Lye Valley: Difference between revisions
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The Lye Valley Nature Park is a secluded area situated east of the Churchill Hospital in Headington, Oxford and has been designated as a Site of Special Scientific Interest (SSSI). The site contains a range of habitats including spring-fed lowland fen, a variety of ponds, and wet woodland with small representations of lowland calcareous grassland, wood pasture and parkland. Lye Valley has one of the best examples of a calcareous valley fen, a nationally rare habitat. The plant and animal species of the Lye Valley fen are thought to have lived there since they colonised the spring areas after the retreat of the last ice age perhaps 8,000 to 10,000 years ago. |
The Lye Valley Nature Park is a secluded area situated east of the Churchill Hospital in Headington, Oxford and has been designated as a Site of Special Scientific Interest (SSSI). The site contains a range of habitats including spring-fed lowland fen, a variety of ponds, and wet woodland with small representations of lowland calcareous grassland, wood pasture and parkland. Lye Valley has one of the best examples of a calcareous valley fen, a nationally rare habitat. The plant and animal species of the Lye Valley fen are thought to have lived there since they colonised the spring areas after the retreat of the last ice age perhaps 8,000 to 10,000 years ago. |
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Revision as of 15:41, 11 April 2011
This article has no links to other Wikipedia articles. (April 2011) |
The Lye Valley Nature Park is a secluded area situated east of the Churchill Hospital in Headington, Oxford and has been designated as a Site of Special Scientific Interest (SSSI). The site contains a range of habitats including spring-fed lowland fen, a variety of ponds, and wet woodland with small representations of lowland calcareous grassland, wood pasture and parkland. Lye Valley has one of the best examples of a calcareous valley fen, a nationally rare habitat. The plant and animal species of the Lye Valley fen are thought to have lived there since they colonised the spring areas after the retreat of the last ice age perhaps 8,000 to 10,000 years ago.
A varied nature trail exists along the stream.
For more information, please see the following link:
http://www.ocv.org.uk/sites.php?id=31
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