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Mesoscale Positive Relief Landforms, Mars

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Encyclopedia of Planetary Landforms

Definition

“Mesoscale positive relief landform” is used here as an umbrella term for <1-km-diameter elevations in the northern hemisphere of Mars in majority, produced by a variety processes, without genetic implications (e.g., Burr et al. 2009a).

Description

Ten to one hundred-m-scale-diameter raised forms of circular, elongate, or irregular plan view shape, which may occur as single or composite structures, isolated or clustered or aligned.

Subtypes by Morphology

  1. (1)

    Elevated structures with raised center or flat top

    1. (1.1)

      Knobs: small, typically rounded, isolated structures, often with steep slopes (isolated peaks) (Fig. 8/1)

    2. (1.2)

      “Mounds” may refer to any typically round-shaped elevation or may be understood as dome-like elevations. Subdued mounds are characterized by low-angle slopes.

      1. (1.2.1)

        Cones (conical mounds) have a circular to subcircular base that tapers to a (in many cases theoretical) point at the top (the apex – the peak), typically with concave or straight slopes...

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  1. Planetary Science Research Group, Eötvös Loránd University, Institute of Geography and Earth Sciences, Budapest, Hungary

    Henrik Hargitai

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  1. Henrik Hargitai
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Hargitai, H. (2014). Mesoscale Positive Relief Landforms, Mars. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_585-1

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  • DOI: https://doi.org/10.1007/978-1-4614-9213-9_585-1

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