Seismic hazard areas definition

Seismic hazard areas means areas that are subject to severe risk of damage as a result of earthquake-induced ground shaking, slope failure, settlement, or soil liquefaction.

Seismic hazard areas means areas subject to severe risk of damage as a result of earthquake- induced ground shaking, slope failure, settlement, soil liquefaction, debris flows, lahars, or tsunamis.

Seismic hazard areas means areas that are subject to severe risk of damage

Examples of Seismic hazard areas in a sentence

• 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.

• Seismic hazard areas are lands that, due to a combination of soil and ground water conditions, are subject to severe risk of ground shaking, lateral spreading, subsidence or liquefaction of soils during earthquakes.

• Seismic hazard areas are subject to severe risk of damage as a result of earthquake-induced ground shaking, slope failure, settlement, soil liquefaction, lateral spreading, or surface failure.

• Seismic hazard areas are areas subject to a severe risk of earthquake damage as a result of seismically induced ground shaking, slope failure, deferential settlement, soil liquefaction, or surface faulting.

• 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.

More Definitions of Seismic hazard areas

Seismic hazard areas means the following:

Seismic hazard areas means areas subject to severe risk of damage as a result of earthquake-

Seismic hazard areas means areas that are subject to severe risk of damage as a result of earthquake induced ground shaking, slope failure, settlement or subsidence, surface faulting, or soil liquefaction. Settlement and soil liquefaction conditions occur in areas underlain by cohesionless (soft or loose) soils of low density (such as alluvium), typically in association with a shallow groundwater table and are typically located on the floors of river valleys. One indicator of potential for future earthquake damage is a record of earthquake damage in the past. Ground shaking is the primary cause of earthquake damage in Washington, and ground settlement may occur with shaking. The strength of ground shaking is primarily affected by:

Seismic hazard areas means those areas subject to severe risk of earthquake damage as a result of soil liquefaction in areas underlain by cohesionless soils of low density and usually in association with a shallow groundwater table or of other seismically induced settlement.

Seismic hazard areas means areas subject to severe risk of earthquake damage as a result of seismic induced settlement or soil liquefaction.

Seismic hazard areas means areas that, due to a combination of soil and ground water conditions, are subject to risk of ground shaking, subsidence or liquefaction of soils during earthquakes. These areas are typically underlain by soft or loose saturated soils (such as alluvium), have a shallow ground water table and are typically located on the floors of river valleys.

Seismic hazard areas means areas subject to severe risk of damage as a result of earthquake induced ground shaking, slope failure, settlement, soil liquefaction, debris flows, or tsunamis. The following areas are considered seismic hazard areas: