The London/Buckinghamshire border - Colne - Harefield Moor
The London, Hillingdon/Buckinghamshire boundary goes northwards along the River Colne
The River Colne flows southwards
Post to the west Tilehouse Lane
The River Colne flows southwards
Post to the west Tilehouse Lane
Post to the south Harefield Moor
Post to the east Harefield Pit and Church Hill
Sites on the London, Hillingdon side of the border
Broadwater.
Access via a derelict area which was the plant area for the gravel pits. The lake is 80 hectares and supports a number of wooded islands. Around the edge are remnants of the original alluvial grasslands and valley alderwoods rising to beech and hornbeam woodland to the west. Broadwater Lake supports important numbers of waterbirds. Since there has been a natural colonisation by typical wetland plants and animals.
Grand Union Canal
Widewater winding hole
River Colne
Is the most natural feature of the site and it has a meandering channel in parts with some pools.
Long Pond
Harefield Pit,
This chalk pit was used as a landfill site and was filled by approximately 30 years ago, it has a strip of dense woodland on steeply undulating raised ground to the south, and a wooded seasonally damp basin to the north. Part of the southern wood is a Site of Special Scientific Interest. The pit provides a key section in the London Basin for a sequence through the Upper Chalk, Reading Beds and London Clay. It is also the only known site for calcareous floral remains in the Reading Beds. It is a disused chalk quarry which has been infilled leaving only the upper faces exposed above ground level.
Sources
Canal plan. web site
Harefield Pit. Wikipedia Web site
Mid Colne Valley. Wikipedia Web site
Post to the east Harefield Pit and Church Hill
Sites on the London, Hillingdon side of the border
Broadwater.
Access via a derelict area which was the plant area for the gravel pits. The lake is 80 hectares and supports a number of wooded islands. Around the edge are remnants of the original alluvial grasslands and valley alderwoods rising to beech and hornbeam woodland to the west. Broadwater Lake supports important numbers of waterbirds. Since there has been a natural colonisation by typical wetland plants and animals.
Grand Union Canal
Widewater winding hole
River Colne
Is the most natural feature of the site and it has a meandering channel in parts with some pools.
Long Pond
Harefield Pit,
This chalk pit was used as a landfill site and was filled by approximately 30 years ago, it has a strip of dense woodland on steeply undulating raised ground to the south, and a wooded seasonally damp basin to the north. Part of the southern wood is a Site of Special Scientific Interest. The pit provides a key section in the London Basin for a sequence through the Upper Chalk, Reading Beds and London Clay. It is also the only known site for calcareous floral remains in the Reading Beds. It is a disused chalk quarry which has been infilled leaving only the upper faces exposed above ground level.
Sources
Canal plan. web site
Harefield Pit. Wikipedia Web site
Mid Colne Valley. Wikipedia Web site
Comments