DNR Reports Landslides

An Evaluation of Debris Avalanches in the Central Cape Breton Highlands, Nova Scotia

Debris avalanches are a complex failure involving components of rock topple, rotational spillage, translational sliding and flow with rates of movement from 0.5 to 30 m/s.
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Triggering Mechanisms of Debris Avalanches in the Central Cape Breton Highlands, Nova Scotia

Debris avalanches result from a complex failure involving components of rock topple, rotational slippage, translational sliding and flow with rates of movement from 0.5 to 30 m/s.
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