Oregon Department of Geology and Mineral Industries
2018
Site ground motion (spectral acceleration at 0.3 second) for a simulated Cascadia Subduction Zone M 9.0 earthquake, Clackamas, Multnomah, and Washington Counties, Oregon
raster digital data
Oregon Department of Geology and Mineral Industries Open-File Report
Open-File Report O-18-02
Portland, Oregon, USA
Oregon Department of Geology and Mineral Industries
http://www.oregongeology.org
Oregon Department of Geology and Mineral Industries
2018
Earthquake regional impact analysis for Clackamas, Multnomah, and Washington Counties, Oregon
file geodatabase
Oregon Department of Geology and Mineral Industries Open-File Report
Open-File Report O-18-02
Portland, Oregon, USA
Oregon Department of Geology and Mineral Industries
http://www.oregongeology.org/
Spectral acceleration at 0.3 second period that is estimated to occur at a location on the soil surface for a simulated earthquake. It is quantified as a proportion of standard acceleration due to gravity (or g).
To provide sa03 (spectral acceleration at 0.3 second) site ground motion information throughout the study area from a simulated Cascadia Subduction Zone M 9.0 earthquake. Used in building and infrastructure damage models.
sa03 is the maximum ground acceleration at 0.3 second period that estimated to occur during earthquake shaking at a particular location. This is a simulated earthquake, or a 'scenario', which represents one realization of a potential future earthquake by assuming a particular magnitude, location, and fault-rupture geometry and estimating shaking using a variety of strategies.
2018
None planned
ISO 19115 Topic Category
geoscientificinformation
Oregon Geospatial Enterprise Office Metadata Keyword Thesaurus
ground motion
ground shaking
earthquake
active fault
strong motion
earthquake hazard
earthquake occurrence
acceleration
Oregon Geospatial Enterprise Office Metadata Keyword Thesaurus
Clackamas
Multnomah
Washington
Oregon Geospatial Enterprise Office Metadata Keyword Thesaurus
Land surface
Oregon Geospatial Enterprise Office Metadata Keyword Thesaurus
None
REPORT DATA: This product is for informational purposes and may not have been prepared for or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to ascertain the usability of the information. This publication cannot substitute for site-specific investigations by qualified practitioners. Site-specific data may give results that differ from the results shown in the publication. See the accompanying text report for more details on the limitations of the methods and data used to prepare this publication.
Oregon Department of Geology and Mineral Industries
mailing and physical address
800 NE Oregon Street Suite 965
Portland
Oregon
97232
USA
1 971 673 1555
1 971 673 1562
dogami-info@oregon.gov
When contacting DOGAMI about this data set, please reference the data set title or other identifying information in your correspondence. DOGAMI publications can be downloaded from http://www.oregongeology.org
John Bauer
Oregon Department of Geology and Mineral Industries
Geohazards Analyst
jpeg image (.jpg)
This work was funded on behalf of Regional Disaster Preparedness Organization with an Urban Area Security Initiative grant for the Portland Metropolitan Region.
Unclassified
Site ground motion developed based on bedrock ground motion, which is a model of a Cascadia Subduction Zone fault. An actual subduction zone earthquake will likely vary significantly in magnitude and in attenuation from the simulated earthquake. Site response is driven by the NEHRP site classification, which was driven by surficial geologic unit designations. Site response can vary significantly, depending on particulars and depth of the soil column relative to the underlying bedrock. The NEHRP site amplification functions are an approximation and generalization of the site effect. Sites classified as "F" were given an "E" rating for loss modeling purposes, and have the largest uncertainty.
Maximum, minimum, average of continuous data is consistent with expectations. Spatial pattern of data consistent with the NEHRP site designations and the expected amplification, given the bedrock ground motion.
All three three counties are fully represented with data. Areas outside of the three counties are represented as NoData.
Site ground motion developed based on bedrock ground motion, which is a model of a Cascadia Subduction Zone fault. An actual earthquake along the CSZ will likely vary significantly in magnitude and in attenuation, compared to the simulated earthquake. Site response is driven by the NEHRP site classification, itself based on geologic polygons drawn at a range of scales, from 1:4000 to 1:24000 in the study area.
not applicable
Oregon Department of Geology and Mineral Industries
2013
Ground motion, ground deformation, tsunami inundation, coseismic subsidence, and damage potential maps for the 2012 Oregon Resilience Plan for Cascadia subduction zone earthquakes
raster digital data
Oregon Department of Geology and Mineral Industries Open-File Report
O-13-06
Portland, Oregon
Oregon Department of Geology and Mineral Industries
Raster dataset: Oregon_M_9_Scenario_Bedrock_SA03
http://www.oregongeology.org/pubs/ofr/p-O-13-06.htm
2013
Oregon Department of Geology and Mineral Industries
2018
NEHRP Site Classification for Clackamas, Multnomah, and Washington Counties, Oregon
vector digital data
Oregon Department of Geology and Mineral Industries Open-File Report
In preparation
Portland, Oregon
Oregon Department of Geology and Mineral Industries
1:4000 - 1:100000
The sa03 bedrock grid from DOGAMI, 2013, was resampled to a 30-ft grid. The NEHRP Site Classification was converted to a 30-ft grid, designating the location as either B, C, D, or E. All sites designated as NEHRP "F" were converted to NEHRP "E".
Site ground motion calculations were performed using the equations listed in the accompanying report, Table 11-1.
Oregon Department of Geology and Mineral Industries
mailing and physical address
800 NE Oregon Street Suite 965
Portland
Oregon
97232
USA
1 971 673 1555
1 971 673 1562
dogami-info@oregon.gov
When contacting DOGAMI about this data set, please reference the data set title or other identifying information in your correspondence. DOGAMI publications can be downloaded from http://www.oregongeology.org
VALUE
Spectral acceleration at 0.3 s, in percent g (acceleration of gravity)
Standard descriptors of strong ground motion that are used in earthquake damage analysis
Oregon Department of Geology and Mineral Industries
mailing and physical address
800 NE Oregon Street Suite 965
Portland
Oregon
97232
USA
1 971 673 1555
1 971 673 1562
dogami-info@oregon.gov
When contacting DOGAMI about this data set, please reference the data set title or other identifying information in your correspondence. DOGAMI publications can be downloaded from http://www.oregongeology.org
Although these data have been processed successfully on a computer system at the Oregon Department of Geology and Mineral Industries, no warranty expressed or implied is made by DOGAMI regarding the utility of the data on any other system, nor shall the act of distribution constitute any such warranty.
Oregon Department of Geology and Mineral Industries
mailing and physical address
800 NE Oregon Street Suite 965
Portland
Oregon
97232
USA
1 971 673 1555
1 971 673 1562
dogami-info@oregon.gov
When contacting DOGAMI about this data set, please reference the data set title or other identifying information in your correspondence. DOGAMI publications can be downloaded from http://www.oregongeology.org
Oregon Department of Geology and Mineral Industries Metadata Standard
1.4
None
None
None
None
None
To provide sa03 (spectral acceleration at 0.3 second) site ground motion information throughout the study area from a simulated Cascadia Subduction Zone M 9.0 earthquake. Used in building and infrastructure damage models.
<DIV STYLE="text-align:Left;"><DIV><P><SPAN>Spectral acceleration at 0.3 second period that is estimated to occur at a location on the soil surface for a simulated earthquake. It is quantified as a proportion of standard acceleration due to gravity (or g).</SPAN></P></DIV></DIV>
This work was funded on behalf of Regional Disaster Preparedness Organization with an Urban Area Security Initiative grant for the Portland Metropolitan Region.
Site ground motion (spectral acceleration at 0.3 second) for a simulated Cascadia Subduction Zone M 9.0 earthquake, Clackamas, Multnomah, and Washington Counties, Oregon
geoscientificinformation
ground motion
ground shaking
earthquake
active fault
strong motion
earthquake hazard
earthquake occurrence
acceleration
<DIV STYLE="text-align:Left;"><DIV><P><SPAN>REPORT DATA: This product is for informational purposes and may not have been prepared for or be suitable for legal, engineering, or surveying purposes. Users of this information should review or consult the primary data and information sources to ascertain the usability of the information. This publication cannot substitute for site-specific investigations by qualified practitioners. Site-specific data may give results that differ from the results shown in the publication. See the accompanying text report for more details on the limitations of the methods and data used to prepare this publication.</SPAN></P></DIV></DIV>
Esri ArcGIS 12.8.0.29751
1
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45.809191
44.853936
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12085800
150000000
5000
1.0
FGDC
CSZ_M9p0_sa03_site
002
545817.745635
1015137.745635
1145201.050827
1481801.050827
1
Projected
GCS_North_American_1983_HARN
Linear Unit: Foot (0.304800)
NAD_1983_HARN_Oregon_Statewide_Lambert_Feet_Intl
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File Geodatabase Raster Dataset
dataset
EPSG
6.12(9.0.0)
Pixel
11220
15644
30.000000
30.000000
32
1
Upper Left
FALSE
NONE
1
pixel codes
FGDBR
TRUE
row and column
30.000000
30.000000
20220823