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词条 Campfield Kettle Hole
释义

  1. Location and natural features

  2. Vegetation

  3. See also

  4. References

  5. External links

{{NOTOC}}{{Infobox SSSI
|name=Campfield Kettle Hole
|aos=Northumberland
|interest=Biological
|gridref={{gbmappingsmall|NT862381}}
|coordinates = {{coord|55.63669|-2.22073|type:landmark_region:GB|display=inline,title}}
|area={{convert|2.92|ha|sigfig=2}}
|notifydate=1969
|enref=1004433
|map=DEFRA MAGIC map
}}Campfield Kettle Hole is the name given to a Site of Special Scientific Interest (SSSI) in north Northumberland, England. The site is thought to be the remains of a kettle hole, a pond formed in the void remaining after a submerged glacial calf block melted. In contemporary times Campfield Kettle Hole is a mix of bog and pond.[1][2]

Location and natural features

Campfield Kettle Hole is situated in the north-east of England, immediately south of the Anglo-Scottish border in the county of Northumberland, some {{convert|0.7|mi}} south of the town of Cornhill-on-Tweed. The pond lies at {{convert|31|m}} above sea level within mildly undulating terrain, and is some {{convert|0.09|mi}} north-south and {{convert|0.22|mi}} east-west. The western end is a permanent pond; the eastern-end is prone to occasional flooding; the remainder of the pond has become peat-filled.[1][2]

The local area has a number of other kettle hole ponds; a second, Barelees Pond, lies {{convert|0.65|mi}} east of Campfield.[1][2]

Vegetation

The kettle hole has deep waterlogged peat soils supporting a carr woodland of birch (Betula sp.) with Scot’s pine (Pinus sylvestris). The woodland floor has bog-mosses (Sphagnum spp.), and hare’s-tail cotton grass (Eriophorum vaginatum) with purple moor-grass (Molinia caerulea) and wavy hair-grass (Deschampsia flexuosa).[2]

The western end of the pond is fringed with yellow iris (Iris pseudacorus), water plantain (Alisma plantago-aquatica) and willow (Salix spp). The perimeter has yellow iris and reed canary-grass (Phalaris arundinacea). The uncommon beetle Agabus uliginosus dispar has been recorded from the wetter areas of the site.[2]

The condition of Campfield Kettle Hole was judged to be unfavourable-recovering in 2013, with previous concerns about tree encroachment settled.[3]

See also

  • List of Sites of Special Scientific Interest in Northumberland

References

1. ^{{cite web| url=http://magic.defra.gov.uk/MagicMap.aspx?startTopic=Designations&activelayer=sssiIndex&query=HYPERLINK%3D%271004433%27|title=MAGIC Map Application - Campfield Kettle Hole|website=DEFRA MAGIC Map|publisher=DEFRA}}
2. ^{{cite web|title=Campfield Kettle Hole SSSI Citation|url=http://www.sssi.naturalengland.org.uk/citation/citation_photo/1004433.pdf|publisher=Natural England}}
3. ^{{cite web|publisher=Natural England|title=Condition of SSSI Units for Site Campfield Kettle Hole|date=26 June 2012|url=https://designatedsites.naturalengland.org.uk/ReportUnitCondition.aspx?SiteCode=S1004433&ReportTitle=Campfield%20Kettle%20Hole%20SSSI}}

External links

  • [https://designatedsites.naturalengland.org.uk/SiteDetail.aspx?SiteCode=S1004307&SiteName=&countyCode=32&responsiblePerson= Natural England] SSSI record for Campfield Kettle Hole

3 : Ponds of Europe|Sites of Special Scientific Interest in Northumberland|Sites of Special Scientific Interest notified in 1969

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