Bidirectional wave ripple, Nomgon, Mongolia

A paleocurrent or paleocurrent indicator is a geological feature (typically a sedimentary structure) that helps one determine the direction of flowing water in the geologic past. This is an invaluable tool in the reconstruction of ancient depositional environments.[1]

There are two main types of paleocurrent indicators:

Paleocurrents are usually measured with an azimuth, or as a rake on a bedding plane, and displayed with a Rose Diagram to show the dominant direction(s) of flow. This is needed because in some depositional environments, like meandering rivers, the paleocurrent resulting from natural sinuosity has a natural variation of 180 degrees or more.[2]

Below are a partial list of common paleocurrent indicators:


Flute cast, showing paleocurrent to the upper right of pic


Parting lineation, from lower right to upper left; Kayenta Formation, Canyonlands National Park.


The Wikibook Historical Geology has a page on the topic of: Paleocurrents
  1. Prothero, D. R. and Schwab, F., 1996, Sedimentary Geology, pg. 48-51, ISBN 0-7167-2726-9
  2. Miaoa, Xiaodong; Huayu Lua; Zhen Lid; Guangchao Caod (July 2008). "Paleocurrent and fabric analyses of the imbricated fluvial gravel deposits in Huangshui Valley, the northeastern Tibetan Plateau, China". Geomorphology. © 2007 Elsevier B.V. 99 (1-4): 433–442. Bibcode:2008Geomo..99..433M. doi:10.1016/j.geomorph.2007.12.005.

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