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Geological Formation

Sihl Valley

Valleys

The Sihl Valley, known in German as Sihltal, is a river valley in the Horgen district of the canton of Zurich in Switzerland, most commonly used to mean the lower valley southwest of the city of Zurich. It was carved as the left moraine of an Ice Age glacier, and Lake Zurich now occupies the bed left behind by that glacier; the valley is drained by the 68 kilometer Sihl river, which rises in the canton of Schwyz. The valley is heavily wooded in its lower reaches, home to the Sihlwald, the largest remaining deciduous forest on the Swiss Plateau, and near its upper end, in the district of Einsiedeln, lies the 8.5 kilometer lake Sihlsee. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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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: Sihl Valley

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: Sihl Valley
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Sources
Sihl Valley (Wikipedia)
Wikidata: Sihl Valley
Wikidata Q682634, class allow-list match (w-wdresolver-0926)View the Source
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