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Black Down, Dorset
| Field | Value |
|---|---|
| name | Black Down |
| photo | Hardy's Monument - geograph.org.uk - 1022562.jpg |
| photo_caption | Black Down and the Hardy Monument |
| elevation_m | 242 |
| elevation_ref | |
| prominence_m | 78 |
| prominence_ref | |
| parent_peak | Lewesdon Hill |
| listing | Tump (hill) |
| location | Dorset, England |
| range | South Dorset Downs |
| coordinates | |
| grid_ref_UK | SY611876 |
| topo | OS Landranger 194 |
Black Down is a hill on the South Dorset Ridgeway about 2 km north-northeast of the village of Portesham in the county of Dorset, England and around 5 km from the coast.
The treeless summit of Black Down is a popular viewing point, crowned by the 72 foot high Hardy Monument built in 1844 in memory of Vice-Admiral Sir Thomas Masterman Hardy who was Admiral Nelson's Flag Captain at the Battle of Trafalgar.
From the top there are views of the Fleet and Chesil Beach as well as the South Dorset Downs. On a fine day The Needles may be visible, some 50 miles away.
The site is owned by the National Trust.
The heathland area around the monument was in 1984 designated a Site of Special Scientific Interest, when the Nature Conservancy Council decided that the geology of the area was very rare.
Geology
Geologically, Black Down is the western tip of the Bagshot gravel beds. The gravel beds extend to the east as far as London.
The ground around the monument is pitted with various holes and craters. Many of these are dolines or swallow holes. These are formed when rain falls on the highly acidic topsoil. The water increases in acidity as it percolates through the topsoil then dissolves the underlying chalk. Eventually there is nothing but topsoil above the caverns so formed and the familiar shape of a doline is created when the topsoil collapses into the cavern beneath. Dolines are usually shaped like a teardrop cut in half vertically and laid down horizontally. Within 1000 m of the monument there are three dolines which were formed by the chalk being dissolved in a vertical fissure in its structure. These dolines are vertically sided and are shaped like wells. The two which opened up in 1956 are some 100 m deep. The one which opened in 2006 is not quite vertical and its depth is unknown.
Gallery
File:Road from Martinstown to Black Down - geograph.org.uk - 1366394.jpg|Road from Martinstown to Black Down (far right)
References
References
- [http://www.viewfinderpanoramas.org/prominence.html ''Summit Listings by Relative Height''] by Jonathan de Ferranti. Accessed on 26 Mar 2013.
- [http://www.nationaltrust.org.uk/hardy-monument/ ''Monument to Vice-Admiral Hardy''] at www.nationaltrust.org.uk. Accessed on 26 Mar 2013.
- [http://www.dorsetaonb.org.uk/heritage/234-hardy-monument ''Hardy Monument and Black Down''] {{Webarchive. link. (2016-03-04 at www.dorsetaonb.org.uk. Accessed on 26 Mar 2013.)
- [http://www.worldheritagecoast.net/place.aspx?place=4 ''Hardy's Monument''] at www.worldheritagecoast.net. Accessed on 26 Mar 2013.
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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