File:Jonathan Run (north-northwest of Fultonham, Ohio, USA) 5 (44319440275).jpg

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(looking upstream)

The boulder-sized sediments along the left bank are fine-grained limestones derived from adjacent outcrops of the Maxville Limestone (Mississippian). Sand-sized fluvial sediments along the right shores of the creek are composed of quartz-lithic sand. Gravel bars along this creek have pebbles and cobbles of Maxville Limestone & siliciclastic sedimentary rocks derived from upstream outcrops of the Waverly Group (Lower Mississippian) & limestone, chert, and shale derived from upstream and uphill Pennsylvanian-aged outcrops. Scarce clasts of crystalline basement rocks from Canada are also present (derived from Ohio's Pleistocene glacial deposits).

Observed fauna in the creek include small water striders, whirligig beetles, Corbicula sp. Asian river clams (= introduced/pest species), a Lasmigona costa freshwater mussel ("fluted shell"), and trails made by Pleurocera semicarinata freshwater snails.

Locality: Jonathan Run, a little upstream from Workman Road bridge, north-northwest of the town of Fultonham, southwestern Muskingum County, eastern Ohio, USA
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Source Jonathan Run (north-northwest of Fultonham, Ohio, USA) 5
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@N05/44319440275 (archive). It was reviewed on 13 October 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

13 October 2019

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current18:08, 13 October 2019Thumbnail for version as of 18:08, 13 October 20193,008 × 2,000 (4.59 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via #flickr2commons

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