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rowmag
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biffvernon said:So now we know that the power station is built on solid geology not alluvium. 'Mudstone' should be read as stone rather than mud. The buildings are not going to slide into the sea, as someone suggested a great many posts ago.
The significant detail about how permeable the rock immediately below the reactors buildings is to the movement of groundwater and potentially radioactive cooling water still eludes us.
Do the N values provide any indirect hints? I don't know how to interpret how they are displayed in the figure, but in the text it mentions that the lower layers typically have N=40 or greater. (I know N is a soil hardness measure, not a permeability one, but could naively imagine that a high N value suggests low permeability, absent cracks.)