Mesoscale Positive Relief Landforms, Mars

Living reference work entry
DOI: https://doi.org/10.1007/978-1-4614-9213-9_585-1

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...

Keywords

Impact Crater Cinder Cone Salt Diapir Tuff Ring Tuff Cone 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
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Copyright information

© Springer Science+Business Media New York 2014

Authors and Affiliations

  1. 1.Planetary Science Research GroupEötvös Loránd University, Institute of Geography and Earth SciencesBudapestHungary