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Parent materials mode of meposition in the Northwest Territories and Nunavut

  • Bog

    Bog

    Peat deposit resulting from accumulation of vegetative (organic) materials. Mesic and fibric sedge and moss peat.

  • Colluvial

    Colluvial

    Regosolic Turbic Cryosol associated with colluviated valley.

  • Colluvial

    Colluvial

    Perennially frozen, loamy-textured, colluviated till. The material is underlain by thick ground ice.

  • Colluvial

    Colluvial

    Thin veneer of colluvium over limestone bedrock. The colluvium consists mainly of rock fragments, sand, silt and clay.

  • Lacustrine

    Lacustrine

    Lacustrine material deposited by glacial lake water. Mostly silt and clay.

  • Morainal

    Morainal

    A Orthic Turbic Cryosol associated with bedrock-controlled till landscape.

  • Morainal

    Morainal

    Morainal material deposited by ice. A mixture of boulders, stones, sand, silt and clay.

  • Morainal

    Morainal

    Perennially frozen, shallow morainal material (till) underlain by granitic bedrock. The loamy textured material is affected by downslope movement.

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