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Abstract— <p>Glacial paleo-landforms in the Northern Okhotsk region mainly occur in Alpine-type mountains at elevations above 1500 m asl and in rugged low mountains (700–1500 m asl). Paleo-glacial surveys in several areas of the region, including the Dukcha Mountains and the Khasyn Range in the Magadan area, Maymandzha and Tuman Ranges, the Kilgana Mountains, as well as the Taynynot Range in the Taygonos Peninsula, have revealed Middle Pleistocene, Late Pleistocene, and Holocene moraine systems.</p>

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Glacial Paleo-Landforms in the Northern Okhotsk Region

  • 期刊论文

  • 发表日期：

    2025年6月26日

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  • O. Yu. Glushkova,
  • V. N. Smirnov

摘要

Abstract—

Glacial paleo-landforms in the Northern Okhotsk region mainly occur in Alpine-type mountains at elevations above 1500 m asl and in rugged low mountains (700–1500 m asl). Paleo-glacial surveys in several areas of the region, including the Dukcha Mountains and the Khasyn Range in the Magadan area, Maymandzha and Tuman Ranges, the Kilgana Mountains, as well as the Taynynot Range in the Taygonos Peninsula, have revealed Middle Pleistocene, Late Pleistocene, and Holocene moraine systems.