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Quarterly Journal of Engineering Geology and Hydrogeology
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Quarterly Journal of Engineering Geology and Hydrogeology; 1987; v. 20; issue.2; p. 187;
DOI: 10.1144/GSL.QJEG.1987.020.02.10
© 1987 Geological Society of London

Commentary

J. HOUSTON, J. EASTWOOD & T. Cosgrove reply

J. Houston, J. Eastwood & T. Cosgrove

1 Hydrotechnica, , Shewsbury
2 Wessex Water Authority, , Poole

We thank Mr Jones and Dr Beeson for their comments. The variation in electrical conductance between pore water and fissure water would have to be large to account for the observed variations in ground conductivity. Similarly for the variations between lithostratigraphic units. There is no evidence to suggest that this is the case at Lulworth.

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This 250-word extract was created in the absence of an abstract.


Related articles in Quarterly Journal of Engineering Geology and Hydrogeology:

Locating potential borehole sites in a discordant flow regime in the Chalk aquifer at Lulworth using integrated geophysical surveys
J. F. T. Houston, J. C. Eastwood, and T. K. P. Cosgrove
Quarterly Journal of Engineering Geology and Hydrogeology 1986 19: 271-282. [Abstract]