. . . . . . . "1770941"^^ . . . . . . . . . . "A Forma\u00E7\u00E3o Weald Clay, tamb\u00E9m conhecida simplesmente como Weald Clay \u00E9 uma unidade de rocha sedimentar do Cret\u00E1ceo Inferior subjacente \u00E0s \u00E1reas do Sudeste da Inglaterra, entre as Colinas do Norte e do Sul, em uma \u00E1rea chamada . \u00C9 a unidade mais alta do de rochas dentro da Bacia Weald, e a por\u00E7\u00E3o superior da unidade \u00E9 equivalente em idade \u00E0 por\u00E7\u00E3o exposta da Forma\u00E7\u00E3o Wessex na Ilha de Wight. Ele consiste predominantemente em lamito com camadas finas. A forma\u00E7\u00E3o foi depositada em condi\u00E7\u00F5es lagunares, lacustres e aluviais que variaram de \u00E1gua doce a salobra. A argila se alterna com outras litologias subordinadas, notavelmente leitos duros de pedra-ferro, calc\u00E1rio (M\u00E1rmore de Sussex) e arenitos, incluindo a unidade de arenito calc\u00E1rio referida como a . Ele tem um contato gradual e conform\u00E1vel com a subjacente e tem um contato brusco e inconform\u00E1vel com a sobrejacente, uma unidade marinha rasa depositada ap\u00F3s a transgress\u00E3o marinha durante o Aptiano."@pt . . . . . . . . . . . . . "27600.0"^^ . . . . . . . . . . . . . . . "Weald Clay exposed at Clock House Brickworks"@en . . . . . . . . . . . . . . . "Extent of the Weald Clay within the Weald Basin, shown with horizontal lines"@en . . "Weald Clay"@en . . . . . . . . . . . . . . . . . "A Forma\u00E7\u00E3o Weald Clay, tamb\u00E9m conhecida simplesmente como Weald Clay \u00E9 uma unidade de rocha sedimentar do Cret\u00E1ceo Inferior subjacente \u00E0s \u00E1reas do Sudeste da Inglaterra, entre as Colinas do Norte e do Sul, em uma \u00E1rea chamada . \u00C9 a unidade mais alta do de rochas dentro da Bacia Weald, e a por\u00E7\u00E3o superior da unidade \u00E9 equivalente em idade \u00E0 por\u00E7\u00E3o exposta da Forma\u00E7\u00E3o Wessex na Ilha de Wight. Ele consiste predominantemente em lamito com camadas finas."@pt . . . . . . . . . . . . . "Hauterivian-Barremian,"@en . . . . . "Horsham Stone Member"@en . . . . "15120"^^ . "Forma\u00E7\u00E3o Weald Clay"@pt . . . . . . . . . . . . . . . . . . "Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of rocks within the Weald Basin, and the upper portion of the unit is equivalent in age to the exposed portion of the Wessex Formation on the Isle of Wight. It predominantly consists of thinly bedded mudstone. The un-weathered form is blue/grey, and the yellow/orange is the weathered form, it is used in brickmaking. The formation was deposited in lagoonal, lacustrine and alluvial conditions that varied from freshwater to brackish. The clay alternates with other subordinate lithologies, notably hard red-weathering beds of ironstone, limestone (Sussex Marble) and sandstones, notably including the calcareous sandstone unit referred to as the Horsham Stone. It has a gradual, conformable contact with the underlying Tunbridge Wells Sand Formation, and has a sharp, unconformable contact with the overlying Atherfield Clay Formation, a shallow marine unit deposited after marine transgression during the Aptian."@en . . . . . . . . . "Barremian"@en . . "1115442793"^^ . . . . . . . "Weald Clay"@en . . . . . . "Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of rocks within the Weald Basin, and the upper portion of the unit is equivalent in age to the exposed portion of the Wessex Formation on the Isle of Wight. It predominantly consists of thinly bedded mudstone. The un-weathered form is blue/grey, and the yellow/orange is the weathered form, it is used in brickmaking."@en . . . .