A basement complex of metamorphic rocks (Asgard Formation) and granites (Wright and Victoria Intrusives) is overlain by quartz sandstones and coal measures (Beacon Group). Both basement and sedimentary rocks are intruded by dolerite sills (Ferrar Dolerite). Rock units previously proposed for the adjacent Wright Valley were found to be applicable. A map and crass section show the geology from the Wright Valley to the Miller Glacier.
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Allen et al. (1962) studied this question.
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