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Titlebook: Rocks and Landforms; A. J. Gerrard Book 1988 J. Gerrard 1988 Denudation.Geomorphology.erosion.evolution.igneous rock

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发表于 2025-3-21 19:23:44 | 显示全部楼层 |阅读模式
书目名称Rocks and Landforms
编辑A. J. Gerrard
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图书封面Titlebook: Rocks and Landforms;  A. J. Gerrard Book 1988 J. Gerrard 1988 Denudation.Geomorphology.erosion.evolution.igneous rock
描述Geomorphology can be defined simply as the study of landforms. Landforms are the result of the interaction between what Ritter (1978) has called the driving and resisting forces. The driving forces or processes are the methods by which energy is exerted on earth materials and include both surface, geomorphological or exogenous processes and subsurface, geological or endogenous processes. The resisting forces are the surface materials with their inherent resistances determined by a complex combination of rock properties. Stated in these simple terms it would be expected that both sides of the equation be given equal weight in syntheses of landform evolution. However, this has not been the case. Until about the 1950s, geomorphology was mainly descriptive and concerned with producing time-dependent models of landscape evolution. Although the form of the land was the main focus, there was little detailed mention of process and scant attention to the properties of surface materials. There were, of course, exceptions. In the late 19th century G.K. Gilbert was stressing the equilibrium between landforms and processes. Many hydrologists were examining the detailed workings of river ‘system
出版日期Book 1988
关键词Denudation; Geomorphology; erosion; evolution; igneous rock
版次1
doihttps://doi.org/10.1007/978-94-011-5983-8
isbn_softcover978-94-011-5985-2
isbn_ebook978-94-011-5983-8
copyrightJ. Gerrard 1988
The information of publication is updating

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Resistance to weathering,ular and submolecular scales. The primary weathering mechanisms are triggered by activating processes, promoted by a variety of activating agencies (Table 5.1). The weathering response is the progression of mineralogical, petrological and mechanical properties as they change through time. These chan
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Instability in jointed and fissured rock,. Bisdom (1967) makes the important distinction between structural microcracks, which are present in unweathered rocks and are straight with angular intersections, and weathering microcracks, which are sinuous and exhibit dendritic patterns. As weathering progresses, grain boundaries become stained
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ere was little detailed mention of process and scant attention to the properties of surface materials. There were, of course, exceptions. In the late 19th century G.K. Gilbert was stressing the equilibrium between landforms and processes. Many hydrologists were examining the detailed workings of river ‘system978-94-011-5985-2978-94-011-5983-8
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A. J. Gerrarde solche aktivierte Adsorption können nur Moleküle erfahren, die in großem Abstand von der Adsorbens-Oberfläche eine kinetische Energie in Richtung senkrecht zur Oberfläche .. > .. besitzen. Zur Desorption der Adteilchen ist eine Desorptionsenergie .. aufzuwenden, die gleich der Adsorptionsenergie .
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