Carpathian Klippen Belt and types of its klippen – an attempt at a genetic classification". Mineralia Slovaca. 50: 1–24. eISSN 1338-3523.
  2. ^ DiPietro, Joseph A. (December 21, 2012). Landscape Evolution in the United States: An Introduction to the Geography, Geology, and Natural History. Newnes. p. 343. ISBN 9780123978066. Retrieved 10 February 2016.
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