Abstract
In 1919 the authors contributed a paper on the sequence, glaciation and correlation of the Carboniferous rocks of the Hunter River district of New South Wales to the proceedings of the Royal Society of New South Wales (1). In this paper the existence of glacial beds in strata of Carboniferous age in the Hunter River district of New South Wales was described and correlations were suggested with various localities both in Australia and in other parts of the world. The views then put forward have been generally accepted by Australian geologists. Since the publication of that paper, much additional information regarding the Carboniferous and Permo-Carboniferous formations of Australia has become available as a result of the labors of many geologists in the various Australian States, but particularly in Western Australia, Queensland and New South Wales.
In 1928 there appeared in these Proceedings (Geological Society of America) a comprehensive paper . . .
