SURFICIAL GEOLOGIC MAPPING OF THE PORTLAND METROPOLITAN AREA, OREGON
New, detailed surficial mapping encompassing the ever-growing Portland metropolitan area is in progress at the Oregon Department of Geology and Mineral Industries (DOGAMI) . This mapping will be produced using digitally compiled information from previous geologic mapping, interpretation of high-resolution lidar data, borehole data, and well log data (courtesy of the Oregon Water Resources Department), the National Resources Conservation Service's soil surveys, and some field data collection. Quaternary deposits resulting from landslides or mass-wasting, fluvial (streams and river) processes, the cataclysmic Missoula floods and man-made disturbances dominate the urban landscape. Outcrops of underlying lavas from the Miocene Columbia River Basalt Group and Pliocene-Pleistocene Boring volcanics can be found at the surface, producing relief of the higher elevations in the fore-arc basin where Portland is situated.
All or parts of twenty 7.5’ quadrangles of new mapping will be compiled and published as a surficial geologic map and assembled into an ESRI ArcGIS geodatabase by DOGAMI. Additionally, the collection of subsurface geologic data at DOGAMI will be compiled into a single geodatabase format, which should provide a base for 3D modeling of geotechnical parameters in the Portland area. The surficial mapping was also carried out in conjunction with the USGS’ Pacific Northwest Urban Corridor Geologic Mapping Project to produce a larger regional-scale geologic map of the Portland and Tualatin Basins in northwest Oregon and part of southwest Washington.