Talus

Definition and stakes

Portrait of Edwin Swift Balch Edwin Swift Balch,  Glacières; or, Freezing Caverns

“ The talus, which was doubtless formed by a great slide at some distant date, consists of granite boulders, some of which are big ones. The ice-bearing portion may be some thirty or forty meters high vertically. It lies in a sort of gully or rock basin, and at the top is about thirty meters broad, tapering to a point at the bottom. The talus faces southward, and during a good part of the day the sun shines full upon it. A thin forest fringes the sides and grows round the bottom, but this can afford but little protection from the winds, especially to those from the south. ”
Source: Gutenberg

William Harmon Norton,  The Elements of Geology

“ TALUS. At the foot of cliffs there is usually to be found a slope of rock fragments which clearly have fallen from above. Such a heap of waste is known as talus. The amount of talus in any place depends both on the rate of its formation and the rate of its removal. Talus forms rapidly in climates where mechanical disintegration is most effective, where rocks are readily broken into blocks because closely jointed and thinly bedded rather than massive, and where they are firm enough to be detached in fragments of some size instead of in fine grains. ”
Source: Gutenberg

Portrait of Hugh Miller Hugh Miller,  The Cruise of the Betsey

“ The clay forms, when cut by a water-course, or assailed on the coast by some unusually high tide, a perpendicular precipice, which in the course of years slopes into a talus; and as it exhibits in most instances no marks of stratification, the clay of the talus—a mere re-formation of fragments detached by the frosts and rains from the exposed frontage—can rarely be distinguished from that of the original deposit. Now, in these consolidated slopes it is not unusual to find remains, animal and vegetable, of no very remote antiquity. ”
Source: Gutenberg

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