Landslide hazard areas include areas subject to landslides based on a combination of geologic, topographic, and hydrologic factors. This includes any areas susceptible to landslide because of any combination of bedrock, soil, slope, slope aspect, structure, hydrology, or other factors, and include, at a minimum, the following criteria:
A. Areas of historic failures, such as:
1. Those areas delineated by the United States Department of Agriculture Natural Resources Conservation Service as having a significant limitation for building site development;
2. Those coastal areas mapped as class u (unstable), uos (unstable old slides), and urs (unstable recent slides) in the department of ecology Washington coastal atlas; or
3. Areas designated as quaternary slumps, earthflows, mudflows, lahars, or landslides on maps published by the United States Geological Survey or Washington department of natural resources.
B. Areas with the following characteristics:
1. Slopes steeper than 15 percent;
2. Hillsides intersecting geologic contacts with a relatively permeable sediment overlying a relatively impermeable sediment or bedrock; and
3. Springs or groundwater seepage.
C. Areas that have shown movement during the Holocene epoch (10,000 years ago to the present) or which are underlain or covered by mass wastage debris of this epoch;
D. Slopes that are parallel or subparallel to planes of weakness, such as bedding planes, joint systems, and fault planes, in subsurface materials;
E. Slopes having a gradient steeper than 80 percent subject to rock fall during seismic shaking;
F. Areas potentially unstable as a result of rapid stream incision, stream bank erosion, and undercutting by wave action, including stream channel migration zones;
G. Areas located in a canyon or on an active alluvial fan, presently or potentially subject to inundation by debris flows or catastrophic flooding;
H. Any area with a slope of 40% or steeper and with a vertical relief of 10 or more feet except areas composed of bedrock. A slope is delineated by establishing the toe and top and measured by averaging the inclination over at least 10 feet of vertical relief;
(Ord. 343 § 1, 2002; Ord. 797, 12/1/2025)