Investigation of the weathering processes and quaternary geology in the Wright Valley and the elevated beach ridges of Marble Point and investigation of the dykes at the Nussbaum Riegel

Pediments, the term being used in a broad sense and not glacial features, are the most striking landscape forms in the middle part of the Wright Valley and were also investigated. In addition, maximum wind velocities were determined in the Bull Pass area by setting up indicators to determine the strength of the wind. The lower Taylor Valley was reconnaissance with observations of local weathering phenomena (polygons, salt deposits, sand entrained on down valley sides of boulders, ridges, etc).

At Marble Point, 12 profiles were measured across the elevated marine shore lines which extend over about half the coast between Gneiss Point and Cape Bernacchi. The dykes at the Nussbaum Riegel contain one of the best exposed and most readily accessible dyke swarms. The various petrological types were collected and the field relations of the dykes were determined.

Samples were collected for K/Ar dating and geochemical analysis. The dykes were previously mapped as being entirely lamprophyres but the more detailed studies have shown that they are more correctly termed dolerite.