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The Lake Edgar Fault in Western Tasmania, Australia is marked by a prominent fault scarp and is a recently reactivated&#13; fault initially of Cambrian age. The scarp has a northerly trend and passes through the western abutment&#13; of the Edgar Dam, a saddle dam on Lake Pedder. The active fault segment displaces geologically young river&#13; and glacial deposits. It is 29 ± 4 km long, and dips to the west. Movement on the fault has ruptured the ground&#13; surface at least twice within the Quaternary and possibly the last ca. 25 000 years; the most recent rupture has&#13; occurred since the last glaciation (within the last ca. 10000 years). This is the only known case of surface faulting&#13; in Australia with evidence for repeated ruptures in the Late Pleistocene. Along its central portion the two&#13; most recent surface-faulting earthquakes have resulted in about 2.5 m of vertical displacement each (western side&#13; up). The Lake Edgar Fault is considered capable of generating earthquakes in the order of magnitude 61/2-71/4.&#13; The Gell River Fault is another fault nearby that was apparently also active in the Late Pleistocene. It has yet to&#13; be studied in detail but the scarp appears to be more degraded and therefore older than the most recent movement&#13; on the Lake Edgar Fault

The Lake Edgar Fault: an active fault in Southwestern Tasmania, Australia, with repeated displacement in the Quaternary