ABSTRACT
Massachusetts geologist Edward Hitchcock was among the first of his American colleagues to investigate the glacial theory of Swiss geologist Louis Agassiz. After studying a copy of Agassiz’s Études sur les Glaciers (1840), Hitchcock displayed an initial enthusiasm regarding its explanatory powers in the published version of his presidential address before the newly-founded Association of American Geologists, and in his concurrently-published Final Report on the Geology of Massachusetts (1841). But that same year, Hitchcock also undertook a 400-mile journey to the White Mountains of New Hampshire, to test the possible validity of a hypothetico-deductive argument that he had formulated, about whether Alpine-style glaciers had once descended from their summits. From the lack of supporting field evidence, Hitchcock abruptly retreated into a non-committal stance that merely argued for some combination of ice-and-water that he labeled “glacio-aqueous action.”