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A sheet of mainly Jurassic limestone fan gravel probably covered most of the vale in the past but has since been eroded away leaving isolated deposits, most notably the Cheltenham Sand, which forms a well-draining light soil in the Cheltenham-Gloucester region. Inferior oolite exposed below Crickley Hillfort on the edge of the Cotswold ...
A limestone pavement is a natural karst landform consisting of a flat, incised surface of exposed limestone that resembles an artificial pavement. [1] The term is mainly used in the UK and Ireland, where many of these landforms have developed distinctive surface patterning resembling paving blocks. [ 2 ]
Carboniferous Limestone – Limestone deposited during the Dinantian Epoch of the Carboniferous Period; Coquina – Sedimentary rock that is composed mostly of fragments of shells; Coral rag – Limestone composed of ancient coral reef material; Chalk – Soft carbonate rock; Fossiliferous limestone – Limestone containing fossils
"Drift" geology is often more important than "solid" geology when considering building works, drainage, siting water boreholes, sand and gravel resources and soil fertility. Although "drift" strictly refers to glacial and fluvio-glacial deposits, the term on geological maps has traditionally included other materials including alluvium, river ...
The Lower Greensand as a broad zone between the brick-patterned chalk (a type of limestone) and the interior large c-shape Weald Clay. Many towns shown are on 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 ages of the Early ...
Somerset. Somerset is a rural county in the southwest of England, covering 4,171 square kilometres (1,610 sq mi).It is bounded on the north-west by the Bristol Channel, on the north by Bristol and Gloucestershire, on the north-east by Wiltshire, on the south-east by Dorset, and on the south west and west by Devon.
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The southeastern margin of the deep Wem-Audlem Sub-basin, at the heart of the southern part of the Cheshire Basin is defined within Shropshire by the northeast-southwest trending Wem Fault. Further southeast is the sub-parallel Hodnet Fault which forms the outer boundary of the larger basin with the area between the two faults hosting a thinner ...