3 Geoscience Education (Posters)

Thursday, 7 May 2009
8:30 AM - 5:30 PM

MAKING GEOLOGICAL HAZARD MAPS FROM HIGH-RESOLUTION GEOLOGICAL MAPS AND A SUBSURFACE DATABASE, MERCER ISLAND, WA

Paper number: 3-4
Program: Technical Sessions
Time: 8:30 AM – 5:30 PM

Authors

Abstract

The City of Mercer Island, in the Puget Lowland of Washington, recently updated its geological hazard maps in accordance with State regulations and the Growth Management Act. Guidance for mapping geological hazards is provided in Washington Administrative Code 365-190-080. “Geologically hazardous areas”, by State definition, “include areas susceptible to erosion, sliding, earthquake, or other geological events. They pose a threat to the health and safety of citizens when incompatible commercial, residential, or industrial development is sited in areas of significant hazard.” The City's suite of maps includes maps showing Seismic Hazards, Slope Hazards, and Erosion Hazards. This new set of maps represents an update of the 2002 Geologic Hazard Map Series and is based on a review of Best Available Science for the Seattle Fault and related events, a new high-resolution Geological Map of Mercer Island, a database of subsurface explorations, and depth to water data.

Comparison of the 2009 to the 2002 geological hazard maps reveals many differences and updates. The main difference between the two maps stems from the underlying geologic base map. The 2002 maps are based on a 1962, 1:63,500 scale geological map. The 2009 maps are based on a 2006 1:12,000 geological map with 4 times the level of detail of the 1962 map. The new geological map was constructed using a database of 2800 subsurface explorations and 164 exposure data points. LIDAR data were used to provide a high-resolution base for geomorphic analyses, mapping of scarps, identification of landslide deposits, and slope classifications allowing the new maps to be both more precise and more accurate. Updated 2009 maps include inventories of landslides, mapping of spring locations, depth to water data, mapping of subaqueous landslides, mapping of critical geological contacts, mapping of infiltration potential, mapping of weak deposits, and mapping of fill materials. A major change to the seismic hazard map is the addition of the Seattle fault zone, an active crustal thrust fault.

City planners and building officials will use these maps to enforce their critical areas codes, building codes, and building permit requirements. These maps also help inform the citizens about the risks and hazards inherent in living and working in the area.