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Information Journal Paper

Title

Cryopediments and Cryoplanations as the Heritages of Periglacial Periods (Case Study: Eastern Slopes of Shirkuh)

Pages

  3-4

Abstract

 Introduction: Cryopediment and Cryoplanation are created in arid and semi-arid regions. According to the studies performed around the world, they are usually formed in the preglacial climatic conditions. The Cryopediments are very gently concave erosional bench-like landforms that are usually cut into the base of valley sides or marginal slopes of highlands and mountains. The Cryopediments developed by cryogenic processes in cold climates of the periglacial climate-morphogenetic zone are mostly created with the presence of permafrost. Cryopediments are developing due to the activity of a range of cryogenic processes whereby frost action, nivation and other processes cause to retreat back scarps. Cryoplanation terraces are bedrock steps or terraces on ridge crests and hilltops. The tread or “ flat” area is 10 to several hundred meters wide and long and the slopes from 1 to 5 degrees parallel to the ridge crests...

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  • Cite

    APA: Copy

    SHARIFI PAICHOON, MOHAMAD. (2018). Cryopediments and Cryoplanations as the Heritages of Periglacial Periods (Case Study: Eastern Slopes of Shirkuh). PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, 50(2 ), 3-4. SID. https://sid.ir/paper/716966/en

    Vancouver: Copy

    SHARIFI PAICHOON MOHAMAD. Cryopediments and Cryoplanations as the Heritages of Periglacial Periods (Case Study: Eastern Slopes of Shirkuh). PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2018;50(2 ):3-4. Available from: https://sid.ir/paper/716966/en

    IEEE: Copy

    MOHAMAD SHARIFI PAICHOON, “Cryopediments and Cryoplanations as the Heritages of Periglacial Periods (Case Study: Eastern Slopes of Shirkuh),” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. 50, no. 2 , pp. 3–4, 2018, [Online]. Available: https://sid.ir/paper/716966/en

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