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Part of the site is owned and managed by Gloucestershire Willdlife Trust and the National Trust as a nature reserve Park. [1] [3] The Cotswold Way National Trail passes through Crickley Hill and Barrow Wake. [4] Barrow Wake and Tuffley's Quarry are listed in the 'Cotswold District' Local Plan 2001–2011 (on line) as Key Wildlife Sites. [5]
Barnsley Warren (grid reference) is a 61.3-hectare (151-acre) biological Site of Special Scientific Interest in Gloucestershire, notified in 1954 and renotified in 1984. [1] The site is also included in A Nature Conservation Review. It lies in a steep-sided dry valley, east of the A429, northeast of Cirencester in the Cotswolds. [2]
The Cotswolds (/ ˈ k ɒ t s w oʊ l d z, ˈ k ɒ t s w əl d z / KOTS-wohldz, KOTS-wəldz) [1] is a region of central South West England, along a range of rolling hills that rise from the meadows of the upper River Thames to an escarpment above the Severn Valley and the Vale of Evesham.
Cowley Manor Experimental Cotswolds hotel review. Daisy Lester. December 29, 2024 at 2:46 PM.
Belas Knap is a neolithic, chambered long barrow situated on Cleeve Hill, near Cheltenham and Winchcombe, in Gloucestershire, England. [1]It is a type of monument known as the Cotswold Severn Cairn, all of which have a similar trapezoid shape, and are found scattered along the River Severn. [2]
Calling all amateur malacologists: With “Memoir of a Snail,” stop-motion director Adam Elliot (an Oscar winner for “Harvie Krumpet”) invites us to study snails of every shape and size, ...
Spot Lane Quarry is a 0.1-hectare (0.25-acre) geological Site of Special Scientific Interest on the eastern outskirts of Maidstone in Kent. [1] [2] It is a Geological Conservation Review site. [3] [4] This site exposes loess, probably dating to the glacial Wolstonian Stage between 352,000 and 130,000 years ago. It contains the fossils of land ...
The site has been identified as of national importance in the Geological Conservation Review. [1] [2] [3] The site probably dates to the Hoxnian interglacial 420,000 to 300,000 years ago. It was then a marsh fed by springs, and it has a tufa which contains fossil land snails and mammal bones which show the climate and local environmental ...