Ullswater is a glacial lake in Cumbria, England, and part of the Lake District National Park. It is the second largest lake in the region by both area and volume, after Windermere. The lake is about long, wide, and has a maximum depth of . Its outflow is the River Eamont, which meets the River Eden at Brougham Castle before flowing into the Solway Firth. The lake forms part of the border between the traditional counties of Cumberland and Westmorland, and is today in the ceremonial county of Cumbria and the unitary authority area of Westmorland and Furness.
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Ullswater is a glacial lake in Cumbria, England, and part of the Lake District National Park. It is the second largest lake in the region by both area and volume, after Windermere. The lake is about long, wide, and has a maximum depth of . Its outflow is the River Eamont, which meets the River Eden at Brougham Castle before flowing into the Solway Firth. The lake forms part of the border between the traditional counties of Cumberland and Westmorland, and is today in the ceremonial county of Cumbria and the unitary authority area of Westmorland and Furness.
==Geography== It is a typical Lake District "ribbon lake", formed after the last ice age by a glacier scooping out the valley floor, which then filled with meltwater. Ullswater was formed by three glaciers. Surrounding hills give it the shape of an extenuated "Z" with three segments or reaches winding through them. For much of its length, Ullswater formed the border between the historic counties of Cumberland and Westmorland.
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).