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Geological Formation

Boston Hollow

Structural and Tectonic Formations

Boston Hollow is a deep ravine in the town of Ashford, Connecticut, cut along an ancient geologic fault within the Central Maine Terrane of the eastern Connecticut highlands, in a formation called the Bigelow Brook Formation made of high grade pelitic schists and gneisses. The hollow runs almost perfectly straight toward the northeast for nearly a mile, between 100 and 500 feet wide, with its floor at 600 to 630 feet elevation and the surrounding ridges rising to 850 feet and higher; its west wall includes sheer rock faces more than 20 feet tall with concave overhangs. Rather than being cut by a stream or a glacier, the hollow reflects the structural displacement of rock along the fault itself. It lies within Yale-Myers Forest and is crossed by the Nipmuck Trail. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Boston Hollow

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Boston Hollow
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Boston Hollow
Sources
Boston Hollow (Wikipedia)
Lead section
Quote, Lead section
Boston Hollow is a deep ravine in Ashford, Connecticut.
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Wikidata: Boston Hollow
Wikidata Q4947936, class allow-list match (w-wdresolver-0926)View the Source
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