# Gibson Knott

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Fell in the Lake District, Cumbria, England

Gibson Knott Highest point Elevation 422 m (1,385 ft) Prominence c. 10 m Parent peak Calf Crag Listing Wainwright Coordinates 54°28′47″N 3°03′09″W / 54.47986°N 3.05253°W / 54.47986; -3.05253 Geography Gibson Knott Location in Lake District, UK Location Cumbria, England Parent range Lake District, Central Fells OS grid NY319099 Topo map OS Explorer OL5, OL7

**Gibson Knott** is a [fell](/source/Fell) in the English [Lake District](/source/Lake_District), an intermediate height on the ridge between Greenburn and Far Easedale in the [Central Fells](/source/Central_Fells).

## Topography

The spine of the Central Fells runs on a north–south axis with the highpoint at [High Raise](/source/High_Raise_(Langdale)). A complex system of daleheads to the east of this apex resolves itself into [Calf Crag](/source/Calf_Crag), a broad-topped ridge featuring a number of rocky tops. This ridge then splits into two arms about the head of Greenburn, the southern branch running on to Gibson Knott and [Helm Crag](/source/Helm_Crag).

Between Calf Crag and Helm Crag the ridge narrows to perhaps a hundred yards in width, gradually curving to the south east on its one and a half mile course. There are several tops on this section, Gibson Knott being halfway along.

The southern face above Far Easedale is rocky, Horn Crag being the principal feature. The northern side drops more gradually to the upper gathering grounds of Greenburn Bottom. There is little loss of height going westward from the summit before the climb to Calf Crag begins on a broadening ridge. Between Gibson Knott and Helm Crag lies the depression of Bracken Hause at around 1,100 ft.

## Geology

The summit knolls are laminated [volcaniclastic](/source/Volcaniclastic) [claystone](/source/Claystone) and [siltstone](/source/Siltstone) of the Esk Pike Formation. The remainder of the ridge top is composed of [dacitic](/source/Dacitic) [lapilli tuff](/source/Lapilli_tuff).[1] There is no history of mining within the area of the fell.

## Summit

There being a couple of rocky knolls of similar height the summit point could be debated, but custom and practice has resulted in a [cairn](/source/Cairn) on the western outcrop.[2][3] There is an all round view although perhaps not as expansive as could be expected from the centre of the District.It can be improved slightly by moving east along the ridge.[2][3]

## Ascents

The fell is most commonly climbed as part of a circuit of Greenburn following a good path, but ascents from Grasmere via either flank of Bracken Hause are also possible.[2][3]

## References

1. **[^](#cite_ref-BGS_1-0)** British Geological Survey: 1:50,000 series maps, *England & Wales Sheets 29, 38*: BGS (1999)

1. ^ [***a***](#cite_ref-wainwright_2-0) [***b***](#cite_ref-wainwright_2-1) [***c***](#cite_ref-wainwright_2-2) [Wainwright, A](/source/Alfred_Wainwright) (1958). *[A Pictorial Guide to the Lakeland Fells](/source/Pictorial_Guide_to_the_Lakeland_Fells), Book 3 The Central Fells*. Westmorland Gazette.

1. ^ [***a***](#cite_ref-richards_3-0) [***b***](#cite_ref-richards_3-1) [***c***](#cite_ref-richards_3-2) Mark Richards: *The Central Fells*: Collins (2003): [ISBN](/source/ISBN_(identifier)) [0-00-711365-X](https://en.wikipedia.org/wiki/Special:BookSources/0-00-711365-X)

v t e Wainwright's Central Fells Armboth Fell Bleaberry Fell Blea Rigg Calf Crag Eagle Crag Gibson Knott Grange Fell Great Crag Harrison Stickle Helm Crag High Raise High Rigg High Seat High Tove Loft Crag Loughrigg Fell Pavey Ark Pike of Stickle Raven Crag Sergeant Man Sergeant's Crag Silver How Steel Fell Tarn Crag Thunacar Knott Ullscarf Walla Crag Full list of Wainwrights by area

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Adapted from the Wikipedia article [Gibson Knott](https://en.wikipedia.org/wiki/Gibson_Knott) by Wikipedia contributors ([contributor history](https://en.wikipedia.org/wiki/Gibson_Knott?action=history)). Available under [Creative Commons Attribution-ShareAlike 4.0 International](https://creativecommons.org/licenses/by-sa/4.0/). Changes may have been made.