Mid Severn Sandstone Plateau in the context of "Kinver Edge"

Play Trivia Questions online!

or

Skip to study material about Mid Severn Sandstone Plateau in the context of "Kinver Edge"




⭐ Core Definition: Mid Severn Sandstone Plateau

The Mid Severn Sandstone Plateau is a rural landscape and one of the natural regions of central England, straddling the border between the counties of Shropshire and Staffordshire. It stretches from the western fringes of the Birmingham conurbation to Telford in the north and Kidderminster in the south. The major feature of the plateau is the valley of the River Severn, which cuts through it from north to south. It consists of Permian and Triassic-age New Red Sandstone getting older as one goes west until one reaches Silurian and Carboniferous-age siltstones and coals west of the river.

↓ Menu

In this Dossier

Mid Severn Sandstone Plateau in the context of Shropshire Hills

The Shropshire Hills are a dissected upland area and one of the natural regions of England. They lie wholly within the county of Shropshire and encompass several distinctive and well-known landmarks, such as the Long Mynd, Wenlock Edge, The Wrekin and the Clees.

The Shropshire Hills lie south of the county town of Shrewsbury between the Welsh border and Much Wenlock, extending as far south as Ludlow. To the north they are bounded by the Shropshire, Cheshire and Staffordshire Plain, to the east by the Severn Valley and Mid Severn Sandstone Plateau, to the southeast by Knighton and the Teme Valley and to the southwest by the Clun and North West Herefordshire Hills.

↑ Return to Menu