A.
Geologic hazard areas identification and designation shall be consistent with the minimum guideline classifications established in WAC 365-190-080(4), which include any future amendments to the code. Areas that are susceptible to one or more of the following types of hazards shall be classified as a geologic hazard area:
B. Erosion Hazard Areas.
Those areas that are identified by the United States Department of Agriculture Soil Conservation Service as having a severe rill and inter-rill erosion hazard.
C. Landslide Hazard Areas.1. 2. 3. 4. 5. 6. 7. 8. 9.
Those areas that are potentially subject to landslides based on a combination of geologic, topographic, and hydrologic factors. They include any areas susceptible because of any combination of bedrock, soil, slope (gradient), slope aspect, structure, hydrology, or other factors. Landslide hazard areas include, but are not limited to, the following types of areas:
Areas delineated by the United States Department of Agriculture Soil Conservation Service as having a severe limitation for building site development;
Areas designated as quaternary slumps, earthflows, mudflows, lahars, or landslides on maps published by the United States Geological Survey or Department of Natural Resources Division of Geology and Earth Resources;
Areas that have shown movement during the Holocene epoch (from 10,000 years ago to the present) or which are underlain or covered by mass wastage debris of that epoch;
Areas with slopes that are parallel or subparallel to planes of weakness (such as bedding planes, joint systems, and fault planes) in subsurface materials;
Areas with slopes having gradients steeper than 80 percent subject to rockfall during seismic shaking;
Areas potentially unstable as a result of rapid stream incision, stream bank erosion and undercutting by wave action;
Areas that show evidence of, or on, an active alluvial fan presently or potentially subject to inundation by debris flows or catastrophic flooding; or
Areas with a slope of 40 percent or steeper and with a vertical relief of 10 or more feet except areas composed of consolidated rock. A slope is delineated by establishing its toe and top and measured by averaging the inclination over at least 10 feet of vertical relief.
D. Seismic Hazard Areas.
Those areas subject to severe risk of damage as a result of earthquake-induced ground shaking, slope failure, settlement, soil liquefaction, or surface faulting. One indicator of potential for future earthquake damage is a record of earthquake damage in the past. Ground shaking is the primary cause of earthquake damage in Washington. The strength of ground shaking is primarily affected by: (1) magnitude of an earthquake; (2) distance from the source of an earthquake; (3) type of thickness of geologic materials at the surface; and (4) type of subsurface geologic structure.
E. Mine Hazard Areas.
Those areas underlain by, adjacent to, or affected by mine working areas as designated by the Washington State Department of Natural Resources.
(Ord. 25-14 § 1.01; Ord. 12-18 § 1 (Exh. A))