File:Glacially-striated granite (Cadillac Mountain Granite, Silurian-Devonian boundary times, ~419 Ma; summit of South Bubble, Acadia National Park, Maine, USA) 4.jpg

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English: Glaciers are rivers of ice. Ice is a mineral (H2O) and glacial ice is a rock. Despite being solid, ice does flow under certain conditions at the Earth’s surface. Occasionally, Earth experiences Ice Ages, during which extensive ice sheets cover and move over significant portions of the Earth’s surface. As ice moves over landmasses, it erodes underlying rocks and picks up small to large pieces of debris. This debris accumulates at the base of the ice sheet and scrapes bedrock as the glacier moves, resulting in glacial scratches (glacial striations) (= thin scratch lines on rock) and glacial grooves (= large channels incised in rock).

The Late Pleistocene glacial striations seen here are developed on a granite surface atop a roche moutonnée in coastal Maine. The rock itself is part of the Cadillac Mountain Granite, a large pluton dating to about 419 million years ago.

Locality: summit of South Bubble (a roche moutonnée), Acadia National Park, Mt. Desert Island, southern-coastal Maine, USA
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Source https://www.flickr.com/photos/47445767@N05/50603374713/
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/50603374713. It was reviewed on 18 November 2020 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

18 November 2020

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current00:59, 18 November 2020Thumbnail for version as of 00:59, 18 November 20203,008 × 2,000 (5.53 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/50603374713/ with UploadWizard

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