Coniston Hall is a former house on the west bank of Coniston Water in the English Lake District. It is recorded in the National Heritage List for England as a designated Grade II* listed building. The house dates from the late 16th century, or possibly earlier. It is built in stone rubble with a slate roof. Part of it is now ruined, part is used as a farmhouse, and another part is used by a sailing club. The hall is owned by the National Trust, but is not open to the public. A privy about 13 metres (43 ft) to the south of the hall is listed at Grade II.

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817 m

Cat Bank

Cat Bank is a hamlet in Cumbria, England.
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924 m

Coniston Water

Coniston Water is a lake in the Lake District in North West England. It is the third largest by volume, after Windermere and Ullswater, and the fifth-largest by area. The lake has a length of 8.7 kilometres (5+3⁄8 mi), a maximum width of 730 metres (800 yd), and a maximum depth of 56.1 m (184 ft 1 in). Its outflow is the River Crake, which drains into Morecambe Bay via the estuary of the River Leven. The lake is in the unitary authority of Westmorland and Furness, the historic county of Lancashire, and the ceremonial county of Cumbria.
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937 m

Brantwood

Brantwood is a historic house museum in Cumbria, England, overlooking Coniston Water. It has been the home to a number of prominent individuals. The house and grounds are administered by a charitable trust, the house serving as a museum dedicated to John Ruskin, one of its final owners. Brantwood is recorded in the National Heritage List for England as a Grade II* listed building, and several buildings on the grounds are also listed.
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953 m

Yewdale Beck

Yewdale Beck is a river in Lake District, Cumbria, England. The Yewdale Beck arises from the confluence of Henfoot Beck and Swallow Scar Beck, as well as other unnamed tributaries east of Wetherlam. The Yewdale Beck first flows in an easterly direction before it turns south-west of the settlement of Lower Tilberthwaite, which it changes again at the northern edge of the town of Coniston to the southeast. It then flows into the Coniston Water. The Yewdale Beck is a Site of Special Scientific Interest. The watercourse is one of the best places for studying stratigraphy and paleogeography of the early Silurian in Great Britain.