place

Lulsgate Plateau

Landforms of SomersetMendip HillsPlateaus of EnglandSomerset geography stubsWrington

Lulsgate Plateau is the name given to the Carboniferous Limestone hills which form a northern outlier of the Mendip Hills, southwest of Bristol, England, approximately 600 feet (180 m) above sea level, which has been occupied since prehistoric times. The major feature on the plateau is Bristol International Airport. Cutting into the western edge of the plateau are two combes, Brockley Combe and Goblin Combe a 52 hectares (128 acres) biological Site of Special Scientific Interest (SSSI). There are two major roads in the area — the A38 cuts across the top of the plateau, while the A370 runs along its western edge. Both run in a southwesterly direction, and join Bristol to towns and villages in Somerset. To the west of the plateau are the North Somerset Levels, and to the south is the Yeo valley.

Excerpt from the Wikipedia article Lulsgate Plateau (License: CC BY-SA 3.0, Authors).

Lulsgate Plateau
Red Hill,

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Lulsgate PlateauContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 51.366666666667 ° E -2.7166666666667 °
placeShow on map

Address

Red Hill

Red Hill
BS40 5TG
England, United Kingdom
mapOpen on Google Maps

Share experience

Nearby Places

Fairy Toot
Fairy Toot

The Fairy Toot is an extensive oval barrow in the civil parish of Nempnett Thrubwell, Somerset, England (grid reference ST520618). It is an example of the Severn-Cotswold tomb type which consist of precisely-built, long trapezoid earth mounds covering a burial chamber. Because of this they are a type of chambered long barrow. Fairy Toot was formerly a chambered cairn which is a Scheduled Ancient Monument. Located south-southwest of Howgrove Farm, it is a mound 60 m long, 25 m wide and now 2.5 m high, retained by a stone wall. Its summit is covered with ash trees and shrubs. Formerly it was considerably higher. On being opened and essentially destroyed between 1787 and 1835 by the Reverend Thomas Bere of Butcombe and the Reverend John Skinner of Camerton, it was found to contain two rows of cells, running from south to north, formed by immense stones set edgeways, and covered by others of larger dimensions. A human skull from the barrow is now in the Bristol Museum and Art Gallery.At the time it was conjectured to be a work of the Druids, but its origins are far older and probably date from the Neolithic period.Wade and Wade in their 1929 book "Somerset" described it as "a remarkably fine tumulus of masonry, said to have been one of the finest in Britain, in the chambers of which skeletons have been discovered. A few vestiges of it now only remain, the rest has been used as a lime-kiln."The site was visited in the past as it was known as a place for curing warts.