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teristics of the prior-, ancestral-, and modern-river channels are described :and compared, and, finally, an attempt to establish the nature of the climate changes and to describe the mechanics of the river adjustment to these changes is made.At least hal£ of t:he report consists of descriptions of the Murrumbidgee River and its associated paleochannels; the climate, vegetation, and geology of the drninage basin and the Riverine Plain; and a review of the previous work of Australian scientists.This material, although necessary for a complete understanding of the problems can be avoided by the reader who may choose to move directly to the section entitled "Comparaltive Morphology and Hydrology of the Riverine Plain Channel's."
Stanley A. Schumm (Mon,) studied this question.