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Solifluction Landforms

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Encyclopedia of Planetary Landforms

Definition

Landforms resulting from the slow downslope flow of saturated unfrozen earth materials (van Everdingen et al. 1998/2005). The term is commonly applied to processes operating in both seasonal frost and permafrost areas.

Synonyms

Mud-debris tongue (not recommended)

Description of Subtypes

Subtypes as defined on Earth:

  1. (1)

    Solifluction lobe: an isolated, tongue-shaped feature on Earth up to 25 m wide and >150 m long. It commonly has a steep (15–60°) front (riser) and a relatively smooth upper surface (thread) (van Everdingen et al. 1998/2005) (Fig. 2).

    1. (1.1)

      Turf-banked lobes are vegetated lobes. They are non-sorted, displaying arcuate bands of tongue-like shaped fronts (Benedict 1970).

    2. (1.2)

      Stone-banked lobes are sorted solifluction lobes (Benedict 1970) (sorted patterned ground: sorted step). Stone-banked lobes are “lobate mass of rocky debris underlain by relatively stone-free fine-textured, moving soil” (Ridefelt 2004).

  2. (2)

    Solifluction terrace: a low step, or bench, with...

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References

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Correspondence to Henrik Hargitai .

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Hargitai, H., Johnsson, A. (2014). Solifluction Landforms. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_534-1

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  • DOI: https://doi.org/10.1007/978-1-4614-9213-9_534-1

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  • Online ISBN: 978-1-4614-9213-9

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