Dorset Downs: Difference between revisions

Coordinates: 50°51′36″N 2°22′40″W / 50.8600°N 2.3777°W / 50.8600; -2.3777
From Wikipedia, the free encyclopedia
Content deleted Content added
m category
Citation bot (talk | contribs)
Misc citation tidying. | Use this bot. Report bugs. | Suggested by AManWithNoPlan | #UCB_CommandLine
 
(61 intermediate revisions by 30 users not shown)
Line 1: Line 1:
{{Use dmy dates|date=April 2022}}
[[Image:Dorset geology.png|thumb|300px|The Dorset Downs shown within Dorset]]
[[Image:Dorset downs.jpg|thumb|250px|The top of the downs from above [[Cerne Abbas]], looking south east towards the [[River Piddle]] valley]]
[[Image:Dorset geology.png|thumb|250px|Map of Dorset, including the Dorset Downs, showing the geology]]{{coord|50.8600|-2.3777|display=title|region:GB_scale:100000}}
The '''Dorset Downs''' are an area of [[chalk]] [[downland]] in the centre of the county [[Dorset]] in south west [[England]]. The downs are the most western part of a larger [[chalk formation]] which also includes (from west to east) [[Cranborne Chase]], [[Salisbury Plain]], [[Hampshire Downs]], [[Chiltern Hills]], [[North Downs]] and [[South Downs]].<ref name="UES">[https://books.google.com/books?id=VLSvQb3TzxkC&dq=%22dorset+downs%22&pg=PA2 ''Uplift, Erosion and Stability: Perspectives on Long-term Landscape Development''] ed. by Smith, Bernard J., Whalley Wilfred B. and Warke Patricia A. (1999), Geological Society Special Publication No. 162, Bath. Accessed on 3 Apr 2013.</ref>


==Physical geography==
The '''Dorset Downs''' are an area of [[Chalk]] [[downland]] in the centre of the county [[Dorset]] in south west [[England]]. The downs are the most western part of a larger [[Chalk Formation]] which includes (from West to East) [[Cranborne Chase]], [[Salisbury Plain]], [[Hampshire Downs]], [[Chiltern Hills]], [[North Downs]] and [[South Downs]].
The Dorset Downs are bounded on the north, along the steep [[escarpment|scarp]] face, by the [[Blackmore Vale]], a large [[clay]] and [[limestone]] [[valley]]. On the east, the Downs were once, thousands of years ago, continuous with Cranborne Chase, but the [[River Stour, Dorset|River Stour]] now cuts a valley between them,{{Dubious|Defies laws of Physics. Gravity powered River Stour cannot cut upwards. River must predate uplift.|date=February 2022}}{{Citation needed|date=February 2022}} which is the location of [[Blandford Forum]] and the eastern boundary of the downs. From the northern scarp face, the hills dip gently southwards before the chalk disappears beneath the [[Bagshot Beds]] which form the heathlands of the county, between [[Dorchester, Dorset|Dorchester]] and [[Wareham, Dorset|Wareham]]. South of the [[River Frome, Dorset|River Frome]], the chalk reappears in a narrower strip, forming coastal cliffs east of [[Weymouth, Dorset|Weymouth]] and, further east, the steep ridge of the [[Purbeck Hills]]. This southerly strip of the visible chalk (sometimes referred to as the '''South Dorset Downs''' or '''South Dorset Ridgeway''') continues westwards behind Weymouth, and rejoins the main body of the downs at their western extremity at [[Eggardon Hill]]. In the west the chalk dips down under [[marl]].


Together with Cranborne Chase, the Dorset Downs have been designated as [[National Character Area]] 134 by [[Natural England]], the UK Government's advisor on the natural environment. In Dorset this area is bounded by the [[Dorset Heaths]] and [[Weymouth Lowlands]] to the south, the [[Marshwood and Powerstock Vales]] to the west and the [[Blackmore Vale]] to the north.<ref name="NCA134">[http://www.naturalengland.org.uk/Images/jca134_tcm6-5480.pdf ''Dorset Downs and Cranborne Chase''] at www.naturalengland.org.uk. Accessed on 3 Apr 2013.</ref>
The Dorset Downs are bounded on the north, along the steep [[scarp]] face, by the [[Blackmore Vale]], a large [[clay]] and [[limestone]] [[valley]]. On the east the Downs would once, thousands of years ago, have been continuous with Cranborne Chase, but the [[River Stour, Dorset|River Stour]] now cuts a valley between them, which is the location of [[Blandford Forum]] and the eastern boundary of the downs. The hills dip gently southwards down to the [[River Frome, Dorset|River Frome]] at [[Dorchester, Dorset|Dorchester]], south of which is a narrow band of [[Purbeck Limestone]] along the [[English Channel]] [[coast]]. In the west the chalk dips down under [[Marl]].


The main land uses on the downs are [[arable land|arable]] [[agriculture]], [[woodland]] and [[calcareous grassland]], a [[habitat (ecology)|habitat]] which is growing as farmers are encouraged to [[set-aside|set aside]] land with [[agricultural subsidy|subsidies]]. Chalk is a rough rock and the Dorset Downs hold a large [[water table]] which acts as a [[reservoir (water)|reservoir]] of drinking water for much of the county. This property of chalk also means there are many seasonal rivers, called [[winterbourne (stream)|winterbourne]]s, that flow depending upon the level of the water table.
[[Image:Dorset downs.jpg|thumb|The top of the downs from above [[Cerne Abbas]] looking south east towards the [[River Piddle]] valley]]


== Hills ==
The main land uses on the downs are as [[arable land|arable]] [[agriculture]], [[woodland]] and [[calcareous grassland]], a [[habitat (ecology)|habitat]] which is growing as farmers are encouraged with [[set-aside]] [[agricultural subsidy|subsidies]]. Chalk is a rough rock and the Dorset Downs hold a large [[water table]] which acts as a [[reservoir (water)|reservoir]] of drinking water for much of the county. This property of chalk also means there are many seasonal rivers, called [[winterbourne (stream)|winterbourne]]s, that flows depending upon the level of the water table.
* [[Bulbarrow Hill]] (274 m), site of Rawlsbury camp and the highest hill in the Downs.
* [[Telegraph Hill, Dorset|Telegraph Hill]] (267 m)
* [[Lyscombe Hill]] (262 m)
* [[Watts Hill, Dorset|Watts Hill]] (261 m)
* [[Bell Hill, Dorset|Bell Hill]] (258 m)
* [[Eggardon Hill]] (252 m), also the western extremity of the [[South Dorset Downs]]
* [[Toller Down]] (252 m)
* [[Ball Hill, Dorset|Ball Hill]] (251 m)
* [[Dogbury Hill]] (248 m)
* [[Beaminster Down]] (244 m)
* [[Shillingstone Hill]] (223 m), a densely wooded scarp face with a large quarry.
* [[Rampisham Down]] (219 m)
* [[Hambledon Hill]] (192 m) and [[Hod Hill]] (143 m), two outliers of [[Cranborne Chase]], separated from the Downs by the [[River Stour, Dorset|River Stour]].


== Fauna ==
The downs are the native home to the [[Dorset Down]] [[sheep]].


==Places of interest==
==Places of interest==
* [[Allsaints school]]
* [[Blandford Forest]]
* [[Blandford Forest]]
* [[Bulbarrow Hill]], including Rawlsbury camp.
* [[Dorsetshire Gap]], a steep valley.
* [[River Cerne|Cerne valley]], including [[Cerne Abbas Giant]].
* [[River Cerne|Cerne valley]], including [[Cerne Abbas Giant]].
* [[Dorsetshire Gap]], a steep valley.
* [[Hambledon Hill]] and [[Hod Hill]], two hills cut off from the downs in the Blackmore Vale.
* [[Milton Abbas]], 18th-century planned estate village and museum.
* [[Minterne Magna]], ''Rhododendron'' garden at Minterne House.
* [[Nettlecombe Tout]] hill fort.
* [[Nettlecombe Tout]] hill fort.
* [[Ringmoor]] settlement and field system.
* [[Ringmoor]] settlement and field system.
* [[Shillingstone Hill]], a densely wooded scarp face with a large quarry.


==External links==
==See also==
* [[Bowerchalke]] - geological profile of a Lower Greensand [[Inliers and outliers (geology)|inlier]] on the chalklands of Cranborne Chase
* [http://www.steinsky.me.uk/special:search.php?key=Dorset_Downs Photographs of the downs]

== References ==
{{Reflist}}


[[Category:Hills of Dorset]]
[[Category:Hills of Dorset]]
[[Category:Geography of Dorset]]
[[Category:Natural regions of Dorset]]
[[Category:Geology of England]]
[[Category:Geology of Dorset]]

Latest revision as of 00:13, 17 March 2023

The top of the downs from above Cerne Abbas, looking south east towards the River Piddle valley
Map of Dorset, including the Dorset Downs, showing the geology

50°51′36″N 2°22′40″W / 50.8600°N 2.3777°W / 50.8600; -2.3777

The Dorset Downs are an area of chalk downland in the centre of the county Dorset in south west England. The downs are the most western part of a larger chalk formation which also includes (from west to east) Cranborne Chase, Salisbury Plain, Hampshire Downs, Chiltern Hills, North Downs and South Downs.[1]

Physical geography[edit]

The Dorset Downs are bounded on the north, along the steep scarp face, by the Blackmore Vale, a large clay and limestone valley. On the east, the Downs were once, thousands of years ago, continuous with Cranborne Chase, but the River Stour now cuts a valley between them,[dubious ][citation needed] which is the location of Blandford Forum and the eastern boundary of the downs. From the northern scarp face, the hills dip gently southwards before the chalk disappears beneath the Bagshot Beds which form the heathlands of the county, between Dorchester and Wareham. South of the River Frome, the chalk reappears in a narrower strip, forming coastal cliffs east of Weymouth and, further east, the steep ridge of the Purbeck Hills. This southerly strip of the visible chalk (sometimes referred to as the South Dorset Downs or South Dorset Ridgeway) continues westwards behind Weymouth, and rejoins the main body of the downs at their western extremity at Eggardon Hill. In the west the chalk dips down under marl.

Together with Cranborne Chase, the Dorset Downs have been designated as National Character Area 134 by Natural England, the UK Government's advisor on the natural environment. In Dorset this area is bounded by the Dorset Heaths and Weymouth Lowlands to the south, the Marshwood and Powerstock Vales to the west and the Blackmore Vale to the north.[2]

The main land uses on the downs are arable agriculture, woodland and calcareous grassland, a habitat which is growing as farmers are encouraged to set aside land with subsidies. Chalk is a rough rock and the Dorset Downs hold a large water table which acts as a reservoir of drinking water for much of the county. This property of chalk also means there are many seasonal rivers, called winterbournes, that flow depending upon the level of the water table.

Hills[edit]

Fauna[edit]

The downs are the native home to the Dorset Down sheep.

Places of interest[edit]

See also[edit]

  • Bowerchalke - geological profile of a Lower Greensand inlier on the chalklands of Cranborne Chase

References[edit]

  1. ^ Uplift, Erosion and Stability: Perspectives on Long-term Landscape Development ed. by Smith, Bernard J., Whalley Wilfred B. and Warke Patricia A. (1999), Geological Society Special Publication No. 162, Bath. Accessed on 3 Apr 2013.
  2. ^ Dorset Downs and Cranborne Chase at www.naturalengland.org.uk. Accessed on 3 Apr 2013.