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Layer: Deposits (ID: 2)

Name: Deposits

Display Field: Project

Type: Feature Layer

Geometry Type: esriGeometryPolygon

Description: <DIV STYLE="text-align:Left;"><DIV><DIV><P><SPAN>These colluvial and alluvial deposits represent the areal extents of significant volumes of earth, debris, and rock fragments that could have accumulated in part because of past debris flows and debris slides and, to a lesser extent, rock falls and rockslides. These colluvial and alluvial deposits indicate areas that can be affected by landslides and can be unstable in some circumstances. The bulk of the deposits are likely prehistoric in age, but their ages have yet to be verified by modern age-dating techniques. Colluvial deposits consist of heterogeneous mixtures of clay, silt, and sand particles with gravel- to boulder-sized rock clasts in various stages of weathering and decomposition. Areas mapped as deposits met two or more of the following criteria: 1) exhibited an elongate, lobate or fan shape, or other landform characteristic of a slope movement deposit, visible at a scale of &lt;1:7,500 using Light Detecting And Ranging (LiDAR) digital elevation model (DEM) derivatives; 2) had an adequate upslope source area where past slope movements could have initiated; 3) were verified in the field to contain gravel- to boulder-sized clasts or other textures and depositional structures that characterize deposits produced by slope movements (i.e. matrix supported or imbricated clasts, or scour and fill structures); and/or contained boulder deposits visible in some recent orthophotography. Many narrow stream valleys likely contain colluvial deposits that are not feasible to map at this scale.</SPAN></P></DIV></DIV></DIV>

Copyright Text: North Carolina Geological Survey (NCGS)

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