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                              <gco:Date>1998-01-01</gco:Date>
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                        <gco:CharacterString>Digital files on CD-ROM are available for $10.00 (contact information below). No fees charged for downloaded files.</gco:CharacterString>
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                        <gco:CharacterString>Ordering Instructions: Order by phone (907-451-5020), e-mail (dggspubs@alaska.gov), or fax (907-451-5050). The DGGS web site (http://www.dggs.alaska.gov/) has a list of electronic data available and an order form that can be printed. Payment accepted: Cash, check, money order, VISA, or MasterCard.</gco:CharacterString>
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                        <gco:CharacterString>Digital downloads: less than 30 minutes for most files. Offline CD/DVD-ROMs: 1-2 weeks unless special arrangements are made and an express fee is paid.</gco:CharacterString>
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               <gmd:measureDescription>
                  <gco:CharacterString>A value of estimated position error in meters. Surficial and bedrock geologic map data have a horizontal positional accuracy dependent on: 1) the 1:50,000-scale (nominal) aerial photographs on which it is based, with an estimated potential error due to a pen line width of approximately 0.001 being equivalent to approximately 1.5 meters on the ground; 2) the accuracy of the human zoom transfer scope operator in tracing the line work from acetate overlays to topographic base maps, with an estimated error due to a pen line width of approximately 0.001 being equivalent to approximately 1.5 meters on the ground; 3) the accuracy of the zoom transfer process itself, error magnitude highly variable and unknown but potentially large; 4) the digitizing RMS error of 0.003 inches (input coverage units), which equates to approximately 5 meters on the ground for a 1:63,360-scale map; and 5) the accuracy of the human operator digitizing the geologic from the topographic base maps, with an estimated error due to a pen line width of approximately 0.001 being equivalent to approximately 1.5 meters on the ground. The bedrock and comprehensive field maps were digitized using a map tablet and cross-hair mouse. Map error is induced by: (1) transferring map data from base topography to a mylar compilation map, with an estimated potential error due to a pen line width of approximately 0.001 being equivalent to approximately 1.5 meters on the ground; (2) the digitizing RMS error [24 control points on a regular grid have an average RMS error of 10.8 meters on the ground; individual control point error ranges from 4.3 to 21.2 meters on the ground]; and (3) the accuracy of the human operator digitizing the geologic line work from the topographic base map, with an estimated error due to a pen line width of approximately 0.001 being equivalent to approximately 1.5 meters on the ground. Total potential horizontal error for bedrock and comprehensive geologic map features is estimated to be approximately 110 meters.</gco:CharacterString>
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               <gmd:result>
                  <gmd:DQ_QuantitativeResult>
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                        <gml:BaseUnit gml:id="d1e563">
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                     <gmd:value>
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         <gmd:report>
            <gmd:DQ_CompletenessOmission>
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            <gmd:DQ_ConceptualConsistency>
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                  <gco:CharacterString>Polygon topology present and clean on appropriate data. Other data are line, point, or annotation data and do not require topologic relationships.</gco:CharacterString>
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               <gmd:result gco:nilReason="unknown"/>
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                        <gco:CharacterString>Field work - Field work for bedrock investigations, including ridge traverses and examination of riverbank exposures, was conducted between June 16 and July 8, 1997. Field notes and rock samples were collected at approximately 700 stations throughout the Tanana A-1 and A-2 Quadrangles. Bedrock mappers recorded observations on 1:50,000- and 1:63,360-scale topographic base maps, compiled onto a 1:50,000-scale mylar map after the field season ended. Field stations were located using hand held GPS units. Field station notes and GPS location data were manually entered into a spreadsheet.</gco:CharacterString>
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                     <gmd:dateTime>
                        <gco:DateTime>1997-01-01T00:00:00</gco:DateTime>
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               <gmd:processStep>
                  <gmd:LI_ProcessStep>
                     <gmd:description>
                        <gco:CharacterString>Fieldwork - Fieldwork for surficial geologic investigations, including ridge and valley traverses, road cut investigations, and river exposures, was conducted for approximately 21 person-days in June and July 1997 by a surficial geologist. Field notes and sediment samples were collected throughout the area for surficial investigations. Surficial mapping involved using sources cited below on a regular basis for checking and correlating general units. The surficial mapper recorded observations on co-registered acetate overlays on 1:50,000-scale (nominal) color-infrared aerial photographs, and directly on 1:63,360-scale topographic base maps. Stations were located using air photos and topographic maps.</gco:CharacterString>
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                        <gco:DateTime>1997-01-01T00:00:00</gco:DateTime>
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                     <gmd:source xlink:href="#id_Newberry and Clautice"/>
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                     <gmd:source xlink:href="#id_1989"/>
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               <gmd:processStep>
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                        <gco:CharacterString>Photo interpretation - Before, during, and after field work, surficial-geologic information was interpreted using 1:50,000-scale (nominal) color-infrared air-photo stereopairs, and compiled onto acetate overlays. Photo interpretation was based on field notes from fieldwork process step (above), observed land forms and relationships in the photos, and all known geologic data from previous work in the area. The main sources of existing data include Eakin (1912; 1913), Hopkins and Tabor (1962), and Yeend (1989). The overlay information was transferred to a paper 1:63,360-scale USGS topographic base using a zoom transfer scope.</gco:CharacterString>
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               <gmd:processStep>
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                        <gco:CharacterString>Digital Cartography - Surficial-geologic information was digitized from the paper USGS topographic base map into Arc/Info 7.0.4 GIS (ArcEdit module) using a large-format digitizing table. Surficial-geologic polygons and lines were then edited and attributed using Arc, Info, and ArcEdit. Bedrock point data of locations of structural observations (strike, dip, cleavage, jointing, etc.) were intersected with the surficial-geologic polygon coverage using the Arc command "intersect" in order to identify locations that were mapped as surficial materials based on aerial photography but were found to have small exposures that were desirable to be mapped as bedrock. These areas were then modified in the surficial-geologic coverages to be areas of bedrock exposure. Final bedrock and surficial geology polygon coverages were merged using the Arc command "union" to generate the polygon coverage used to make the comprehensive geologic map. Other cartographic elements, primarily text and tables, were created in CorelDraw, converted to CGM format, and imported into ArcPlot for final layout. Data from the comprehensive geologic map of the area were used as the basis for generating the derivative engineering-geologic map. An ArcInfo lookup table was made to assign geologic units (item UNIT) from the comprehensive map to appropriate engineering-geologic units (item MAT) based on the Unified Soil Classification System as described by Wagner (1957). This lookup table was applied to the ArcInfo polygon coverage containing the geologic units and a new engineering-geologic polygon coverage was generated using the "dissolve" command based on the new materials-unit item "MAT." Additional features were mapped from ground observations and interpretation of air photos, and digitized and attributed using ArcInfo. ArcPlot was used to generate plot files of the resulting materials coverage using DGGS-standard symbology.</gco:CharacterString>
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                        <gco:DateTime>1997-01-01T00:00:00</gco:DateTime>
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                        <gco:CharacterString>Source Contribution: This map contains geologic unit descriptions and outcrop locations and was used to plan traverses and help define geologic units.Source Type: paper</gco:CharacterString>
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                              <gco:CharacterString>The Rampart and Hot Springs regions</gco:CharacterString>
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                                    <gco:Date>1912-01-01</gco:Date>
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                                    <gco:CharacterString>U.S. Geological Survey</gco:CharacterString>
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                              <gco:CharacterString>A geologic reconnaissance of a part of the Rampart Quadrangle, Alaska</gco:CharacterString>
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                                    <gco:CharacterString>Bulletin 535</gco:CharacterString>
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                              <gco:CharacterString>p. 38</gco:CharacterString>
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                  <gmd:LI_Source id="id_Hopkins_and_Taber,_1962">
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                        <gco:CharacterString>Source Contribution: This map contains geologic unit descriptions and outcrop locations and was used to plan traverses and help define geologic units.Source Type: paper</gco:CharacterString>
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                     <gmd:sourceCitation>
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                           <gmd:title>
                              <gco:CharacterString>Asymmetrical valleys in central Alaska (abs.)</gco:CharacterString>
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                              <gmd:CI_Date>
                                 <gmd:date>
                                    <gco:Date>1962-01-01</gco:Date>
                                 </gmd:date>
                                 <gmd:dateType>
                                    <gmd:CI_DateTypeCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_DateTypeCode"
                                                         codeListValue="publication">publication</gmd:CI_DateTypeCode>
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                              </gmd:CI_Date>
                           </gmd:date>
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                              <gmd:CI_ResponsibleParty>
                                 <gmd:organisationName>
                                    <gco:CharacterString>Geological Society of America</gco:CharacterString>
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                                 <gmd:contactInfo>
                                    <gmd:CI_Contact>
                                       <gmd:address>
                                          <gmd:CI_Address>
                                             <gmd:city>
                                                <gco:CharacterString>Boulder</gco:CharacterString>
                                             </gmd:city>
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                                                <gco:CharacterString> CO, USA</gco:CharacterString>
                                             </gmd:administrativeArea>
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                                    <gco:CharacterString>Hopkins, D.M.</gco:CharacterString>
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                                    <gco:CharacterString>Taber, B.</gco:CharacterString>
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                                    <gco:CharacterString>Special Paper</gco:CharacterString>
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                                    <gco:CharacterString>v. 68</gco:CharacterString>
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                              <gco:CharacterString>p. 116</gco:CharacterString>
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                        <gco:CharacterString>Source Contribution: This report contains information that was used to aid in the creation of and sample preparation for the surficial geologic map (PDF 98-37C).Source Type: paper</gco:CharacterString>
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                           <gmd:title>
                              <gco:CharacterString>Compositions of placer gold in the Rampart-Eureka-Manley-Tofty area, eastern Tanana and western Livengood quadrangles, central Interior Alaska, determined by electron microprobe analysis</gco:CharacterString>
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                                 <gmd:date>
                                    <gco:Date>1997-01-01</gco:Date>
                                 </gmd:date>
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                                    <gco:CharacterString>State of Alaska, Department of Natural Resources, Division of Geological &amp; Geophysical Surveys (DGGS)</gco:CharacterString>
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                              <gco:CharacterString>The use of the Unified Soil Classification System by the Bureau of Reclamation</gco:CharacterString>
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                                    <gco:Date>1957-01-01</gco:Date>
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