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| | Summary: Pediments |
 | | Pediment surfaces typically are cut across rocks of different types and ages, and the same erosional surface may thus be traced across several different localities within a region. |
 | | In basin-and-range deserts, pediments are excellent routes for vehicular and foot travel, because they do not have the hazards of the lower basin floors (see Summarys for Playas, Drainage Courses, and Depressions), and because pediment passes may be routes to, and at places across, mountain ranges. |
 | | Pediments generally lack sources of surface water, and bedrock occurs at shallow depths, shallowest at the upslope margin. |
| www.tec.army.mil /research/products/desert_guide/lsmsheet/lsped.htm (451 words) |
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