| Titre | The Great Slave Lowland: the legacy of Glacial Lake McConnell |
| Auteur | Wolfe, S A; Morse, P D; Kokelj, S V; Gaanderse, A J |
| Source | Landscapes and landforms of western Canada; par Slaymaker, O (éd.); World Geomorphological Landscapes 2016 p. 87-96, https://doi.org/10.1007/978-3-319-44595-3 5 |
| Année | 2016 |
| Séries alt. | Secteur des sciences de la Terre, Contribution externe 20140375 |
| Éditeur | Springer International Publishing |
| Document | publication en série |
| Lang. | anglais |
| DOI | https://doi.org/10.1007/978-3-319-44595-3 5 |
| Media | papier; en ligne; numérique |
| Formats | pdf (Adobe® Reader®) |
| Province | Territoires du Nord-Ouest |
| SNRC | 85I/03; 85I/04; 85I/05; 85I/06; 85I/11; 85I/12; 85I/13; 85I/14; 85J; 85K/01; 85K/02; 85K/03; 85K/06; 85K/07; 85K/08; 85K/09; 85K/10; 85K/11; 85K/14; 85K/15; 85K/16; 85N/01; 85N/02; 85N/03; 85N/06; 85N/07;
85N/08; 85N/09; 85N/10; 85N/11; 85O/01; 85O/02; 85O/03; 85O/04; 85O/05; 85O/06; 85O/11; 85O/12; 85P/03; 85P/04 |
| Région | Grand lac des Esclaves; Yellowknife; Dettah; Behchoko; Edzo |
| Lat/Long OENS | -117.5000 -113.0000 63.7500 62.0000 |
| Sujets | antecedents glaciaires; glaciation; déglaciation; lacs glaciaires; niveaux d'eau; emersion; pergélisol; glace fossile; lentilles de glace; caractéristiques périglaciaires; végétation; dépôts organiques;
tourbières; sols; argiles; silts; climat; temperature; affaissement; glissements; analyses thermiques; regimes thermiques; Lac glaciaire de McConnell; Bouclier Canadien; Calotte glaciaire Laurentide; sédiments glaciolacustres; sédiments lacustres
prélittoraux; buttes cryogènes; forêt; limites de submersion, glaciolacustre; changement climatique; géologie des dépôts meubles/géomorphologie; géologie de l'environnement; Nature et environnement; Phanérozoïque; Cénozoïque; Quaternaire |
| Illustrations | cartes de localisation; cartes géolscientiques généralisées; photographies; profils; représentations schématiques |
| Programme | Géosciences de changements climatiques, Infrastructures terrestres |
| Diffusé | 2016 12 02 |
| Résumé | (disponible en anglais seulement)
The Great Slave Lowland of the Taiga Shield is an 11,000 km2 low-elevation granitic bedrock plain along the north shore of Great Slave Lake, Northwest
Territories. It is characterized by a mosaic of coniferous and deciduous forest cover, wetlands, sparsely vegetated bedrock outcrops, and peatlands. The region was glaciated until about 13,000 years ago and then inundated by Glacial Lake McConnell
and by ancestral Great Slave Lake, which gradually declined towards the present lake elevation. Consequently, fine-grained glacilacustrine and nearshore lacustrine sediments are broadly distributed across the region. Permafrost is widespread within
forest-covered sediments and peatlands, but is not sustained beneath bedrock outcrops, leading to an extensive, but discontinuous, permafrost distribution. Lithalsas, which are permafrost mounds up to 8 m in height and several hundred metres in
length, are also abundant. These form by ice segregation within mineral soil, as permafrost aggrades into the fine-grained sediments following lake level recession. Lithalsas are most common within the first few tens of metres above the present level
of Great Slave Lake, indicating that many are late Holocene in age and some <1000 years. These elevated surfaces favour the establishment of deciduous forests with thin organic ground cover and with mean annual ground temperatures typically between
-0.5 and -1.5 °C. With annual mean air temperatures consistently warming since the 1940s, this terrain is vulnerable to thawing and subsidence, with impacts on the ecology, hydrology, and population of the region. |
| GEOSCAN ID | 295681 |
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