(Table 4) Erosion since slump initiation of retrogressive thaw slumps on Herschel Island and King Point

DOI

Estimated based on the slope angle of stabilised slump floors and the estimated position of the bottom of the massive ice layer.

Identifier
DOI https://doi.org/10.1594/PANGAEA.810042
Related Identifier https://doi.org/10.1594/PANGAEA.810045
Related Identifier https://doi.org/10.1002/ppp.1731
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.810042
Provenance
Creator Lantuit, Hugues ORCID logo; Pollard, Wayne H; Couture, Nicole ORCID logo; Fritz, Michael ORCID logo; Schirrmeister, Lutz ORCID logo; Meyer, Hanno ORCID logo; Hubberten, Hans-Wolfgang ORCID logo
Publisher PANGAEA
Publication Year 2012
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 28 data points
Discipline Earth System Research
Spatial Coverage (-139.014W, 69.082S, -137.902E, 69.576N); King Point, Yukon Territory