Lichenometric dating of debris-flow deposits in the scottish highlands Lichenometric dating of debris-flow deposits in the Scottish Highlands

Lichenometric dating of debris-flow deposits in the scottish highlands

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Publication History Issue online: Go to old article view. Both burning and overgrazing can be cited as potential causal factors.

The temporal and spatial development of landslides in the axmouth-lyme regis undercliffs national nature reserve, Devon Next article in issue: By continuing to browse this site you agree to us using cookies as described in About Cookies Remove maintenance message.

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Articles related to the one you are viewing Please enable Javascript to view the related content of this article. McDonaldJohn D. A laboratory simulation Next article in issue: QuiringChris HouserFrederick E.

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Number of times cited: Keywords Debris flows; Overgrazing; Lichenometry; Moor-burning. The timing of the increase suggests that it is related to landuse changes in the Scottish Highlands during the 19th and early 20th centuries.

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RegmiJohn R. View all 77 citations. Previous article in issue: LeviaTracy L.

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The temporal and spatial development of landslides in the axmouth-lyme regis undercliffs national nature reserve, Devon. Vitek,19CrossRef 9 Netra R. BruneauJohn E.

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Progressive weathering and climatic change can be discounted as the prime cause of the increase in the incidence of debris flows. NelsonSoil moisture: Close article support pane. GiardinoEric V.

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A laboratory simulation Previous article in issue: Next article in issue: Continue reading full article. Abstract Debris-flow deposits, dated by lichenometry, indicate that the majority of hillslope debris flows in Scotland have occurred within the last years. AylesAn examination of controls on debris flow mobility: DeLibertySteven M.

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Rainfall interception and splash detachment with a Brussels sprouts plant: