South West England - Subregion 3

Question

Accepted Answer

The screening report hosted on this site is a technical exercise across England, Wales and Northern Ireland. No specific location in England, Wales or Northern Ireland has been identified as a potential GDF site. Any future decision on geological disposal would be subject to community agreement and planning and environmental consents.

Details

Our work shows that we may find a suitable geological setting for a GDF in most of this subregion.

Given that the southern half of this subregion is the inshore which extends to 20km from the coast, rock can only be seen at the surface in the sea cliffs between Budleigh Salterton and Lyme Regis and in man-made excavations such as quarries or road cuttings. A small number of boreholes and geophysical investigations give us an understanding of the geology at depth.

There are various types of gaps in our understanding of geology and we deal with these gaps in a number of ways.

There are clay-rich rock layers under the whole of the subregion in which we may be able to site a GDF. There are also slates and similar strong rocks around Taunton and off the coast of Budleigh Salterton, and layers of rock salt between Lyme Regis and Chard, in which we may be able to site a GDF. We would need to do more work to find out whether these rocks have suitable properties and thicknesses.

Even where individual clay-rich rock layers are found not to be thick enough to host a GDF they may support the siting of a GDF in deeper rocks as they could act as a barrier to groundwater flow from depth. This is important because movement of groundwater is one of the ways in which radioactive material could be carried back to the surface.

There are no known coal, oil, gas or metal resources in this subregion which means that it is unlikely that future generations may disturb a facility.

For further information, read the report below.