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The geomorphic work of George Leslie Adkin (1888–1964) and glaciation in the Tararua Range, North Island, New Zealand

机译:乔治·莱斯利·阿德金(George Leslie Adkin)的地貌工程(1888年至1964年)和新西兰北岛塔拉鲁瓦山脉的冰川

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摘要

Research initiated in 1909 by G. Leslie Adkin (1888–1964) suggested Park Valley in the Tararua Range was glaciated during the Late Quaternary, based on the 'U-shaped' cross-profiles in the uppermost parts of several valleys. Findings were published, but were not met with universal acceptance. Adkin's work remained the only glacial research undertaken on the North Island's axial ranges until the latter part of the 20th century. Adkin holds a special position in New Zealand, because although he worked full-time as a farmer he published nearly 40 articles in scientific journals on topics as varied as Māori archaeology and geomorphology.
机译:G. Leslie Adkin(1888–1964)于1909年发起的研究表明,塔拉鲁阿山脉的公园山谷是第四纪晚期的冰川,其基础是几个山谷最上部的“ U形”剖面。研究结果已经发表,但并未得到普遍认可。直到20世纪后期,阿德金(Adkin)的工作仍然是北岛轴向范围内进行的唯一冰川研究。阿德金(Adkin)在新西兰担任特殊职务,因为尽管他全职从事农场工作,但他在科学期刊上发表了近40篇文章,主题涉及诸如毛利人考古学和地貌学。

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