|Titre||Lithalsa distribution, morphology and landscape associations in the Great Slave Lowlands, Northwest Territories|
|Auteur||Stevens, C W; Wolfe, S A|
|Source||40th Annual Yellowknife Geoscience Forum, abstracts of talks and posters; par Watson, D M (éd.); Northwest Territories Geoscience Office, Yellowknife Geoscience Forum Abstracts Volume 2012, 2012 p.
|Séries alt.||Secteur des sciences de la Terre, Contribution externe 20120249|
|Réunion||40th annual Yellowknife Geoscience Forum; Yellowknife; CA; Novembre 13-15, 2012|
|Document||publication en série|
|Province||Territoires du Nord-Ouest|
|Sujets||glace; glace fossile; pergélisol; elements glaciaires; types de paysage; géologie des dépôts meubles/géomorphologie|
|Programme||Infrastructures terrestres, Géosciences de changements climatiques|
|Liens||Online - En Ligne |
|Résumé||(disponible en anglais seulement)|
The distribution of ice-rich terrain is an important geotechnical consideration for the engineering of northern infrastructure. Within the Great Slave Lowlands,
Northwest Territories, fine-grained silts and clays deposited by Glacial Lake McConnell (ca. 13 to 9.5 cal ka BP) and ancestral Great Slave Lake (post 9.5 cal ka BP) are widely distributed across discontinuous permafrost terrain. Whereas these
sediments are known to contain excess ice attributable to permafrost aggredation and ice segregation, little is known about the distribution of ice-rich terrain in this region.
Mineral lithalsas are permafrost mounds, caused by the formation of
segregate ice when the permafrost aggrades into the ground, and are most commonly encountered within fine-grained (lacustrine, glaciolacustrine or marine) sediments in discontinuous permafrost terrain. Lithalsas, like ice-wedges and pingos, represent
a form of ice-rich permafrost terrain that can be readily identified on the basis of surface geomorphology. A total of 1,777 ice-rich mineral lithalsas have been mapped over 3,680 km2 using monochromatic stereo-pair aerial photographs, across the
Great Slave Lowlands and Uplands. Drill cores indicate lithalsas in this region consist of ice-rich silt and clay, with segregated ice lenses up to 10 cm thick. Three distinct morphologies are recognized including: i) circular, ii) linear and (iii)
crescentic shapes, exhibiting conical and ride-like forms up to 8 m in height and more than 100 m in width. A linear correlation between lithalsa height and width suggests that 1 cm of vertical growth is accompanied by about 15 cm of lateral growth
at the peripheral edge. Lithalsa distribution is skewed towards lower-elevation terrain, with 97.7% located within the Great Slave Lowlands, and most of these within 10-15 m above present-day (~156 m asl) lake level. This proximity to present-day
lake levels suggests that many lithalsas in the region are late Holocene in age. These features predominately occur adjacent to water bodies and follow the regional distribution of frost susceptible silt and clay, particularly within former streams,
embayments and fault-controlled valleys. Landscape associations suggest lithalsa formation is controlled by sedimentological, thermal and hydrological conditions.
The thermal and physical disturbance of lithalsa features in the Great Slave
Lowlands can result in substantial terrain subsidence. Analysis of historical aerial photographs has identified lake expansion caused by the recent degradation of lithalsa. In addition, road surface subsidence on the order of 85 cm in the last decade
along a section of Highway 3 at Boundary Creek can be attributed to degradation of permafrost within a mineral lithalsa following road construction.