<?xml version="1.0" encoding="UTF-8"?>
<metadata>
  <idinfo>
    <citation>
      <citeinfo>
        <origin>SeanPaul M. La Selle</origin>
        <origin>Alan R. Nelson</origin>
        <origin>Robert C. Witter</origin>
        <origin>Guy Gelfenbaum</origin>
        <origin>Jason S. Padgett</origin>
        <origin>Bruce E. Jaffe</origin>
        <pubdate>20240417</pubdate>
        <title>Thickness distribution of the most recent sandy tsunami deposit in the Salmon River estuary, Oregon</title>
        <geoform>comma-delimited text</geoform>
        <serinfo>
          <sername>data release</sername>
          <issue>DOI: 10.5066/P9M86S7D</issue>
        </serinfo>
        <pubinfo>
          <pubplace>Pacific Coastal and Marine Science Center, Santa Cruz, California</pubplace>
          <publish>U.S. Geological Survey</publish>
        </pubinfo>
        <onlink>https://doi.org/10.5066/P9M86S7D</onlink>
        <lworkcit>
          <citeinfo>
            <origin>SeanPaul M. La Selle</origin>
            <origin>Alan R. Nelson</origin>
            <origin>Robert C. Witter</origin>
            <origin>Jason S. Padgett</origin>
            <origin>Bruce E. Jaffe</origin>
            <origin>Guy Gelfenbaum</origin>
            <pubdate>2024</pubdate>
            <title>Tsunami deposit data and sediment transport models from the Salmon River estuary, central Oregon</title>
            <serinfo>
              <sername>data release</sername>
              <issue>DOI: 10.5066/P9M86S7D</issue>
            </serinfo>
            <pubinfo>
              <pubplace>Pacific Coastal and Marine Science Center, Santa Cruz, CA</pubplace>
              <publish>U.S. Geological Survey</publish>
            </pubinfo>
            <othercit>Suggested Citation: Suggested Citation: La Selle, S.M., Nelson, A.R., Witter, R.C., Padgett, J.S., Jaffe, B.E., Gelfenbaum, G., 2024, Tsunami deposit data and sediment transport models from the Salmon River, central Oregon coast: U.S. Geological Survey data release, https://doi.org/10.5066/P9M86S7D.</othercit>
            <onlink>https://doi.org/10.5066/P9M86S7D</onlink>
          </citeinfo>
        </lworkcit>
      </citeinfo>
    </citation>
    <descript>
      <abstract>This portion of the data release provides the spatial thickness distribution of sandy deposits inferred to have been deposited at the Salmon River, OR by a circa 1700 CE tsunami. Data were collected by describing hand-operated gouge cores at 129 sites in 2017 and 2018, and supplemented by 114 core descriptions from 1987 (Nelson and others, 2004).</abstract>
      <purpose>In the absence of detailed historical records of tsunami inundation along the Cascadia subduction zone, the geologic evidence of such events can be used to reconstruct the size and slip distribution of prehistoric earthquakes and tsunamis. The tsunami deposit thickness data presented in this portion of the data release can be used to infer the minimum inundation extent of a ca. 1700 CE tsunami and can be used to test models of earthquake rupture and tsunami sediment transport.</purpose>
      <supplinf>Additional information about the field activity or activities from which these data were derived is available online at:
https://cmgds.marine.usgs.gov/fan_info.php?fan=2017-643-FA
https://cmgds.marine.usgs.gov/fan_info.php?fan=2018-625-FA

Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.</supplinf>
    </descript>
    <timeperd>
      <timeinfo>
        <rngdates>
          <begdate>19870902</begdate>
          <enddate>20180515</enddate>
        </rngdates>
      </timeinfo>
      <current>ground condition at time data were collected</current>
    </timeperd>
    <status>
      <progress>Complete</progress>
      <update>None planned</update>
    </status>
    <spdom>
      <bounding>
        <westbc>-123.99883</westbc>
        <eastbc>-122.97704</eastbc>
        <northbc>45.03989</northbc>
        <southbc>45.023606</southbc>
      </bounding>
    </spdom>
    <keywords>
      <theme>
        <themekt>USGS Metadata Identifier</themekt>
        <themekey>USGS:fd531723-31bf-4671-a2b3-1e19bbffb979</themekey>
      </theme>
      <theme>
        <themekt>ISO 19115 Topic Category</themekt>
        <themekey>geoscientificInformation</themekey>
      </theme>
      <theme>
        <themekt>Data Categories for Marine Planning</themekt>
        <themekey>Substrate</themekey>
      </theme>
      <theme>
        <themekt>USGS Thesaurus</themekt>
        <themekey>tsunami</themekey>
        <themekey>sediment transport</themekey>
        <themekey>deposit</themekey>
      </theme>
      <theme>
        <themekt>Marine Realms Information Bank (MRIB) keywords</themekt>
        <themekey>sediment</themekey>
        <themekey>Global Positioning System observations</themekey>
      </theme>
      <theme>
        <themekt>None</themekt>
        <themekey>U.S. Geological Survey</themekey>
        <themekey>USGS</themekey>
        <themekey>Coastal and Marine Hazards and Resources Program</themekey>
        <themekey>CMHRP</themekey>
        <themekey>Pacific Coastal and Marine Science Center</themekey>
        <themekey>PCMSC</themekey>
      </theme>
      <place>
        <placekt>Geographic Names Information System</placekt>
        <placekey>Salmon River</placekey>
        <placekey>Lincoln County</placekey>
        <placekey>State of Oregon</placekey>
      </place>
    </keywords>
    <accconst>None</accconst>
    <useconst>USGS-authored or produced data and information are in the public domain from the U.S. Government and are freely redistributable with proper metadata and source attribution. Please recognize and acknowledge the U.S. Geological Survey as the originator(s) of the dataset and in products derived from these data.</useconst>
    <ptcontac>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey, Pacific Coastal and Marine Science Center</cntorg>
          <cntper>PCMSC Science Data Coordinator</cntper>
        </cntorgp>
        <cntaddr>
          <addrtype>mailing and physical</addrtype>
          <address>2885 Mission Street</address>
          <city>Santa Cruz</city>
          <state>CA</state>
          <postal>95060</postal>
        </cntaddr>
        <cntvoice>831-427-4747</cntvoice>
        <cntemail>pcmsc_data@usgs.gov</cntemail>
      </cntinfo>
    </ptcontac>
    <browse>
      <browsen>deposit_preview.jpg</browsen>
      <browsed>Photo of the buried soil, tsunami sand, and post-tsunami tidal silt from a core in the Salmon River estuary, OR.</browsed>
      <browset>JPG</browset>
    </browse>
    <native>Microsoft Windows 10 running Microsoft Excel</native>
    <crossref>
      <citeinfo>
        <origin>SeanPaul M. La Selle</origin>
        <origin>Alan R. Nelson</origin>
        <origin>Robert C. Witter</origin>
        <origin>Guy Gelfenbaum</origin>
        <origin>Jason S. Padgett</origin>
        <origin>Bruce E. Jaffe</origin>
        <pubdate>2024</pubdate>
        <title>Testing megathrust rupture models using tsunami deposits</title>
        <othercit>La Selle, S.M., Nelson, A.R., Witter, R.C., Gelfenbaum, G., Padgett, J.S., and Jaffe, B.E., 2024, Testing megathrust rupture models using tsunami deposits: Journal of Geophysical Research: Earth Surface, https://doi.org/10.1029/2023JF007444.</othercit>
        <onlink>https://doi.org/10.1029/2023JF007444</onlink>
      </citeinfo>
    </crossref>
    <crossref>
      <citeinfo>
        <origin>J. Troels-Smith</origin>
        <pubdate>1955</pubdate>
        <title>Karakterisering af lo se jordarter (Characterisation of Unconsolidated Sediments)</title>
        <othercit>Troels-Smith, J., 1955, Karakterisering af lo se jordarter (Characterisation of Unconsolidated Sediments): Geologiske Undersogelse, v. 3, p. 39-73.</othercit>
        <onlink>https://doi.org/10.34194/raekke4.v3.6989</onlink>
      </citeinfo>
    </crossref>
    <crossref>
      <citeinfo>
        <origin>Alan R. Nelson</origin>
        <pubdate>2015</pubdate>
        <title>Chapter 4: Coastal Sediments</title>
        <pubinfo>
          <pubplace>West Sussex, UK</pubplace>
          <publish>Wiley-Blackwell</publish>
        </pubinfo>
        <othercit>Nelson, A.R., 2015, Chapter 4: Coastal Sediments: Handbook of Sea-level Research. Wiley-Blackwell</othercit>
        <onlink>https://doi.org/10.1002/9781118452547.ch4</onlink>
      </citeinfo>
    </crossref>
  </idinfo>
  <dataqual>
    <attracc>
      <attraccr>No formal attribute accuracy tests were conducted.</attraccr>
    </attracc>
    <logic>No formal logical accuracy tests were conducted.</logic>
    <complete>Dataset is considered complete for the information presented, as described in the abstract. Users are advised to read the rest of the metadata record carefully for additional details.</complete>
    <posacc>
      <horizpa>
        <horizpar>The locations of sites from 2017 and 2018 were determined using a Garmin etrex 30x handheld global satellite navigation system (GNSS) receiver capable of receiving wide area augmentation system (WAAS) signals. The manufacturer reported accuracy for horizontal positions is 3-5 m while receiving WAAS signals. Positional accuracy from the georeferenced 1987 cores is assumed to be worse than 5 m, due to errors in triangulation and digital georeferencing.</horizpar>
      </horizpa>
      <vertacc>
        <vertaccr>No formal positional accuracy tests were conducted, nor were they applicable for this dataset.</vertaccr>
      </vertacc>
    </posacc>
    <lineage>
      <srcinfo>
        <srccite>
          <citeinfo>
            <origin>Alan R. Nelson</origin>
            <origin>Andrew C. Asquith</origin>
            <origin>Wendy C. Grant</origin>
            <pubdate>2004</pubdate>
            <title>Great earthquakes and tsunamis of the past 2000 years at the Salmon River estuary, central Oregon coast, USA</title>
            <geoform>Raster Digital</geoform>
            <pubinfo>
              <pubplace>online</pubplace>
              <publish>Seismological Society of America</publish>
            </pubinfo>
            <onlink>https://doi.org/10.1785/012003210</onlink>
          </citeinfo>
        </srccite>
        <typesrc>Hardcopy Resources (photographs and photocopied field notes).</typesrc>
        <srctime>
          <timeinfo>
            <rngdates>
              <begdate>19870902</begdate>
              <enddate>19880901</enddate>
            </rngdates>
          </timeinfo>
          <srccurr>ground condition at time data were collected</srccurr>
        </srctime>
        <srccitea>Nelson and others, (2004)</srccitea>
        <srccontr>Legacy core locations and descriptions</srccontr>
      </srcinfo>
      <procstep>
        <procdesc>Legacy core locations and descriptions collected by Wendy G. Walter in 1987 and published in Nelson and others, (2004) were georeferenced and reanalyzed to extract tsunami deposit thicknesses and the presence or absence of a buried soil horizon. Original core locations were determined through triangulation and annotated onto aerial photos. These photos were georeferenced in a geographic information system to determine the latitude and longitude for each site. Uncertainty in the 1987 core locations is unknown but assumed to be greater than the positional accuracy of GNSS-derived positions. The 1987 core descriptions note the depth of sandy layers and buried soil horizons that were originally interpreted to be from the 26 January, 1700 earthquake and tsunami.</procdesc>
        <srcused>Nelson and others, (2004)</srcused>
        <procdate>20170601</procdate>
      </procstep>
      <procstep>
        <procdesc>The USGS collected cores from the Salmon River estuary in 2017 and 2018. Cores were described in the field and the presence or absence of a buried soil horizon was noted. Stratigraphy was described using the sediment classification schemes outlined in Troels-Smith (1955) and Nelson (2015). If present, depths and thicknesses of the sand layer immediately above the buried soil horizon were recorded. At the far inland extent of the sandy tsunami deposits, where the visually estimated bulk grain size of the deposit was a mixture of very fine sand and silt, only sandy lamina 1 mm or greater in thickness were identifiable as sandy deposits.</procdesc>
        <procdate>20180515</procdate>
      </procstep>
    </lineage>
  </dataqual>
  <spdoinfo>
    <direct>Point</direct>
  </spdoinfo>
  <spref>
    <horizsys>
      <geograph>
        <latres>0.00001</latres>
        <longres>0.00001</longres>
        <geogunit>Decimal degrees</geogunit>
      </geograph>
      <geodetic>
        <horizdn>WGS_1984</horizdn>
        <ellips>WGS_1984</ellips>
        <semiaxis>6378137.0</semiaxis>
        <denflat>298.257223563</denflat>
      </geodetic>
    </horizsys>
  </spref>
  <eainfo>
    <detailed>
      <enttyp>
        <enttypl>salmonriver_thickness.csv</enttypl>
        <enttypd>Comma Separated Value (.csv) file containing sandy deposit thickness data.</enttypd>
        <enttypds>producer defined</enttypds>
      </enttyp>
      <attr>
        <attrlabl>field_activity_number</attrlabl>
        <attrdef>Field Activity Number. Data collected in 1987 and 1988 were not associated with a unique field activity number, indicated by “nan”.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <udom>Unique identifier for the U.S. Geological Survey field activity.</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>site_id</attrlabl>
        <attrdef>For USGS collected data (2017-2018): Name of site in LocalityYear-CoreID format, where LocalityYear is the first two letters of the field locality (SR = Salmon River) followed by the 2-digit year (17 = 2017, 18 = 2018), and core ID is the unique name given to a core. For non-USGS collected data (1987-1988): Name of site in LocalityCoreID format, where LocalityYear is the first two letters of the field locality (SR = Salmon River) and core ID is the unique name given to a core.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <udom>Unique identifier for the sample used given in the field</udom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>site_type</attrlabl>
        <attrdef>Type of coring device used to collect sediment and determine sand bed thicknesses.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <edom>
            <edomv>30 mm gouge</edomv>
            <edomvd>30 mm gouge cores are side-filling hand-operated peat-coring augers that are 100 cm and long and 30 mm in diameter.</edomvd>
            <edomvds>producer defined</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>60 mm gouge</edomv>
            <edomvd>60 mm gouge cores are side-filling hand-operated peat-coring augers that are 100 cm and long and 60 mm in diameter.</edomvd>
            <edomvds>producer defined</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>cut bank</edomv>
            <edomvd>Cutbanks are sites along tidal channels that expose the site stratigraphy without having to dig or core.</edomvd>
            <edomvds>producer defined</edomvds>
          </edom>
        </attrdomv>
        <attrdomv>
          <edom>
            <edomv>Russian core</edomv>
            <edomvd>Russian cores are side-filling hand operated peat-coring augers with a flap that traps sediment and are 50 cm long and 60 mm in diameter.</edomvd>
            <edomvds>producer defined</edomvds>
          </edom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>latitude</attrlabl>
        <attrdef>Latitude of site, in decimal degrees.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>45.02361</rdommin>
            <rdommax>45.03989</rdommax>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>longitude</attrlabl>
        <attrdef>Longitude of site, in decimal degrees.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>-123.99883</rdommin>
            <rdommax>-123.9645</rdommax>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>date_collected</attrlabl>
        <attrdef>Date on which stratigraphy at the site was observed in yyyy-mm-dd format.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>1987-09-02</rdommin>
            <rdommax>2018-05-15</rdommax>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>sand_top_depth_cm</attrlabl>
        <attrdef>The depth in centimeters from the surface to the top of the circa 1700 CE sandy tsunami deposit. Blank values indicate the absence of the sand.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>20</rdommin>
            <rdommax>98</rdommax>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>sand_top_depth_cm</attrlabl>
        <attrdef>The depth in centimeters from the surface to the bottom of the circa 1700 CE sandy tsunami deposit. Blank values indicate the absence of the sand.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>24</rdommin>
            <rdommax>98.1</rdommax>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>sand_thickness_cm</attrlabl>
        <attrdef>The thickness in centimeters of the circa 1700 CE sandy tsunami deposit.</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>0</rdommin>
            <rdommax>19.5</rdommax>
          </rdom>
        </attrdomv>
      </attr>
      <attr>
        <attrlabl>subsidence_contact_present</attrlabl>
        <attrdef>Boolean (1 = yes, 0 = no).</attrdef>
        <attrdefs>producer defined</attrdefs>
        <attrdomv>
          <rdom>
            <rdommin>0</rdommin>
            <rdommax>1</rdommax>
          </rdom>
        </attrdomv>
      </attr>
    </detailed>
    <overview>
      <eaover>The first line of the csv file is a header line.</eaover>
      <eadetcit>U.S. Geological Survey</eadetcit>
    </overview>
  </eainfo>
  <distinfo>
    <distrib>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey - CMGDS</cntorg>
        </cntorgp>
        <cntaddr>
          <addrtype>mailing and physical</addrtype>
          <address>2885 Mission Street</address>
          <city>Santa Cruz</city>
          <state>CA</state>
          <postal>95060</postal>
        </cntaddr>
        <cntvoice>1-831-427-4747</cntvoice>
        <cntemail>pcmsc_data@usgs.gov</cntemail>
      </cntinfo>
    </distrib>
    <resdesc>The thickness of the most recent sandy tsunami deposits in the Salmon River estuary are provided in a comma-separated-value (.csv) file.</resdesc>
    <distliab>Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty.</distliab>
    <stdorder>
      <digform>
        <digtinfo>
          <formname>Comma delimited text</formname>
          <formcont>A Comma Separated Value (.csv) file containing the locations, depths, and thicknesses of sandy tsunami deposits in the Salmon River estuary, OR.</formcont>
          <filedec>none</filedec>
          <transize>0.0156</transize>
        </digtinfo>
        <digtopt>
          <onlinopt>
            <computer>
              <networka>
                <networkr>https://doi.org/10.5066/P9M86S7D</networkr>
              </networka>
            </computer>
            <accinstr>Data and metadata can be downloaded using the Network_Resource_Name links and scrolling down to the "Environmental Data" section.</accinstr>
          </onlinopt>
        </digtopt>
      </digform>
      <fees>None</fees>
    </stdorder>
  </distinfo>
  <metainfo>
    <metd>20240420</metd>
    <metc>
      <cntinfo>
        <cntorgp>
          <cntorg>U.S. Geological Survey, Pacific Coastal and Marine Science Center</cntorg>
          <cntper>PCMSC Science Data Coordinator</cntper>
        </cntorgp>
        <cntaddr>
          <addrtype>mailing and physical</addrtype>
          <address>2885 Mission Street</address>
          <city>Santa Cruz</city>
          <state>CA</state>
          <postal>95060</postal>
        </cntaddr>
        <cntvoice>831-427-4747</cntvoice>
        <cntemail>pcmsc_data@usgs.gov</cntemail>
      </cntinfo>
    </metc>
    <metstdn>Content Standard for Digital Geospatial Metadata</metstdn>
    <metstdv>FGDC-STD-001-1998</metstdv>
  </metainfo>
</metadata>
