{"data":{"id":"10.6084/m9.figshare.3475409","type":"dois","attributes":{"doi":"10.6084/m9.figshare.3475409","prefix":"10.6084","suffix":"m9.figshare.3475409","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Ewertowski, Marek W.","nameType":"Personal","givenName":"Marek W.","familyName":"Ewertowski","affiliation":[],"nameIdentifiers":[]},{"name":"Evans, David J. A.","nameType":"Personal","givenName":"David J. A.","familyName":"Evans","affiliation":[],"nameIdentifiers":[]},{"name":"Roberts, David H.","nameType":"Personal","givenName":"David H.","familyName":"Roberts","affiliation":[],"nameIdentifiers":[]},{"name":"Tomczyk, Aleksandra M.","nameType":"Personal","givenName":"Aleksandra M.","familyName":"Tomczyk","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Glacial geomorphology of the terrestrial margins of the tidewater glacier, Nordenskiöldbreen, Svalbard"}],"publisher":"Taylor \u0026 Francis","container":{},"publicationYear":2016,"subjects":[{"subject":"Space Science"},{"subject":"Medicine"},{"subject":"Physiology"},{"subject":"FOS: Biological sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Biological sciences","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"59999 Environmental Sciences not elsewhere classified","subjectScheme":"FOR"},{"subject":"FOS: Earth and related environmental sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Earth and related environmental sciences","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Ecology"},{"subject":"20199 Astronomical and Space Sciences not elsewhere classified","subjectScheme":"FOR"},{"subject":"FOS: Physical sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Physical sciences","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Sociology"},{"subject":"FOS: Sociology","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"FOS: Sociology","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"69999 Biological Sciences not elsewhere classified","subjectScheme":"FOR"}],"contributors":[],"dates":[{"date":"2016-07-09","dateType":"Created"},{"date":"2018-07-12","dateType":"Updated"},{"date":"2016","dateType":"Issued"}],"language":null,"types":{"ris":"DATA","bibtex":"misc","citeproc":"dataset","schemaOrg":"Dataset","resourceType":"Dataset","resourceTypeGeneral":"Dataset"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.1080/17445647.2016.1192329","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["68309073 Bytes"],"formats":[],"version":null,"rightsList":[{"rights":"Creative Commons Attribution 4.0 International","rightsUri":"https://creativecommons.org/licenses/by/4.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-4.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"description":"A 1:4000 scale map of the terrestrial margins of the foreland of Nordenskiöldbreen depicts a polythermal glacial landsystem containing a record of the landform signatures of individual ice flow units that operate within the glacier snout. A 1:700 map provides a detailed overview of fluted terrain, based on unmanned aerial vehicle images captured in 2014. The pattern of landforms lying inside the Little Ice Age (LIA) latero-frontal moraine on the northern side of the fjord comprises a fluted till surface, which in turn grades into ice-moulded bedrock. This signature records the recession of a single, wide ice flow unit, which was characterised by limited incorporation of subglacial material and restricted delivery of supraglacial debris. Inside the latero-frontal moraine on the south side of the fjord, a fluted surface is subordinate to a pronounced and large ice-cored moraine complex related to the confluence of five narrower ice flow units, each of which transported significant quantities of englacial and supraglacial debris at their suture zones as a series of longitudinal debris stripes. The suite of foreland landforms is diagnostic of both temperate subglacial and frozen-snout conditions, indicating the operation of a warm polythermal glacier fed by multiple flow units during the LIA.","descriptionType":"Abstract"}],"geoLocations":[],"fundingReferences":[],"xml":"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","url":"https://tandf.figshare.com/articles/dataset/Glacial_geomorphology_of_the_terrestrial_margins_of_the_tidewater_glacier_Nordenski_ldbreen_Svalbard/3475409","contentUrl":null,"metadataVersion":3,"schemaVersion":"http://datacite.org/schema/kernel-4","source":"mds","isActive":true,"state":"findable","reason":null,"viewCount":0,"viewsOverTime":[],"downloadCount":0,"downloadsOverTime":[],"referenceCount":1,"citationCount":0,"citationsOverTime":[],"partCount":0,"partOfCount":0,"versionCount":0,"versionOfCount":0,"created":"2016-07-09T09:13:15.000Z","registered":"2016-07-09T09:13:16.000Z","published":"2016","updated":"2020-09-04T06:32:11.000Z"},"relationships":{"client":{"data":{"id":"figshare.ars","type":"clients"}},"provider":{"data":{"id":"otjm","type":"providers"}},"media":{"data":{"id":"10.6084/m9.figshare.3475409","type":"media"}},"references":{"data":[{"id":"10.1080/17445647.2016.1192329","type":"dois"}]},"citations":{"data":[]},"parts":{"data":[]},"partOf":{"data":[]},"versions":{"data":[]},"versionOf":{"data":[]}}}}