The Gault Formation is a geological formation of stiff blue

clay Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...

deposited in a calm, fairly deep-water marine environment during the Lower Cretaceous Period (Upper and Middle

Albian The Albian is both an age of the geologic timescale and a stage in the stratigraphic column. It is the youngest or uppermost subdivision of the Early/Lower Cretaceous Epoch/ Series. Its approximate time range is 113.0 ± 1.0 Ma to 100.5 ± 0 ...

). It is well exposed in the coastal cliffs at Copt Point in Folkestone,

Kent Kent is a county in South East England and one of the home counties. It borders Greater London to the north-west, Surrey to the west and East Sussex to the south-west, and Essex to the north across the estuary of the River Thames; it faces ...

England England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe b ...

, where it overlays the

Lower Greensand The Lower Greensand Group is a geological unit present across large areas of Southern England. It was deposited during the Aptian and Albian stages of the Early Cretaceous. It predominantly consists of sandstone and unconsolidated sand that were ...

formation, and underlies the

Upper Greensand Formation The Upper Greensand Formation is a Cretaceous formation of Albian to Cenomanian in age, found within the Wessex Basin and parts of the Weald Basin in southern England. It overlies the Gault Clay and underlies the Chalk Group. It varies in thick ...

. 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 etymology of the name is uncertain and probably of local origin.

Distribution

It is found in exposure on the south side of the North Downs and the north side of the South Downs. It is also to be found beneath the scarp of the

Berkshire Downs The Berkshire Downs are a range of chalk downland hills in South east England split between the counties of Berkshire and Oxfordshire. They are part of the North Wessex Downs Area of Outstanding Natural Beauty. The western parts of the downs ...

, in the Vale of White Horse, in Oxfordshire, England, and on the

Isle of Wight The Isle of Wight ( ) is a Counties of England, county in the English Channel, off the coast of Hampshire, from which it is separated by the Solent. It is the List of islands of England#Largest islands, largest and List of islands of England#Mo ...

where it is known as Blue Slipper. Gault underlies the chalk beneath the

London Basin The London Basin is an elongated, roughly triangular sedimentary basin approximately long which underlies London and a large area of south east England, south eastern East Anglia and the adjacent North Sea. The basin formed as a result of compre ...

, generally overlying eroded rocks of Jurassic and Devonian age; lower gault is present only below the outer parts of the basin and is absent under central London. 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

onlap Onlap or ''overlap'' is the geological phenomenon of successively wedge-shaped younger rock strata extending progressively further across an erosion surface cut in older rocks. It is generally associated with a marine transgression. It is a more ge ...

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

Uses

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

Dunton Green Dunton Green is a small village and civil parish in the Sevenoaks District of Kent, England. It lies in the valley of the River Darent, north of the town of Sevenoaks. Dunton Green is designated as being part of the Kent Downs area of outstandin ...

and Wye in

. Gault often contains numerous phosphatic nodules, some thought to be

coprolites A coprolite (also known as a coprolith) is fossilized feces. Coprolites are classified as trace fossils as opposed to body fossils, as they give evidence for the animal's behaviour (in this case, diet) rather than morphology. The name is d ...

, and may also contain sand as well as small grains of the mineral

glauconite Glauconite is an iron potassium phyllosilicate ( mica group) mineral of characteristic green color which is very friable and has very low weathering resistance. It crystallizes with a monoclinic geometry. Its name is derived from the Gre ...

. Crystals of the mineral selenite are fairly common in places, as are nodules of pyrite.

Fossils

Hamitidae Fossil in Wear Bay in Folkestone in England

Gault yields abundant marine

fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...

s, including ammonites (such as ''Hoplites'', ''Hamites'', '' Euhoplites'', ''Anahoplites'', and ''Dimorphoplites''), belemnites (such as ''Neohibolites''), bivalves (such as ''Birostrina'' and ''Pectinucula''),

gastropods The gastropods (), commonly known as snails and slugs, belong to a large taxonomic class of invertebrates within the phylum Mollusca called Gastropoda (). This class comprises snails and slugs from saltwater, from freshwater, and from land. The ...

(such as ''Anchura''), solitary corals,

fish Fish are aquatic, craniate, gill-bearing animals that lack limbs with digits. Included in this definition are the living hagfish, lampreys, and cartilaginous and bony fish as well as various extinct related groups. Approximately 95% of ...

remains (including shark teeth), scattered

crinoid Crinoids are marine animals that make up the class Crinoidea. Crinoids that are attached to the sea bottom by a stalk in their adult form are commonly called sea lilies, while the unstalked forms are called feather stars or comatulids, which are ...

remains, and

crustacean Crustaceans (Crustacea, ) form a large, diverse arthropod taxon which includes such animals as decapods, seed shrimp, branchiopods, fish lice, krill, remipedes, isopods, barnacles, copepods, amphipods and mantis shrimp. The crustacean group can ...

s (such as the crab ''Notopocorystes''). Occasional fragments of fossil wood may also be found.

References

{{reflist

External links

Fossils of the Gault Clay

Sedimentary rocks Cretaceous paleontological sites of Europe Geology of England Geology of Kent Geology of Oxfordshire Albian Stage Lower Cretaceous Series of Europe

Distribution

Uses

Fossils

See also

References

External links