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Organic-rich sands and silts estimated to be about 25 000 to 40 000 years in age indicate that alpine-subalpine herb, shrub and heath vegetation communities occurred at 250 m altitude in the King Valley prior to the maximum phase of the Last Glaciation. Mean temperature was probably SC colder than at present and the climate was wet.

Vegetation history and climate before the maximum of the last Glaciation at Crotty, western Tasmania