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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Mark D. Petersen</dc:contributor>
  <dc:contributor>Peter M. Powers</dc:contributor>
  <dc:contributor>Sanaz Rezaeian</dc:contributor>
  <dc:creator>Allison Shumway</dc:creator>
  <dc:date>2018</dc:date>
  <dc:description>&lt;p&gt;The 2014 update of the U.S. Geological Survey (USGS) National Seismic Hazard Model (NSHM) for the conterminous&amp;nbsp;United States (2014 NSHM; Petersen and others, 2014, 2015) included probabilistic ground motion maps for 2 percent and&amp;nbsp;10 percent probabilities of exceedance in 50 years, derived from seismic hazard curves for peak ground acceleration (PGA) and&amp;nbsp;0.2 and 1.0 second spectral accelerations (SAs) with 5 percent damping for the National Earthquake Hazards Reduction Program&amp;nbsp;(NEHRP) site class boundary B/C (time-averaged shear wave velocity in the upper 30 meters [V&lt;sub&gt;S30&lt;/sub&gt;]=760 meters per second&amp;nbsp;[m/s]). We now provide uniform NEHRP site class maps for 2, 5, and 10 percent probabilities of exceedance in 50 years derived&amp;nbsp;from hazard curves for additional spectral periods. For the central and eastern United States (CEUS) and western United States&amp;nbsp;(WUS), hazard curves and maps for PGA, 0.1, 0.2, 0.3, 0.5, 1.0, and 2.0 second SAs are now available. The WUS additionally&amp;nbsp;includes hazard curves and maps for 0.75, 3.0, 4.0, and 5.0 second SAs. The use of region-specific suites of weighted ground&amp;nbsp;motion models (GMMs) in the 2014 NSHM precluded the calculation of ground motions for a uniform set of periods and site&amp;nbsp;classes for the conterminous United States. At the time of the development of the 2014 NSHM, there was no consensus in the&amp;nbsp;CEUS on an appropriate site-amplification model to use; therefore, we calculated hazard curves and maps for NEHRP site class A,&amp;nbsp;for which most stable continental GMMs were originally developed, based on simulations for hard rock site conditions (V&lt;sub&gt;S30&lt;/sub&gt;=2,000 m/s).&amp;nbsp;In the WUS, however, the active crustal Next Generation Attenuation Relationships for the WUS (NGA-West2 GMMs) and&amp;nbsp;subduction GMMs allow amplification of ground motions based on site class (defined by V&lt;sub&gt;S30&lt;/sub&gt;); so we calculated hazard curves&amp;nbsp;and maps for NEHRP site classes B (V&lt;sub&gt;S30&lt;/sub&gt;=1,080 m/s), C (V&lt;sub&gt;S30&lt;/sub&gt;=530 m/s), D (V&lt;sub&gt;S30&lt;/sub&gt;=260 m/s), and E (V&lt;sub&gt;S30&lt;/sub&gt;=150 m/s) and site class&amp;nbsp;boundaries A/B (V&lt;sub&gt;S30&lt;/sub&gt;=1,500 m/s), B/C (V&lt;sub&gt;S30&lt;/sub&gt;=760 m/s), C/D (V&lt;sub&gt;S30&lt;/sub&gt;=365 m/s), and D/E (V&lt;sub&gt;S30&lt;/sub&gt;=185 m/s). The 2014 NSHM introduced&amp;nbsp;a set of criteria for selecting GMMs for use in the NSHMs. When calculating additional period and site class maps, we verified&amp;nbsp;whether the 2014 NSHM original suites of GMMs satisfied these ground motion selection criteria at all additional periods and&amp;nbsp;site classes using GMM magnitude-distance scaling relation plots. Results of our analysis show that certain GMMs give unrealistic&amp;nbsp;results at longer periods, distances, and softer soils in the WUS. In these rare instances, the GMM was removed from the original&amp;nbsp;suite of GMMs (for all periods and site classes) and the weights of the remaining GMMs in the suite were renormalized. Ratio&amp;nbsp;maps show these updated suites of weighted GMMs result in probabilistic ground motion changes of less than 10 percent in&amp;nbsp;the WUS at PGA, as well as 0.2 and 1.0 second SAs, except in the Pacific Northwest, where differences as much as 20 percent&amp;nbsp;are seen. Hazard curves and uniform hazard response spectra at test sites across the conterminous United States were produced to&amp;nbsp;verify that results were reasonable. The additional period and site class maps, and the hazard curves from which they were derived,&amp;nbsp;are available for download from the USGS ScienceBase Catalog.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20181111</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Additional period and site class maps for the 2014 National Seismic Hazard Model for the conterminous United States</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>