Chapter 23.50
GEOLOGICALLY HAZARDOUS AREAS

Sections:

23.50.010    Designation.

23.50.020    Mapping.

23.50.030    Exemptions.

23.50.040    Contents of critical areas reports.

23.50.050    Substantive requirements.

23.50.010 Designation.

Areas susceptible to one or more of the following types of hazards are hereby designated geologically hazardous areas, in accordance with WAC 365-190-080(4)(a):

A. Erosion hazard areas are areas identified by the U.S. Department of Agriculture’s Natural Resources Conservation Service as having a moderate-to-severe, severe, or very severe rill and inter-rill (sheet wash) erosion hazard.

B. Landslide hazard areas are areas subject to landslides based on geology, soils, topography, and hydrology, including:

1. Areas delineated by the U.S. Department of Agriculture’s Natural Resources Conservation Service as having a severe limitation for building site development;

2. Areas mapped by the Washington Department of Ecology (Coastal Zone Atlas) or the Washington State Department of Natural Resources (slope stability mapping) as unstable (U or Class 3), unstable old slides (UOS or Class 4), or unstable recent slides (URS or Class 5);

3. Areas designated as quaternary slumps, earthflows, mudflows, lahars, or landslides on maps published by the U.S. Geological Survey or Washington State Department of Natural Resources;

4. Areas where the following coincide: slopes steeper than 15 percent, a relatively permeable sediment overlying a relatively impermeable sediment or bedrock, and ground water seepage;

5. Areas that have shown movement in the past 10,000 years or that are underlain or covered by mass wastage debris of that time frame;

6. Slopes that are parallel or subparallel to planes of weakness (such as bedding planes, joint systems, and fault planes) in subsurface materials;

7. Slopes steeper than 80 percent subject to rock fall during seismic shaking;

8. Areas potentially unstable because of rapid stream incision, stream-bank erosion, and undercutting by wave action;

9. Areas at risk from snow avalanches;

10. Canyons or active alluvial fans subject to debris flows or catastrophic flooding; and

11. Slopes of 40 percent or steeper with a vertical relief of 10 or more feet except areas composed of consolidated rock.

C. 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. One indicator of potential earthquake damage is a record of past earthquake damage. Settlement and soil liquefaction occur in areas underlain by cohesionless, loose, or soft-saturated soils of low density, typically in association with a shallow ground water table.

D. Mine hazard, volcanic, and tsunami hazard areas (none known to be present: see WAC 365-190-080).

E. Other hazard areas include areas susceptible to mass wasting, debris flows, rock falls, and differential settlement. (Ord. 1592 § 1, 2004).

23.50.020 Mapping.

The following maps, which may be continuously updated, may be used as a guide for locating geologically hazardous areas:

A. U.S. Geological Survey landslide hazard, seismic hazard, and volcano hazard maps;

B. Washington State Department of Natural Resources seismic hazard maps for Western Washington;

C. Washington State Department of Natural Resources slope stability maps;

D. Locally adopted maps. (Ord. 1592 § 1, 2004).

23.50.030 Exemptions.

In addition to those listed in PMC 23.10.070, the following developments shall be exempt from this chapter:

A. Buildings with less than 2,500 square feet of floor area which are not used as places of residence, employment, or public assembly;

B. Additions of under 250 square feet to single-story residences;

C. Fences; and

D. Other minor developments as determined by the director. (Ord. 1592 § 1, 2004).

23.50.040 Contents of critical areas reports.

In addition to the requirements of PMC 23.10.090, critical areas reports for geologically hazardous areas shall include, where applicable:

A. Site history regarding landslides, erosion, and prior grading;

B. Topography in suitable contour intervals;

C. Height of slope, slope gradient, slope stability, and slope retreat rate recognizing potential catastrophic events;

D. Description of the geology (including faults), hydrology (including springs, seeps, and surface runoff features), soils (including, in seismic hazard areas, thickness of unconsolidated deposits and liquefaction potential), and vegetation;

E. Type, extent, and severity of geologic hazard(s);

F. Analysis of the proposal’s risk from geologic hazard and the proposal’s potential for exacerbating off-site hazards;

G. Recommended buffers and other conditions of approval. In areas of erosion or landslide hazard, the recommended conditions may include:

1. Clearing, fill, and hard-surfacing limits, slope stabilization measures, and vegetation management plan;

2. Limitation on clearing during the rainy season, generally from October 1st to May 1st;

3. Design parameters of foundations and retaining structures; and

4. Drainage plan and erosion and sediment control plan in compliance with city storm water management regulations; and

H. Overview of field investigations, measurements, references, and past assessments of the site. (Ord. 1592 § 1, 2004).

23.50.050 Substantive requirements.

In addition to the substantive requirements of PMC 23.10.130, the following requirements shall apply to geologic hazard areas:

A. Proposed developments shall not increase the long-term risk of or exposure to geological hazard on-site or off-site.

B. Hazard mitigation shall not rely on actions that require extensive maintenance.

C. Development near an erosion or landslide hazard area shall:

1. Observe a buffer from the edges thereof, of adequate width to comply with the substantive requirements;

2. Not decrease the factor of safety for landslides below the limits of 1.5 for static conditions and 1.2 for dynamic conditions. Analysis of dynamic conditions may be based on a minimum horizontal acceleration as established by the International Building Code;

3. Cluster structures and improvements as necessary to avoid hazard areas;

4. Use retaining walls that allow the retention of existing natural slopes when possible rather than graded artificial slopes;

5. Place utility lines and pipes in erosion and landslide hazard areas only when no other alternative is available and when the line or pipe can be installed above-ground in such a manner as to remain intact without leaks in the event of a slide;

6. Discharge water from surface water facilities and roof drains onto or upstream from an erosion or landslide hazard area only if:

a. Discharged at flow durations matching predeveloped conditions, with adequate energy dissipation, into existing channels; or

b. Dispersed upslope of the steep slope onto a low-gradient undisturbed buffer of adequate infiltrate capacity without increasing saturation of the slope; and

7. Locate any on-site sewage drain fields outside the hazard area and related buffers. (Ord. 1592 § 1, 2004).