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Title

A PERSPECTIVE ON THE CLIMATIC CONDITION OF IRAN DURING THE QUATERNARY ICE AGE

Pages

  211-228

Abstract

 Climatic condition of Iran during the ice age has been attractive for many geographers and geologists since the earlier years of the 20th century, and for geomorphologists at the end of the same century. The perspectives of these pioneers will be expressed, in this regard, in two general categories of “dry and cold weather” and “the weather colder than today with more showers.” Enormous amounts of geomorphologic evidence in the plateau of Iran indicate that it is not possible to generalize either of the two mentioned ideas to all parts of the plateau. From the other perspective, combination of these two theories, as some theorists have proposed, might not be comprehensive enough, but considering the varieties in the GEOMORPHOLOGY of the area, five climatic conditions can be indicated for this plateau: 1. Cold and icy climate, 2. Cold climate close to the icy one, 3. Cold and rainy climate, 4. Warm and humid climate or warm and rainy one, 5. Dry and semi dry climate. In determining this expanse, not only geomorphologic shapes, but also geographical conditions, topographical states, and the direction of hillsides have had significant roles.

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    APA: Copy

    ASGHARI MOGHADAM, M.R.. (2010). A PERSPECTIVE ON THE CLIMATIC CONDITION OF IRAN DURING THE QUATERNARY ICE AGE. GEOGRAPHY, 4(13), 211-228. SID. https://sid.ir/paper/208021/en

    Vancouver: Copy

    ASGHARI MOGHADAM M.R.. A PERSPECTIVE ON THE CLIMATIC CONDITION OF IRAN DURING THE QUATERNARY ICE AGE. GEOGRAPHY[Internet]. 2010;4(13):211-228. Available from: https://sid.ir/paper/208021/en

    IEEE: Copy

    M.R. ASGHARI MOGHADAM, “A PERSPECTIVE ON THE CLIMATIC CONDITION OF IRAN DURING THE QUATERNARY ICE AGE,” GEOGRAPHY, vol. 4, no. 13, pp. 211–228, 2010, [Online]. Available: https://sid.ir/paper/208021/en

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