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Faults in the Drift at Hitchin
Published online by Cambridge University Press: 01 May 2009
Abstract
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1 I may as well observe, that the faults at Hitchin station, large and small, are very nearly parallel to one another–as in most of our faulted districts. I think this indicates a more general movement than is implied in the idea of subsidence over cavernous ground, such as may account for the minor flexures in the drift giavel.—J.W.S.