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4 edition of Geomorphology and changing environments in Central Europe found in the catalog.

Geomorphology and changing environments in Central Europe

European Regional Geomorphological Conference (1996 Hungary)

Geomorphology and changing environments in Central Europe

International Association of Geomorphologists, European Regional Geomorphological Conference, Hungary, April, 1996

by European Regional Geomorphological Conference (1996 Hungary)

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  • 36 Currently reading

Published by Gebrüder Borntraeger in Berlin .
Written in English

    Subjects:
  • Geomorphology -- Carpathian Mountains Region -- Congresses,
  • Geomorphology -- Europe, Central -- Congresses,
  • Geomorphology -- Hungary -- Congresses,
  • Mountains -- Europe, Central -- Congresses

  • Edition Notes

    Includes bibliographical references.

    Statementedited by Hanna Bremer and Dénes Lóczy.
    SeriesZeitschrift für Geomorphologie, Supplementband -- n.F. 110, Zeitschrift für Geomorphologie -- n.F. 110.
    ContributionsBremer, Hanna., Lóczy, Dénes., International Association of Geomorphologists.
    The Physical Object
    Paginationvi, 261 p. :
    Number of Pages261
    ID Numbers
    Open LibraryOL15443641M
    ISBN 103443211100
    OCLC/WorldCa37900471

    This book is destined to become the classic volume on arid and semi-arid geomorphology for advanced students and researchers in physical geography, geomorphology, Earth science, sedimentology, environmental science, and archaeology. The book will be a reference for a variety of professionals and students, both graduate and undergraduate, with interests in Physical Geography, Geomorphology, Ecology, and Environmental Science. Because of the importance of the alpine treeline ecotone for recreation and aesthetic interests in mountain environments, wildland and park managers.

    Professor Bernard John Smith (21 March – 31 October ) was an English geomorphologist and physical geographer. [1] [2] He was born in the English village of Beer in Dorset where he attended the local school until the family's relocation to mater: University of Reading.   Post by Dr. James Lea. I’m James Lea, and I’ve just started in the department as a new lecturer in glacial geomorphology. My research looks at how glacial and geomorphic processes can aid our understanding of the past, present, and potential future behaviour of glaciers and ice sheets, though I also have more general interests in Quaternary environments, remote sensing, and numerical.

    Buy Changing Climates, Ecosystems and Environments Within Arid Southern Africa and Adjoining Regions (): NHBS - Jürgen Runge, Routledge. Across Europe, that enlargement--not as a one-time event but as an ongoing process--is proclaimed to stabilize East-Central Europe and to create a Europe that is finally "whole and free". Europe's eastern enlargement is a profoundly geographic and geopolitical project, as it is based on territorial conceptions about the essence of places, the.


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Geomorphology and changing environments in Central Europe by European Regional Geomorphological Conference (1996 Hungary) Download PDF EPUB FB2

Get this from a library. Geomorphology and changing environments in Central Europe: International Association of Geomorphologists, European Regional Geomorphology and changing environments in Central Europe book Conference, Hungary, April, [Hanna Bremer; Dénes Lóczy; International Association of Geomorphologists.;].

Get this from a library. Geomorphology and changing environments in Central Europe: with 22 tables. [Hanna Bremer; International Association of Geomorphologists.; European Regional Geomorphological Conference (, Veszprém);].

A List of IAG/AIG and IAG/AIG-related Publications Conference Research Monographs Conference Abstract Volumes Conference Research Papers IAG/AIG Publication Series IAG/AIG Special Series Newsletter Field Guides Miscellaneous Conference Related Publications IAG/AIG Report Series 1.

Conference Research Monographs Gardiner, V., Ed. () International Geomorphology. Geomorphology (from Ancient Greek: γῆ, gê, "earth"; μορφή, morphḗ, "form"; and λόγος, lógos, "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near the Earth's surface.

Geomorphologists seek to understand why landscapes look the way they do, to understand. Geomorphology of Desert Environments. Desert plains and aeolian dunes in the central basin are the related products of contemporary climate.

Arid geomorphology: Changing perspectives on. Yet, LULC changes are considered as one of the most rapid drivers of global change (Slaymaker, ), especially in mountainous environments of Western Europe where slopes experienced a decrease. Abstract. Natural hazards research was initiated in the 's by Gilbert White and his students who promulgated a research paradigm that involved assessing risk from a natural event, identifying adjustments to cope with the hazard, determining people's perception of the event, defining the process by which people choose adjustments, and estimating the effects of public policy on the choice.

The changing focus and approach of geomorphic research suggests that the time is opportune for a summary of the state of discipline. The number of peer-reviewed papers published in geomorphic journals has grown steadily for more than two decades and, more importantly, the diversity of authors with respect to geographic location and disciplinary background (geography, geology, ecology, civil.

The book seeks to provide a comprehensive account of present aeolian processes, landforms and sediments, together with an analysis of past aeolian environments. Further, it looks at some of the anthropogenic pressures on aeolian processes, both on coasts and in deserts, and discusses some management solutions.

The book is richly illustrated in the form of both black-and-white and colour photos (but the colour photos duplicate the black-and-white ones!), graphs and diagrams." (Geologos, July ) Examines the physical systems occurring in desert environments, including climate, hydrology, past and present lakes, weathering, hillslopes, geomorphic Author: Julie J Laity.

Cambridge Core - Geomorphology and Physical Geography - Geomorphology in the Anthropocene - by Andrew S. GoudieCited by: The landmass now covered by the North Sea, here referred to as Doggerland, has had an important but neglected influence on the course of prehistory in northwestern Europe.

The physical character of Doggerland in the Late Glacial and earlier Holocene is assessed, together with its re-colonization by humans after the Last Glacial Maximum.

Important research about the drylands of the greater Central Asia region by several professors in the Michigan State University Department of Geography, Environment, and Spatial Sciences has recently been featured in a book published by Springer volume is edited by the department’s own Drs.

Jiquan Chen and Geoffrey Henebry, in conjunction with Garik Gutman, Program Manager for the. and biologically dynamic and newly colonized region of Europe. The first four chapters (by H. Usinger, P. de Klerk, N. Benecke, and K. Kaiser) cover aspects of the changes in vegetation, geomorphology, and fauna, with particularly detailed information on palynology and the development of the lake-riddled environments of northeastern Germany.

The number of peer-reviewed papers published in geomorphic journals has grown steadily for more than two decades and, more importantly, the diversity of authors with respect to geographic location and disciplinary background (geography, geology, ecology, civil engineering, computer science, geographic information science, and others) has expanded dramatically.

This new Encyclopedia of Coastal Science stands as the latest authoritative source in the field of coastal studies, making it the standard reference work for specialists and the interested lay person.

Unique in its interdisciplinary approach. This Encyclopedia features contributions by well-known international specialists in their respective fields and is abundantly illustrated with line 4/5(3).

Periglacial geomorphology applies the established rules gained by studies in recent periglacial environments to former ones of the Pleistocene past; it tries to use its models to predict future changes and developments of recent periglacial environments.

Periglacial geomorphology, thus, comprises a much wider field than in Thorn's by: Central among their results stands the observation that most geomorphic surfaces and elements in the aggradational sectors of present day continental basins belong to distributive (e.g. responses to variable sediment supply and axial incision and changing distal environments due to basin hydrology).

Geomorphology of Desert Environments. central Europe and China, in particular. Although the book identifies the Clarens area of the northeastern Free State as one of the world’s 61 major sandstone landscapes, relatively little is known about the diversity of sandstone phenomena and their process origins in southern Africa.

Professor Tony Parsons: books Research monographs. Parsons, A.J. Hillslope Form, Routledge, 0 7. The study of hillslopes is a central element of geomorphology and many of the major methodological disputes in the subject have been focused around hillslopes.

In geography, a plain is a flat, sweeping landmass that generally does not change much in occur as lowlands along valleys or on the doorsteps of mountains, as coastal plains, and as plateaus or uplands.

In a valley, a plain is enclosed on two sides, but in other cases a plain may be delineated by a complete or partial ring of hills, by mountains, or by cliffs.Geomorphology of Desert Environments, Chapman & Hall, London, U. K., p. Figure World map of pediments as described in the literature from over references as of The book Fluvial Processes in Geomorphology, first published inis a reference.

The flow that shapes the minor bed or morphogenic flow has since been considered as the full-body flow, i.e. the flow that just overflows over the banks and has a return period of 1 to 2 years.