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Titlebook: Environmental Change in Iceland: Past and Present; Judith K. Maizels,Chris Caseldine Book 1991 Springer Science+Business Media Dordrecht 1

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發(fā)表于 2025-3-21 16:52:14 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Environmental Change in Iceland: Past and Present
編輯Judith K. Maizels,Chris Caseldine
視頻videohttp://file.papertrans.cn/313/312557/312557.mp4
叢書名稱Glaciology and Quaternary Geology
圖書封面Titlebook: Environmental Change in Iceland: Past and Present;  Judith K. Maizels,Chris Caseldine Book 1991 Springer Science+Business Media Dordrecht 1
描述3 new biota and extinction of others, and extensive soil erosion reaching almost catastrophic proportions have led to desertification of many upland areas and abandonment by local populations. The role of climatic change as opposed to deforestation and sheep grazing in creating these new environments has proved a further issue of great controversy. While our understanding of historic environmental changes remains inadequate, our knowledge of processes that are modifying the present-day landscape is also sparse and selective. Little is known of active periglacial processes, slope instabilities, and rates of soil erosion by slope wash and aeolian transport. Coastal processes of erosion and beach formation have been studied only locally. Most of our information on recent or active processes comprises records of glacier fluctuations, volcanic eruptions and jOkulhlaup events, but sti11little is known of the mechanisms and processes of landscape change effected by these events. This volume of papers, based on a conference sponsored by the Quaternary Research Association and the Geologists Association and held at the University of Aberdeen in April 1989, addresses many of these crucial un
出版日期Book 1991
關(guān)鍵詞environment; hydrogeology; ecotoxicology
版次1
doihttps://doi.org/10.1007/978-94-011-3150-6
isbn_softcover978-94-010-5389-1
isbn_ebook978-94-011-3150-6Series ISSN 0924-5006
issn_series 0924-5006
copyrightSpringer Science+Business Media Dordrecht 1991
The information of publication is updating

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Implantation: Lessons from a Primate Model dramatic example of this relationship was felt at the close of the last glaciation, when the marine polar front migrated thousands of kilometres between 13,000 and 11,000 BP, and again between 11,000 and 10,000 BP, associated with the complex climatic perturbations occurring during the final decay
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Introduction to Non-parametric Theories,the Eemian Interglacial, the Fossvogur layers, now seems to be of Late Weichselian age. Consequently the till in the upper part of the Fossvogur sediments must be considered to be of Younger Dryas or Preboreal age. This till is connected to a series of end moraines, one of which is the so-called ?lf
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Environmental Change in Iceland: Past and Present. An introduction dramatic example of this relationship was felt at the close of the last glaciation, when the marine polar front migrated thousands of kilometres between 13,000 and 11,000 BP, and again between 11,000 and 10,000 BP, associated with the complex climatic perturbations occurring during the final decay
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A Revised Model of Weichselian Deglaciation in South and South West Icelandthe Eemian Interglacial, the Fossvogur layers, now seems to be of Late Weichselian age. Consequently the till in the upper part of the Fossvogur sediments must be considered to be of Younger Dryas or Preboreal age. This till is connected to a series of end moraines, one of which is the so-called ?lf
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https://doi.org/10.1007/978-94-011-3150-6environment; hydrogeology; ecotoxicology
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978-94-010-5389-1Springer Science+Business Media Dordrecht 1991
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