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appendix a - National Grid

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5.3 Geology<br />

TEP on behalf of <strong>National</strong> <strong>Grid</strong> 7 of 21<br />

King’s Lynn 400kV Connection<br />

110488-FRA-R1(1)<br />

According to the published 1:50,000-scale geological map of the area, superficial<br />

geology of the site is underlain by tidal flat deposits with clay and silt. The bedrock<br />

geology of the site is characterised by the Kimmeridge Clay formation.<br />

5.4 Hydrogeology<br />

As shown on the EA map (Figure 2), the nearest aquifer is approximately 1km to the<br />

east of the site in West Winch where the superficial deposits is made up of ‘Secondary<br />

(Undifferentiated)’ and the bedrock aquifer as ‘Principal’. ‘Secondary (Undifferentiated)’<br />

aquifers indicate that the layer has previously been designated as both minor and nonaquifer<br />

due to variable characteristics of the rock type. ‘Principal’ aquifers are major<br />

aquifers with high permeability.<br />

The site itself is located on a non-aquifer, however, depending on the exact make up of<br />

the superficial geology (tidal flat deposits) some perched shallow groundwater may be<br />

present.

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