File:Small landslide (Roaring Run, Warren County, Ohio, USA) 6 (45456449122).jpg

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In geology, "landslides" are referred to as mass wasting. There are many specific types of mass wasting including mudflows, debris flows, earth flows, rock falls, debris falls, rock slides, debris slides, lahars, avalanches, solifluction, slump, and creep.

This small landslide occurred on a mostly non-vegetated, moderately steep creek bank (just off to the right of the picture). The creek cut consists of weathered shales and some thin limestone beds of the Upper Ordovician Waynesville Formation. Waynesville shales are famous for weathering into soft, clayey "butter beds". Landslides are more likely to occur on slopes having such materials.

Locality: creek cut along Roaring Run, just west of the western end of Caesar Creek Lake's emergency spillway, Caesar Creek Lake State Park, northeastern Warren County, southwestern Ohio, USA (~vicinity of 39° 28' 41.63" North latitude, 84° 03' 46.83" West longitude)
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Source Small landslide (Roaring Run, Warren County, Ohio, USA) 6
Author James St. John

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This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/45456449122 (archive). It was reviewed on 7 November 2018 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

7 November 2018

James St. John

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current00:30, 7 November 2018Thumbnail for version as of 00:30, 7 November 20184,000 × 3,000 (9.67 MB)Lu Brito (talk | contribs)Transferred from Flickr via #flickr2commons

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