File:Glacial Till, Glen Ross 0684 (4548480262).jpg

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Description The Trent Hills consist of drumlins which are basically glacial till from the last ice age. As you can see from this old landslide just south of Glen Ross, there is no bedrock. The drumlins sit on a limestone shale substrate and consist mostly of dirt and stones. They are held in place by the trees. Unfortunately, these drumlins make the southern third of Hastings County ideal for sand and gravel pits.
Date
Source Glacial Till, Glen Ross_0684
Author Robert Taylor from Stirling, ON, Canada
Camera location44° 15′ 36.29″ N, 77° 35′ 32.26″ W Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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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 Bobolink at https://flickr.com/photos/24854893@N00/4548480262. It was reviewed on 27 May 2023 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

27 May 2023

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current06:53, 27 May 2023Thumbnail for version as of 06:53, 27 May 20233,456 × 2,304 (5.88 MB)Geo Swan (talk | contribs)Transferred from Flickr via #flickr2commons

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