Abstract:
Three bore holes were drilled in the Marshall Valley approximately 1km apart to determine the Quaternary glacial stratigraphy of the area. The first hole was 24.52m in depth, the second was 31.92m and the third only 14.12m.
Robinson, P.H. 1987 Interpretation of glacigene sediments from drill core in Marshall Valley, Antarctica. New Zealand Geological Survey record 18: 49-57
Robinson, P.H. 1986 Lithological logs of drill cores MV 1, 2, and 3, Marshall Valley, Antarctica. NZ Geological Survey report G111