Sandgate Formation
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Sandgate Formation
The Lower Greensand Group is a geological unit present across large areas of Southern England. It was deposited during the Aptian and Albian ages of the Early Cretaceous. It predominantly consists of sandstone and unconsolidated sand that were deposited in shallow marine conditions. Lithology The Lower Greensand typically comprises loose, unconsolidated sandstone (termed rubblestone/rubble in construction) and sands of varying grain size with subordinate amounts of siltstones, mudstones (containing smectites and similar) and limestones. The name "greensand" is derived from the presence of the green coloured mineral glauconite, which forms in shallow marine conditions. In the Weald of East Sussex the lowermost part of the group is recognised by green glauconitic clays with a basal bed of phosphate nodules. These clays are overlain by green sandy clays and silts and finally homogeneous fine grained sands.Lake, R.D. & Shepard-Thorn, E.R. (1987) ''Geology of the country around Ha ...
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Dryhill
Dryhill is a small hamlet in the Sevenoaks (district), Sevenoaks district, in the county of Kent, England. Location It is about two miles away from the large town of Sevenoaks, located near the A25 road between Sevenoaks and Sundridge, Kent, Sundridge. Transport For transport there is the Sevenoaks railway station and the A25 road, the M25 motorway, M20 motorway and the M26 motorway nearby. Local Nature Reserve The Dryhill Local Nature Reserve based on an old ragstone quarry at the edge of the village covers some 20 hectares ( ). The quarry is also a Geological interest listed Site of Special Scientific Interest. It is no longer managed by Kent County Council, but remains open as a Country Park and picnic area. References

* A-Z Great Britain Road Atlas (page 181) Hamlets in Kent Sevenoaks District Country parks in Kent, Dryhill Picnic Site Local Nature Reserves in Kent Sites of Special Scientific Interest in Kent, Allington Quarry {{Kent-geo-stub ...
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