File:Loess Plains (south of Maxwell, Nebraska, USA) 10.jpg
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| Description |
English: The hills in the distance are part of the "Loess Plains" of Nebraska. "Plains" implies a planar or level landscape. The irregular topography is the result of erosion and dissection.
"Loess" refers to wind-blown silt deposits. The silt was usually derived from glacial sediments in ancient rivers that drained melting summertime glaciers during the Pleistocene Ice Age. Some loess deposits consist of silt derived from non-glacial sources. Ancient loess deposits that have been lithified into siltstones are called "paleoloess" or "loessite". Note: "loess" is pronounced "luhss". Info. at: en.wikipedia.org/wiki/Loess |
| Date | |
| Source | https://www.flickr.com/photos/47445767@N05/52032852333/ |
| 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@N05/52032852333. It was reviewed on 27 April 2022 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 12:07, 27 April 2022 | | 3,008 × 1,503 (3.06 MB) | Ser Amantio di Nicolao (talk | contribs) | Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/52032852333/ with UploadWizard |
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