A.
Designation. Geologically hazardous areas are areas susceptible to erosion, landsliding, earth-quake activity or other geological processes. Areas susceptible to these types of hazards are hereby designated as geologically hazardous areas and shall be subject to the provisions of this chapter.
B.
Mapping. The approximate location and extent of geologically hazardous areas are shown on mapping resources that support the city’s identification of critical areas. These resources serve as guidance for the city, applicants, and property owners, and may be updated as new critical areas are identified. They do not provide a definitive critical area designation. Mapping resources include:
C.
Classification. Geologically hazardous areas shall be classified as follows:
1.
Landslide and Erosion Hazard Areas. Erosion hazard areas include those identified by the U.S. Department of Agriculture’s Natural Resources Conservation Service as having a moderate to severe, severe, or very severe erosion hazard because of natural characteristics, including vegetative cover, soil texture, slope, gradient, and rainfall patterns, or human-induced changes to natural characteristics. Landslide hazard areas are areas potentially subject to risk of mass movement due to a combination of geologic, topographic, and hydrologic factors. Landslide and erosion hazard areas include areas with the following characteristics:
a.
Areas that have shown movement during the Holocene epoch (from 10,000 years ago to the present) or that are underlain or covered by mass wastage debris of that epoch;
b.
Slopes that are parallel or subparallel to planes of weakness (such as bedding planes, joint systems, and fault planes) in subsurface materials;
c.
Slopes having gradients steeper than 80 percent subject to rockfall during seismic shaking;
d.
Areas potentially unstable because of stream incision and stream bank erosion;
e.
Areas located in a canyon, ravine, or on an active alluvial fan, presently or potentially subject to inundation by debris flows or flooding;
f.
Any area with a slope of 40 percent or steeper and a vertical relief of 10 or more feet except areas composed of consolidated rock and properly engineered manmade slopes/retained fill. A slope is delineated by establishing its toe and top and measured by averaging the inclination over at least 10 feet of vertical relief;
g.
Areas with a severe limitation for building development because of slope conditions, according to the Natural Resource Conservation Service; and
h.
Areas meeting all three of the following criteria: slopes steeper than 15 percent except that slopes of less than 15 percent may be considered erosion hazard areas if they have certain unstable soil and drainage characteristics; hillsides intersecting geologic contacts with a relatively permeable sediment overlying a relatively impermeable sediment or bedrock; and wet season springs or ground water seepage.
2.
Seismic Hazard Areas. Seismic hazard areas are areas subject to severe risk of damage as a result of earthquake-induced ground shaking, slope failure, settlement, soil liquefaction, lateral spreading, or surface faulting. Settlement and soil liquefaction conditions occur in areas underlain by cohesionless, loose, or soft-saturated soils of low density, typically in association with a shallow ground water table.
(Ord. 2004-603 § 2; Ord. 2026-945 § 2 (Att. A))