Dorset Downs: Difference between revisions

Coordinates: 50°51′36″N 2°22′40″W / 50.8600°N 2.3777°W / 50.8600; -2.3777
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{{Use dmy dates|date=April 2022}}
[[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 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|The Dorset Downs shown within Dorset (click on image for larger scale)]]{{coord|50.8600|-2.3777|display=title|region:GB_scale:100000}}
[[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">[http://books.google.co.uk/books?id=VLSvQb3TzxkC&pg=PA2&dq=%22dorset+downs%22&hl=en&sa=X&ei=e25cUd2lEsGntAb54IDQCA&ved=0CEsQ6AEwBg#v=onepage&q=%22dorset%20downs%22&f=false ''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>
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==
==Physical geography==
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, 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]].
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>
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 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.
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.
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* [[Rampisham Down]] (219 m)
* [[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]].
* [[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==

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.