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High Tove

Fell in the Lake District, England


Fell in the Lake District, England

FieldValue
nameHigh Tove
photoHigh_Tove_and_Watendlath.jpg
photo_captionThe slope of High Tove rising behind Watendlath and its tarn
elevation_m515
prominence*c.* 16 m
parent_peakHigh Seat
listingWainwright
locationCumbria, England
rangeLake District, Central Fells
coordinates
grid_ref_UKNY288166
topoOS *Explorer* OL4
mapUnited Kingdom Lake District
map_captionLocation in Lake District, UK

High Tove is a fell in the English Lake District, close to the geographical centre of the Cumbrian hills. It forms part of the watershed between the Derwentwater and Thirlmere catchments, a ridge running broadly north-south.

Topography

Sitting astride the spine of the Central Fells, High Tove is an outlier of High Seat. It is separated from its taller northern neighbour by the Pewits, an extremely boggy depression. The ridge moves on south across further upland marsh towards Ullscarf, passing over the three rocky (and dry) outcrops of Middle Crag, Shivery Knott and Watendlath Fell (summit unnamed on Ordnance Survey maps). Armboth Fell lies to the south east of High Tove, connected to the ridge by a broad heathery saddle.

High Tove covers around one and a half miles of the north-south ridge, which is approximately a mile in width. It is bounded on the west by Watendlath Gill and its main feeder, Blea Tarn Gill. These flow to Watendlath Tarn, a popular beauty spot. The tarn is available for private fishing, being well stocked with trout. It holds a wide selection of flora, including water lilies and is at least 50 ft deep. Fisher and Launchy Gills provide the eastern boundaries of High Tove, flowing north and south around Armboth Fell respectively. Both are feeders of Thirlmere.

Geology

The summit is an island outcrop of the Thirlmere Member in a sea of drift deposits. The Thirlmere Member comprises welded rhyodacitic tuff with breccia.

Ascents

A bridleway provides the pass from Watendlath to Armboth crossing the ridge. Unusually it keeps to the summit rather than a depression, in an attempt to avoid wet ground. A further path runs along the watershed, accompanied by a wire fence. This can prove useful for crossing the worst of the bogs.

Summit

The top has a large cairn, which in Wainwright's words offers a seat to travellers who wish to pour the water out of their boots.

The views are good to the either side, the Helvellyn range nearby to the east and a wide selection of major fells visible on the opposite flank of the ridge. Higher neighbours obstruct the view to north and south.

References

References

  1. Don Blair: ''Exploring Lakeland Tarns'': Lakeland Manor Press (2003): {{ISBN. 0-9543904-1-5
  2. British Geological Survey: 1:50,000 series maps, ''England & Wales Sheet 29'': BGS (1999)
  3. Wainwright, A. (1958). "[[Pictorial Guide to the Lakeland Fells". Westmorland Gazette.
  4. Bill Birkett: ''Complete Lakeland Fells'': Collins Willow (1994): {{ISBN. 0-00-713629-3
  5. Mark Richards: ''The Central Fells'': Collins (2003): {{ISBN. 0-00-711365-X
Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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