{
    "@context": "http://schema.org/",
    
      "@type": "Dataset",
    
    
    "@id": "https://antcat.antarcticanz.govt.nz/geonetwork/srv/api/records/79607650-9fba-4a7a-beb4-7d5ad3deab3e",
    "includedInDataCatalog":[{"@type":"DataCatalog","url":"https://antcat.antarcticanz.govt.nz/geonetwork/srv/search#","name":""}],
    
    "inLanguage":"eng",
    
    "name": "Exposure Ages of Glacial Erratics and Bedrock along Byrd Glacier to Determine Long-Term Thinning History, Antarctica, 2019",

    
    "alternateName": [
    ],
    "dateCreated": [
    
      "2024-02-22T17:17:01"],
    "dateModified": [
    ],
    "datePublished": [
    
      "2024-02-22T17:17:01"],
    "thumbnailUrl": [
    
      "https://antcat.antarcticanz.govt.nz:/geonetwork/srv/api/records/79607650-9fba-4a7a-beb4-7d5ad3deab3e/attachments/K861.png"],
    "description": "Cosmogenic surface exposure chronologies were used to quantitatively constrain past rates of ice thinning, and the absolute timing of ice discharge and thinning events.\n\nWe sampled glacial erratics and bedrock from Byrd Glacier (LW1 Nunatak, LW2 Nunatak, Lonewolf Nuntataks, Tiger Nunatak, Mt. Tadpole). Samples were analysed for their exposure history, and all sites contained glacial erratics. In particular, the Lonewolf Nunataks sites, which is located along the margin of the East Antarctic Ice Sheet revealed a plethora of glacial cobbles.\n\nFurther details can be found at: https:\/\/doi.org\/10.1002\/esp.5701\n\nGET DATA: https:\/\/version2.ice-d.org\/antarctica\/publication\/1139\/",

    
    
    


    
    "keywords":[
    "K861A","BYRD GLACIER","GLACIAL RETREAT","GLACIER ELEVATION\/ICE SHEET ELEVATION","ISOTOPES","ALUMINUM-26 ANALYSIS","NUNATAKS","GLACIATION","GLACIER STRIATIONS\/GROOVES","BERYLLIUM-10 ANALYSIS","ISOTOPE RATIOS","DIGITAL ELEVATION\/TERRAIN MODEL (DEM)","ROCHE MOUNTONNEES\/SHEEPBACK","PALEOCLIMATE RECONSTRUCTIONS","ISOTOPE MEASUREMENTS","GLACIAL DRIFT","SEDIMENTARY ROCK VERTICAL\/GEOGRAPHIC DISTRIBUTION","BEDROCK LITHOLOGY","ISOTOPIC AGE","FIELD SURVEYS","FIELD INVESTIGATION","GROUND-BASED OBSERVATIONS","COMPASSES","INCLINOMETERS","GNSS RECEIVER","ANTARCTICA","ASP"
    ]


    
    ,"creator": [

          {
          
          
          "@type":"Person"
          
            ,"name": "Stutz, J."
            ,"email":  ["jamey.stutz@vuw.ac.nz"]
          

          
          ,"contactPoint": {
          "@type" : "PostalAddress"
          
          }
          }

          ]
        ,"publisher": [

          {
          

          
          "@type":"Organization"
          
            ,"name": "Informal Cosmogenic-Nuclide Exposure-Age Database"
            ,"email":  [""]
          

          
          ,"contactPoint": {
          "@type" : "PostalAddress"
          
          }
          }


          ]

        

    
    
    ,"distribution": [
    
      {
      "@type":"DataDownload",
      "contentUrl": "https:\/\/version2.ice-d.org\/antarctica\/sites\/",
      "encodingFormat": "WWW:LINK-1.0-http--link",
      "name": "Distribution Metadata"
      
      }]
    
      ,"encodingFormat": [
      
      ]
    


    ,"spatialCoverage": [
    
      {"@type":"Place",
      "description": [
      
      ],
      "geo": [
      
        {"@type":"GeoShape",
        "box": "-81.406 152.096 -78.594 162.603"
        }
      ]
      }]

    ,"temporalCoverage": [
    
      "2019-12-23T00:00:00/2020-01-11T12:00:00"
      ]


    
      ,"license": [
          {
          "@type": "CreativeWork",
          "name": "This data set conforms to the CC BY Attribution License (https:\/\/creativecommons.org\/licenses\/by\/4.0\/)"
          }
        ]
    
    
    
    

    , "citation": "Stutz, J., Eaves, S.,  (
    2024
    ) Exposure Ages of Glacial Erratics and Bedrock along Byrd Glacier to Determine Long-Term Thinning History, Antarctica, 2019.
    Informal Cosmogenic-Nuclide Exposure-Age Database.
        ,
    Accessed: 2026-07-07+12:00"

    }