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The Gault Clay is a formation of stiff blue clay deposited in a calm, fairly deep water marine environment during the Lower Cretaceous Period (Upper and Middle Albian). It is well exposed in the coastal cliffs at Copt Point in Folkestonemarker, Kentmarker, Englandmarker, where it overlays the Lower Greensand formation,and is found in exposure on the south side of The North Downsmarker and the north side of the South Downsmarker. It is also to be found beneath the scarp of the White Horse Hills, in the Vale of White Horsemarker, in Oxfordshire, England, and on the Isle of Wightmarker where it is known as Blue Slipper. The Gault underlies the chalk beneath the London Basin, generally overlying eroded rocks of Jurassic and Devonian age; the lower Gault is present only below the outer parts of the basin and is absent under central London..

The clay has been used in several locations for making bricks, notably near Wyemarker in Kentmarker.

The Gault Clay often contains numerous phosphatic nodules,some thought to be coprolites and may also contain sand as well as small grains of the mineral glauconite. Crystals of the mineral selenite are fairly common in places, as are nodules of pyrite.

The Gault Clay yields abundant marine fossils, including ammonites (such as Hoplites, Hamites, Euhoplites, Anahoplites, and Dimorphoplites), belemnites (such as Neohibolites), bivalves (such as Birostrina and Pectinucula), gastropods (such as Anchura), solitary corals, fish remains (including shark teeth), scattered crinoid remains, and crustaceans (such as the crab Notopocorystes). Occasional fragments of fossil wood may also be found.

For more detailed information on the fossils found in the Gault Clay, please visit the following websites:

Gault Formation

The Gault Formation consists of the Gault Clay and the Upper Greensand. These represent different facies, with the sandier parts probably being deposited close to the shore and the clay in quieter water further from the source of sediment; both are believed to be shallow-water deposits.

The Gault Formation represents a marine transgression following erosion of the Lower Greensand. It is subdivided into two sections, the Upper Gault and the Lower Gault. The Upper Gault onlaps onto the lower Gault. The Gault Formation thins across the London Platform and then terminates against the Red Chalk just to the south of The Washmarker.

The Gault exposure at Copt Point, which is the type locality for the formation, is 40 m in thickness.


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