Question

Lattman lh, parizek rp (1964) relationship between fracture traces and the occurrence of ground water in carbonate rocks. J hydrol 2:73–

Answer 1

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➡️Fracture traces visible on aerial photographs are natural linear-drainage, soiltonal, and topographic alignments which are probably the surface manifestation of underlying zones of fracture concentration. The relationship between fracture traces and occurrence of ground water was studied in Nittany Valley of Central Pennsylvania, U.S.A., an area underlain by folded and faulted Lower Paleozoic carbonate rocks with interbedded sandstones. Several bore-hole caliper surveys were run to determine if fracture zones underlying fracture traces localized cavernous openings. 

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