By Roy C. Sidle

ISBN-10: 0875903150

ISBN-13: 9780875903156

ISBN-10: 1118665503

ISBN-13: 9781118665503

About The Product

Published by means of the yank Geophysical Union as a part of the Water assets Monograph Series.

This monograph compiles learn findings on soil mass stream right into a structure usable through practitioners and scholars. functions are under pressure within the parts of intensive and administration practices instead of engineering earthworks. Examples are incorporated to demonstrate quite a few prediction, avoidance, and regulate measures utilized in dealing with volatile terrain.

We use the time period soil (i.e., soil mass stream) to intend the mantle of unconsolidated or poorly consolidated fabric of both residual or transported beginning, that overlies bedrock and types the skin of the land. This utilization is in line with the normal civil engineering use of the notice and is synonymous with the geological time period regolith and with soil mantle.

Content:
Chapter 1 value of Soil Mass stream (pages 1–9): Roy C. Sidle, Andrew J. Pearce and Colin L. O'Loughlin
Chapter 2 significant kinds of Soil Mass circulation (pages 11–18): Roy C. Sidle, Andrew J. Pearce and Colin L. O'Loughlin
Chapter three Slope balance research (pages 19–30): Roy C. Sidle, Andrew J. Pearce and Colin L. O'Loughlin
Chapter four ordinary elements Affecting Slope balance (pages 31–72): Roy C. Sidle, Andrew J. Pearce and Colin L. O'Loughlin
Chapter five results of Land administration on Soil Mass flow (pages 73–88): Roy C. Sidle, Andrew J. Pearce and Colin L. O'Loughlin
Chapter 6 Predicting, warding off and Controlling Soil Mass flow (pages 89–118): Roy C. Sidle, Andrew J. Pearce and Colin L. O'Loughlin

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Sample text

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Rapiderosion bymass movement forlongdurations (>10'•yr)canprobably onlyoccur where acontinu- ousinputof gravitationalenergyis providedby tectonicuplift;otherwise, existingdrainagesystemsdictateslopegradientand only slowerformsof erosionoperate. ,CarsonandPetley,1970],which viewsslopeangleas the main drivingforceof massmovement,especially for shallow slides. , Carsonand Kirkby, 1972, p. 156]. Slowerprocesses, suchasslumpsandearthflows, aregenerally initiatedongentlerslopes. 17. Lowerlimitof slopegradient, generally measured ina representative portionofthescouringzone,for varioussoilmassmovements (datacompiled frommanysources).

G•:•:'•:• ...... •-" •,,' Fig. 16b. Fig. 16. Detailshowshow the clay layerhassmoothedthe formerlyroughsurfaceof the conglomerate (New ZealandForest Servicephotosby H. Hemmingand C. O'Loughlin).

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Hillslope Stability and Land Use by Roy C. Sidle


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