Geologic hazard areas shall be classified according to the criteria in this section as follows:
A. Landslide Hazard Areas. Landslide hazard areas are those areas potentially subject to land-slide activity based on a combination of geologic, topographic, and hydrogeologic factors as classified in subsection
B of this section with slopes 15 percent or steeper within a vertical elevation change of at least 10 feet or all areas of prior landslide activity regardless of slope. A slope is delineated by establishing its toe and top, and measuring the inclination over 10 feet of vertical relief (see Figure 20.240.220(A)). The edges of the geologic hazard are identified where the characteristics of the slope cross-section change from one landslide hazard classification to another, or no longer meet any classification. Additionally:
1. The toe of a slope is a distinct topographic break that separates slopes inclined at less than 15 percent from slopes above that are 15 percent or steeper when measured over 10 feet of vertical relief; and
2. The top of a slope is a distinct topographic break that separates slopes inclined at less than 15 percent from slopes below that are 15 percent or steeper when measured over 10 feet of vertical relief.
Figure 20.240.220(A): Illustration of slope calculation for determination of top and toe of landslide hazard area. |
B. Landslide Hazard Area Classification. Landslide hazard areas are classified as follows:
1. Moderate to High Risk.
a. Areas with slopes between 15 percent and 40 percent and that are underlain by soils that consist largely of sand, gravel, or glacial till that do not meet the criteria for very high risk areas in subsection (B)(2) of this section;
b. Areas with slopes between 15 percent and 40 percent that are underlain by soils consisting largely of silt and clay and do not meet the criteria for very high risk areas in subsection (B)(2) of this section; or
c. All slopes of 10 to 20 feet in height that are 40 percent slope or steeper and do not meet the criteria for very high risk in subsection (B)(2)(a) or (b) of this section.
2. Very High Risk.
a. Areas with slopes steeper than 15 percent with zones of emergent water (e.g., springs or ground water seepage);
b. Areas of landslide activity (scarps, movement, or accumulated debris) regardless of slope; or
c. All slopes that are 40 percent or steeper and more than 20 feet in height when slope is averaged over 10 vertical feet of relief.
Figure 20.240.220(B): Illustration of very high risk landslide hazard area delineation (no midslope bench). |
C. Seismic Hazard Areas. Seismic hazard areas are lands that, due to a combination of soil and ground water conditions, are subject to risk of ground shaking, lateral spreading, or subsidence or liquefaction of soils during earthquakes. These areas are typically underlain by soft or loose saturated soils (such as alluvium) or peat deposits and have a shallow ground water table. These areas are designated as having “high” and “moderate to high” risk of liquefaction as mapped on the Liquefaction Susceptibility and Site Class Maps of Western Washington State by County by DNR.
D. Erosion Hazard Areas. Erosion hazard areas are lands or areas underlain by soils identified by the U.S. Department of Agriculture (USDA) Natural Resources Conservation Service (formerly the Soil Conservation Service) as having “severe” or “very severe” erosion hazards. This includes, but is not limited to, the following group of soils when such soils occur on slopes of 15 percent or greater: Alderwood-Kitsap (AkF), Alderwood gravelly sandy loam (AgD), Kitsap silt loam (KpD), Everett (EvD), and Indianola (InD).
(Ord. 856 § 2 (Exh. B), 2019)