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D M Barnett

Biographic Data

ID2741210
NAMED M Barnett
GIVEN NAMESD M
FAMILY NAMEBarnett
SIGNATUREBARNETT D M
AFFILIATIONSMcGill University
ORCID0000-0001-6606-0581
VERIFIEDYes
TOTAL WORKS4
TOTAL CITATIONS4
WORKS AS AUTHOR4
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1964
LATEST PUBLICATION YEAR1978
H-INDEX1
  • Holocene Emergence of the South and East Coasts of Melville Island, Queen Elizabeth Islands, Northwest Territories, Canada

    Open Access•Patrick McLaren, D M Barnett•ARTICLE•ARCTIC•1978

    Twenty-five radiocarbon dates from the coast of Melville Island show that there has been up to 100 m of Holocene emergence. This evidence of post-glacial rebound suggests there was significant late-Wisconsin glacier cover on or near the island. The Winter Harbour moraine on the south coast is thought to mark the maximum northward advance of the Laurentide ice. However, emergence for this area appears to be essentially complete, whereas the northe…

  • Sensitivity of Surface Materials and Vegetation to Disturbance in the Queen Elizabeth Islands

    Open Access•D M Barnett, S A Edlund et al.•ARTICLE•ARCTIC•1975

    Concern about potential and actual disturbance of surface materials, vegetation and wildlife of the Queen Elizabeth Islands has risen sharply in the last few years. The purpose of this paper is to outline an approach to the problem, based on terrain studies, and to offer a commentary on the recent paper by T.A. Babb and L.C. Bliss in Arctic. ... For a rational assessment of the problem, information is required on: a) surface materials - ice conte…

  • Geographica

    Open Access•D M Barnett, J A Peterson•ARTICLE•Canadian Geographies /…•1968

  • The Significance of Glacial Lake Naskaupi 2 in the Deglaciation of Labrador‐ungava

    Open Access•D M Barnett, J A Peterson•ARTICLE•Canadian Geographies /…•1964•Cited by: 4•References: 8

    Ce mémoire apporte de nouvelles données concernant le lac glaciaire Naskaupi 2, données utilisées pour mieux comprendre le déroulement de la déglaciation dans la péninsule d'Ungava‐Labrador. Des isobases ont été tracées pour le plan d'eau du lac Naskaupi 2. Elles ont été calculées en résolvant des triangles par la géométric. On s'est servi seulement de triangles sans angle aigueë prononcée, dont la longueur minimum d'un côtéétait de 7.14 milles, …

  • The Significance of Glacial Lake Naskaupi 2 in the Deglaciation of Labrador‐ungava

    Open Access•D M Barnett, J A Peterson•ARTICLE•Canadian Geographies /…•1964•Cited by: 4•References: 8

    Ce mémoire apporte de nouvelles données concernant le lac glaciaire Naskaupi 2, données utilisées pour mieux comprendre le déroulement de la déglaciation dans la péninsule d'Ungava‐Labrador. Des isobases ont été tracées pour le plan d'eau du lac Naskaupi 2. Elles ont été calculées en résolvant des triangles par la géométric. On s'est servi seulement de triangles sans angle aigueë prononcée, dont la longueur minimum d'un côtéétait de 7.14 milles, …

  • The Significance of Glacial Lake Naskaupi 2 in the Deglaciation of Labrador‐ungava

    Open Access•D M Barnett, J A Peterson•ARTICLE•Canadian Geographies /…•1964•Cited by: 4•References: 8

    Ce mémoire apporte de nouvelles données concernant le lac glaciaire Naskaupi 2, données utilisées pour mieux comprendre le déroulement de la déglaciation dans la péninsule d'Ungava‐Labrador. Des isobases ont été tracées pour le plan d'eau du lac Naskaupi 2. Elles ont été calculées en résolvant des triangles par la géométric. On s'est servi seulement de triangles sans angle aigueë prononcée, dont la longueur minimum d'un côtéétait de 7.14 milles, …

  • Geographica

    Open Access•D M Barnett, J A Peterson•ARTICLE•Canadian Geographies /…•1968

  • Sensitivity of Surface Materials and Vegetation to Disturbance in the Queen Elizabeth Islands

    Open Access•D M Barnett, S A Edlund et al.•ARTICLE•ARCTIC•1975

    Concern about potential and actual disturbance of surface materials, vegetation and wildlife of the Queen Elizabeth Islands has risen sharply in the last few years. The purpose of this paper is to outline an approach to the problem, based on terrain studies, and to offer a commentary on the recent paper by T.A. Babb and L.C. Bliss in Arctic. ... For a rational assessment of the problem, information is required on: a) surface materials - ice conte…

  • Holocene Emergence of the South and East Coasts of Melville Island, Queen Elizabeth Islands, Northwest Territories, Canada

    Open Access•Patrick McLaren, D M Barnett•ARTICLE•ARCTIC•1978

    Twenty-five radiocarbon dates from the coast of Melville Island show that there has been up to 100 m of Holocene emergence. This evidence of post-glacial rebound suggests there was significant late-Wisconsin glacier cover on or near the island. The Winter Harbour moraine on the south coast is thought to mark the maximum northward advance of the Laurentide ice. However, emergence for this area appears to be essentially complete, whereas the northe…

Climate change and permafrost (3 works) · Geography (3 works) · Geology (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Cartography (2 works) · Cryospheric studies and observations (2 works) · Humanities (2 works) · Landform (2 works) · Oceanography (2 works)

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