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The local topography consists of rugged and undulating terrain with mountains (to a maximum height of 525 m a.s.l.), hills, valleys, and creeks. The surficial deposit ranges from 2.4 to 4 m thick and is mostly composed of till (sandy clay loam) and shattered rock filled with ice. The permafrost is >600 m thick. The underlying bedrock is highly calcareous, composed of argillite with greywacke in some places. The uplands are mostly mesic, xeric, or barren, and consist mainly of boulder, frost-shattered rock, gravel, and polygonal nets of till, with low vegetation cover growing inside soil interstices. In the lowlands, where some soil moisture accumulates, a more continuous vegetation cover develops, consisting primarily of grasses and sedges.
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