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Information Journal Paper

Title

Sea-level Changes during 2600 BP and Little Ice Age and its Impacts on Iranian Coast

Pages

  15-17

Abstract

 Introduction: The Caspian Sea (CS) can be subdivided into three parts: North, Middle and south parts. The sea experienced many cycles of Sea-level changes with vast emerged and submerged areas. In the terraces in Dagestan, two major phases have been distinguished. The Early Khvalyn Transgression is represented by five successive marine terraces between +50 and 0 m atabsolute height. Furthermore, at the boundary of Late Pleistocene and Holocene a-50 and by other researcher a-113 sea level record has been identified. This is why many researchers call it as a capricious level due to great sea level changes. Recent sea-level changes also got attention, experienced around 3 m sea-level changes between 1929 and 1977 and rose back in 1995. Five late Holocene records have been identified at least up to-22 absolute elevation. Present work aims at showing two phases of Transgression and its impact on Iranian coast by Arial photograph and radiocarbon dating, a 2600 BP and Littlie Ice age....

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    • Cite

    APA: Copy

    Abdollahi Kakroodi, ata. (2017). Sea-level Changes during 2600 BP and Little Ice Age and its Impacts on Iranian Coast. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, 49(1 ), 15-17. SID. https://sid.ir/paper/717667/en

    Vancouver: Copy

    Abdollahi Kakroodi ata. Sea-level Changes during 2600 BP and Little Ice Age and its Impacts on Iranian Coast. PHYSICAL GEOGRAPHY RESEARCH QUARTERLY[Internet]. 2017;49(1 ):15-17. Available from: https://sid.ir/paper/717667/en

    IEEE: Copy

    ata Abdollahi Kakroodi, “Sea-level Changes during 2600 BP and Little Ice Age and its Impacts on Iranian Coast,” PHYSICAL GEOGRAPHY RESEARCH QUARTERLY, vol. 49, no. 1 , pp. 15–17, 2017, [Online]. Available: https://sid.ir/paper/717667/en

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