The following terms shall have the following meanings when used in this chapter and in other places in this code unless another meaning is clear from the use of the term:
“Alluvial fan”means a relatively flat to gently sloping mass of loose rock materials, shaped like an open fan or a segment of a cone, that has been deposited by a stream or debris flow at the place where it issues from a narrow mountain valley upon a plain or broad valley.
“Alluvium”means a general term for clay, silt, sand, gravel, or similar unconsolidated detrital materials, deposited during comparatively recent geologic time by a stream or other body of running water, as a sorted or semisorted sediment in the bed of the stream or on its floodplain or delta.
“Aquifer”is a subsurface, saturated geologic formation which produces, or is capable of producing, a sufficient quantity of water to serve as a private or public water supply.
“Aquifer recharge areas”means those areas which serve as critical ground water recharge areas and which are highly vulnerable to contamination from intensive land uses within these areas.
“Bedrock”means a general term for the rock, typically hard, consolidated geologic material, that underlies soil or other unconsolidated, superficial material.
“Critical areas”include the following areas and ecosystems:
3. Frequently flooded areas (flood hazard areas);
4. Geologically hazardous areas; and
5. Fish and wildlife habitat conservation areas.
“Debris avalanche”means a rapid and sudden sliding or flow of rock materials; or the deposits of such materials.
“Debris flow”means a moving mass of rock fragments, soil and mud, more than half of the particles being larger than sand size. Rapid debris flows can move up to one hundred sixty kilometers per hour.
“Debris torrent”means a violent and rushing mass of water, logs, boulders and other debris.
“Earthflow”means a mass-movement landform and process characterized by downslope translation of soil and weathered rock over a discrete basal shear surface within well defined lateral boundaries. Earthflows grade into mudflows through a continuous range associated with increasing water contact.
“Erosion hazard area”means any area identified by the U.S. Department of Agriculture Natural Resource Conservation Service as having a severe rill and interrill erosion hazard.
“Fault”means a fracture or a zone of fractures along which there has been displacement of the sides relative to each other.
“Fish and wildlife habitat conservation”means land management for maintaining species in suitable habitats within their natural geographic distribution so that isolated subpopulations are not created. This does not mean maintaining all individuals of all species at all times, but it does mean that cooperative and coordinated land use planning is critically important in the city.
“Fish and wildlife habitat conservation areas”include:
1. Areas with which endangered, threatened, and sensitive species have primary association;
2. Habitats and species of local importance;
3. Commercial and recreational shellfish areas;
4. Naturally occurring ponds under twenty acres and their submerged aquatic beds that provide fish or wildlife habitat;
6. Lakes, ponds, streams and rivers planted with game fish by a governmental or tribal entity; or
7. State natural area preserves and natural resource conservation areas.
8. “Fish and wildlife habitat conservation areas” are areas that serve a critical role in sustaining needed habitats and species for the functional integrity of the ecosystem, and which, if altered, may reduce the likelihood that the species will persist over the long term. These areas may include, but are not limited to, rare or vulnerable ecological systems, communities, and habitat or habitat elements including seasonal ranges, breeding habitat, winter range, and movement corridors and areas with high relative population density or species richness. Counties and cities may also designate locally important habitats and species. “Fish and wildlife habitat conservation areas” was amended to reflect statutory amendment in 2012 to RCW
36.70A.030 to not include such artificial features or constructs as irrigation delivery systems, irrigation infrastructure, irrigation canals, or drainage ditches that lie within the boundaries of, and are maintained by, a port district or an irrigation district or company.
“Flood hazard area”means an area of “special flood hazard” identified pursuant to PMC 16.18.320.
“Geologically hazardous area”means an area that, because of its susceptibility to erosion, sliding, earthquake or other geological event, is not suited to the siting of commercial, residential or industrial development consistent with public health or safety concerns. “Geologically hazardous area” includes any erosion hazard area, landslide hazard area, seismic hazard area, mine hazard area, and volcanic hazard area.
“Gradient”means a degree of inclination, or a rate of ascent or descent, of an inclined part of the earth’s surface with respect to the horizontal; the steepness of a slope. It is expressed as a ratio (vertical to horizontal), a fraction (such as meters/kilometers or feet/miles), a percentage (of horizontal distance), or an angle (in degrees).
“Joint”means a surface of fracture or parting in a rock, without lateral displacement; the surface is usually planar and commonly occurs in groups to form a joint set.
“Lahar”means a mudflow or debris flow (mass movement) composed chiefly of volcaniclastic materials on the flank of a volcano. The debris carried in the flow includes pyroclasts, blocks from primary lava flows, and other rock debris.
“Landslide”means a general term covering a wide variety of mass movement landforms and processes involving the downslope transport, under gravitational influence, of soil and rock material en masse. Included are debris flows, debris avalanches, earthflows, mudflows, slumps, mudslides, rockslides and rock falls.
“Landslide hazard area”means an area subject to landslides based on a combination of geologic, topographic, and hydraulic factors. A landslide hazard area includes any area susceptible because of any combination of bedrock, soil, slope (gradient), slope aspect, structure, hydrology, or other factors. Examples of these areas may include, but are not limited to, the following:
1. Areas designated as slumps, earth flows, mudflows, lahars, or landslides on maps published by the U.S. Geological Survey;
2. Slope stability maps for the Pomeroy area provided by the Washington State Department of Natural Resources Division of Geology and Earth Resources;
3. City of Pomeroy critical areas inventory maps as the same exist now or may be hereafter developed and/or amended;
4. Areas with all three of the following characteristics: Slopes steeper than fifteen percent, hillsides intersecting geologic contacts with a relatively permeable sediment overlying a relatively impermeable sediment or bedrock, and springs or groundwater seepage;
5. Any areas of old landslide deposits;
6. Slopes that are parallel or subparallel to planes of weakness, such as bedding planes, joint systems, and fault planes in subsurface materials;
7. Areas potentially unstable as a result of rapid stream incision, stream bank erosion, and undercutting by wave action;
8. Areas that show evidence of, or are at risk from, snow avalanches;
9. Areas located in a canyon, ravine or bluff; and
10. Any area with a slope of thirty-five percent or steeper and with a vertical relief of ten or more feet.
“Mass wasting” (also known as “mass movement”)means a general term for the dislodgement and downslope transport of soil and rock material under the direct application of gravitational body stresses. Mass wasting includes slow displacements, such as creep and solifluction, and rapid movements such as rock falls, rockslides, and mud, earth and debris flows.
“Mine hazard area”means an area directly underlain by, adjacent to or affected by mine workings such as adits, tunnels, drifts or airshafts. Mine hazard areas may also include steep and unstable slopes created by open mines.
“Mineral resource area”means land that is not already characterized by urban growth and is of long-term commercial significance for the extraction of minerals, including gravel, sand and valuable metallic substances.
“Mudflow”means a general term for a mass movement landform and a process characterized by a flowing mass of predominantly fine-grained earth material possessing a high degree of fluidity during movement. If more than half of the solid fraction of such a mass consists of material larger than sand size, the term “debris flow” is preferable. The water content of mudflows may range up to sixty percent; with increasing fluidity, mudflows grade into muddy floods; with less fluidity, mudflows grade into earth flows.
“Mudslide”means a relatively slow-moving mudflow in which movement occurs predominantly by sliding upon a discrete boundary shear surface.
“Pyroclastic”means pertaining to clastic rock material formed by volcanic explosion or aerial expulsion from a volcanic vent.
“Pyroclastic flow”means hot clouds of ash, gas, and volcanic rock that flow rapidly down slope under gravity. These may flow at velocities up to one hundred fifty kilometers per hour. It is a synonym of ash flow, and may be projected from a laterally directed blast.
“Rill”means a steep-sided channel resulting from accelerated erosion. A rill generally is a few inches deep and not wide enough to be an obstacle for farm machinery. Rill erosion tends to occur on steep slopes with poor vegetative cover.
“Seismic hazard area”is an area posing significant, predictable hazards to life and property resulting from earthquakes and the associated ground shaking, differential settlement, and/or soil liquefaction.
“Slope”means:
2. The inclined surface of any part on the earth’s surface. It is delineated by establishing its toe and top, and measured by averaging the inclination over at least ten feet of vertical relief.
“Slope failure”means gradual or rapid downslope movement of soil or rock under gravitational stress.
“Slump”means a landslide characterized by a shearing and rotary movement of a generally independent mass of rock or earth along a curved slip surface by backward tilting of the mass. Slumps occur in unconsolidated materials and are often the result of undercutting or steepening of the slope.
“Soil”means the upper layers of ground, consisting of unconsolidated materials typically made up of broken and decomposed rock and decayed organic matter.
“Tephra”is a collective term for all size grades of particles of solidified magma blown out under gas pressure from a volcanic vent.
“Toe”means:
1. The lowest part of a slope or cliff;
2. The downslope end of an alluvial fan; or
“Top”means:
2. The highest point of contact above a land-slide hazard area.
“Volcanic hazard area”means an area subject to pyroclastic flows, lateral blasts, tephra, lava flows, and inundation by debris flows, mudflows, avalanches, or related flooding resulting from volcanic activity.
“Wetland(s)”means areas that are inundated or saturated by surface water or ground water at a frequency and duration sufficient to support, and that under normal circumstances do support, a prevalence of vegetation typically adapted for life in saturated soil conditions. Wetlands generally include swamps, marshes, bogs and similar areas. Wetlands do not include those artificial wetlands intentionally created from nonwetland sites, including but not limited to irrigation and drainage ditches, grassline swales, canals, detention facilities, wastewater treatment facilities, farm ponds, landscaped amenities or those wetlands created after July 1, 1990, that were unintentionally created as a result of the construction of a road, street or highway. Wetlands may include artificial wetlands intentionally created from nonwetland areas to mitigate conversion of wetland.
“Wetland professional”means a qualified professional for wetlands who must be a professional wetland scientist with at least two years of full-time work experience as a wetlands professional, including delineating wetlands using the federal manual and supplements, preparing wetlands reports, conducting function assessments, and developing and implementing mitigation plans.
(Ord. 804 § 1 (part), 2004; Ord. 910, 2019)