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Addlestone
Addlestone (/ˈædəlstən/ or /ædəlstoʊn/) is a town in Surrey, England. It is located approximately 18+1⁄2 miles (30 kilometres) southwest of London. The town is the administrative centre of the Borough of Runnymede, of which it is the largest settlement.
Addlestone is approximately 10 miles (16 kilometres) northeast of Guildford and 18+1⁄2 mi (30 km) southwest of London.
Narrow green buffers separate the town from Weybridge, Chertsey and Ottershaw. There is no precisely defined southern boundary with New Haw.
Addlestone is home to the ancient Crouch Oak tree, under which it is said Queen Elizabeth I picnicked. It also marked the edge of Windsor Forest before it was largely cut down for fields and settlements.
Elevations range between 11 and 40 metres (36 and 131 ft). The maximum is on Row Hill recreation ground, Row Town, Addlestone; a ridge that continues to the northwest of Row Town where it is known as Ongar/Spinney Hill, where Great Grove Farm in its centre also reaches this height; the minimum is by the Thames and along the Woburn Park Stream which is the main distributary of The Bourne the main waterway of the village, a stream rising as the Windle Brook in Windlesham cutting a shallow ravine, flowing past the McLaren Technology Centre and Woodham then passing to the east of the village.
Eminences of the Bagshot Sand stand out above the river most notably the western hills mentioned and Woburn Hill which is 25 metres (82 ft) AOD compared to St Ann's Hill, Chertsey's 61 metres (200 ft), however, is part of the landscape critical to Woburn Park and the private gardens of Woburn Hill.
Major climate changes in Britain causing sea level changes in the last 2.58 million years, with mini Ice Ages, the ice sheets did not extend to Surrey but sand and gravel deposits swept towards the fledgling River Thames were spread in all lower parts. Gravel terraces at various heights on the valley sides are the remnants of successive floodplains, the highest terrace being the oldest and the lowest the youngest. The most prominent terraces mark the former levels of the Thames in north Surrey. Along tributary slopes, a deposit, head, forms the main sediment of latest age. Head comprises angular pieces of rock and soil derived locally from the extensive frost-shattering of rocks and the subsequent movement of this material down valley slopes.
Soil is predominantly "loamy soil with naturally high groundwater". Woburn Hill has "slowly permeable seasonally wet slightly acid but base-rich loamy and clayey soil". New Haw, the southern part of the Addlestone post town and historically a part has "freely draining slightly acid loamy soils"; so does Great Grove Farm. West of the M25 as far as the centre of Ottershaw is a belt of "slightly acid loamy and clayey soils with impeded drainage" soil.
Hub AI
Addlestone AI simulator
(@Addlestone_simulator)
Addlestone
Addlestone (/ˈædəlstən/ or /ædəlstoʊn/) is a town in Surrey, England. It is located approximately 18+1⁄2 miles (30 kilometres) southwest of London. The town is the administrative centre of the Borough of Runnymede, of which it is the largest settlement.
Addlestone is approximately 10 miles (16 kilometres) northeast of Guildford and 18+1⁄2 mi (30 km) southwest of London.
Narrow green buffers separate the town from Weybridge, Chertsey and Ottershaw. There is no precisely defined southern boundary with New Haw.
Addlestone is home to the ancient Crouch Oak tree, under which it is said Queen Elizabeth I picnicked. It also marked the edge of Windsor Forest before it was largely cut down for fields and settlements.
Elevations range between 11 and 40 metres (36 and 131 ft). The maximum is on Row Hill recreation ground, Row Town, Addlestone; a ridge that continues to the northwest of Row Town where it is known as Ongar/Spinney Hill, where Great Grove Farm in its centre also reaches this height; the minimum is by the Thames and along the Woburn Park Stream which is the main distributary of The Bourne the main waterway of the village, a stream rising as the Windle Brook in Windlesham cutting a shallow ravine, flowing past the McLaren Technology Centre and Woodham then passing to the east of the village.
Eminences of the Bagshot Sand stand out above the river most notably the western hills mentioned and Woburn Hill which is 25 metres (82 ft) AOD compared to St Ann's Hill, Chertsey's 61 metres (200 ft), however, is part of the landscape critical to Woburn Park and the private gardens of Woburn Hill.
Major climate changes in Britain causing sea level changes in the last 2.58 million years, with mini Ice Ages, the ice sheets did not extend to Surrey but sand and gravel deposits swept towards the fledgling River Thames were spread in all lower parts. Gravel terraces at various heights on the valley sides are the remnants of successive floodplains, the highest terrace being the oldest and the lowest the youngest. The most prominent terraces mark the former levels of the Thames in north Surrey. Along tributary slopes, a deposit, head, forms the main sediment of latest age. Head comprises angular pieces of rock and soil derived locally from the extensive frost-shattering of rocks and the subsequent movement of this material down valley slopes.
Soil is predominantly "loamy soil with naturally high groundwater". Woburn Hill has "slowly permeable seasonally wet slightly acid but base-rich loamy and clayey soil". New Haw, the southern part of the Addlestone post town and historically a part has "freely draining slightly acid loamy soils"; so does Great Grove Farm. West of the M25 as far as the centre of Ottershaw is a belt of "slightly acid loamy and clayey soils with impeded drainage" soil.