What is Cotswold Chips Grey?
The spine of the Cotswolds runs southwest to northeast through six counties, particularly Gloucestershire, west Oxfordshire and south western Warwickshire. The northern and western edges of the Cotswolds are marked by steep escarpments down to the Severn valley and the Warwickshire Avon. This feature, known as the Cotswold escarpment, or sometimes the Cotswold Edge, is a result of the uplifting (tilting) of the limestone layer, exposing its broken edge. This is a cuesta, in geological terms. The dip slope is to the southeast. On the eastern boundary lies the city of Oxford and on the west is Stroud. To the southeast, the upper reaches of the Thames Valley and towns such as Lechlade, Tetbury and Fairford are often considered to mark the limit of this region. To the south the Cotswolds, with the characteristic uplift of the Cotswold Edge, reach beyond Bath, and towns such as Chipping Sodbury and Marshfield share elements of Cotswold character.
Cotswold Shale: The Cotswolds is an area in south central England containing the Cotswold Hills, a range of rolling hills which rise from the meadows of the upper Thames to an escarpment, known as the Cotswold Edge, above the Severn Valley and Evesham Vale. The area is defined by the bedrock of Jurassic limestone that creates a type of grassland habitat rare in the UK and that is quarried for the golden coloured Cotswold stone. It contains unique features derived from the use of this mineral; the predominantly rural landscape contains stone-built villages, historical towns and stately homes and gardens.
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