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WSPC03680
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Last modified
1/26/2010 11:35:56 AM
Creation date
10/9/2006 4:07:40 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
5000.300
Description
Flood Protection Section - Mudflow Mitigation Plan - 1987
State
CO
Basin
Statewide
Date
1/1/1987
Title
Colorado Landslide Hazard Mitigation Plan - 1987 - Preliminary Draft
Water Supply Pro - Doc Type
Report/Study
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<br />002792 <br /> <br />2.0 LANDSLIDE PROCESSES AND PREDICTION <br /> <br />The term "landslide" is often used to describe a wide variety of processes that <br />result in the downward and outward movement of slope-forming materials composed <br />of rocks, soils, artificial fill, or a combination of these. The materials may <br />move in any of the following ways: falling, toppling, sliding, spreading, or <br />flowing (USGS, 1981). The various types of landslides can be differentiated by <br />the kind of material involved and the method of movement. An example of a classi- <br />fication system based on these parameters is shown in figure __' Other classifi- <br />cation systems also incorporate such variables as the rate of movement and the <br />water, air, or ice content. Different types of landslides are described below. <br /> <br />TYPES OF LANDSLIDES <br /> <br />Rockfalls and Other Earthfalls <br /> <br />Falls are abrupt movements of rock masses which become detached from steep <br />slopes or cliffs. Rock separation occurs along a surface on which little or <br />no shear displacement takes place and movement occurs through free-fall. <br />bouncing, and rolling (Varnes, 1978). <br /> <br />Rockfalls (figure __) consist of detached masses of bedrock and are strongly <br />influenced by the presence of fractures, joints, and bedding planes. <br /> <br />Falls composed of other types of earth materials result in soil-falls, debris- <br />falls, earth-falls, boulder-falls, and so on. All types of falls are promoted <br />by undercutting, differential weathering, excavation, or stream erosion. <br /> <br />Topples <br /> <br />Toppling failures (figure ) are distinguished by "...the forward rotation of <br />a unit or units about some pivotal point, below or low in the unit, under the <br />action of gravity and forces exerted by adjacent units or by fluids in <br />cracks. It is tilting without collapse." (Varnes, 1978). <br /> <br />Sl ides <br /> <br />Althou9h many types of mass movement are included in the general term <br />"1 ands 1 ide", the more restri ct ive use of the term refers to on ly "... those mass <br /> <br />- 6 - <br />
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