Results 81 to 90 of about 365 (128)
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Proceedings of the Geologists' Association, 1975
The soils of the Weald are determined largely by the nature of the underlying solid geology and the widespread distribution of superficial drift. Thirteen soil associations have been recognised and a map and extended legend are presented. For each association a general account of the soils is given, together with a discussion of the practical ...
S.G. McRae, C.P. Burnham
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The soils of the Weald are determined largely by the nature of the underlying solid geology and the widespread distribution of superficial drift. Thirteen soil associations have been recognised and a map and extended legend are presented. For each association a general account of the soils is given, together with a discussion of the practical ...
S.G. McRae, C.P. Burnham
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New insects from the Weald Clay of the Weald
Proceedings of the Geologists' Association, 1991The following new insect taxa are described and their significance discussed: Yuripopovia woottoni gen. et sp. nov. (Hemiptera: Progonocimicidae); Architipula austeni sp. nov. and Gynoplistial mitchelli sp. nov. (Diptera: Tipulidae); Necrotaulius mantellorum sp. nov. (Trichoptera: Necrotauliidae); Archisphex boothi sp. nov.
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The structure of the Weald—a review
Proceedings of the Geologists' Association, 1975Regional analyses of the structure of sedimentary basins distinguish structures reflecting basement structures from later tensional phase structures within the basin-fill. The effects of overburden-thickness and stratal competence are also considered. In the Weald, discrete structural zones are identified in the strata beneath the Weald Clay which can ...
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On the uplift and denudation of the Weald
Geological Society, London, Special Publications, 1999Abstract The evolution of the Weald has been the subject of continuing controversy over nearly two centuries of investigation. This paper reviews current knowledge of the area’s development during the Tertiary against this background and produces an evolutionary geomorphology focused on a cross-section reconstruction of the Weald
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The economic geology of the Weald
Proceedings of the Geologists' Association, 1975The major proportion of the minerals of economic importance in the Weald is consumed by the construction industry. These minerals include sand and gravel for aggregate, clay for brick manufacture, chalk for cement, limestone (ragstone) for roadstone, and gypsum for plaster, plasterboard and cement manufacture. In addition the Weald is a major source of
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2018
A detailed magnetometer survey conducted over approximately 36 ha of arable farmland at North Weald Basset has identified 19th century field boundaries, with similarly aligned possible linear features possibly related to earlier boundaries, no longer present in the 19th or 20th centuries.
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A detailed magnetometer survey conducted over approximately 36 ha of arable farmland at North Weald Basset has identified 19th century field boundaries, with similarly aligned possible linear features possibly related to earlier boundaries, no longer present in the 19th or 20th centuries.
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