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[[image - landscape drawing]] C Douglas bight [[end page]] [[start page]] They are somewhat faulted and the ash beds are often stream-waved and sometimes contain pebbly layers. The plants (No 92) are mostly reeds, grasses &c as if the deposit was a marsh flora. To the south three glaciers are visible in the range, two come down south of Cape Douglas and one ends in a stream discharging into the bight. The southernmost is the largest. The peninsula west of the bight is composed of a very level layer of columnar andesite about 40 ft thick with a talus of broken material of the same, and indications of leaf beds below. The top of this bed has been moderately glaciated (as also the eastern peninsula) and shows a few erratics. The agency might have been an extension of the glacier whose stream now discharges into the bight as the grooving points toward it. The rocks are a good deal de-