Glacial Records in the Medicine Bow Mountains and Sierra Madre of Southern Wyoming and Adjacent Colorado, with a Traveler's Guide to Their Sites PDF Download
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Author: Brainerd Mears
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 36
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Author: Brainerd Mears
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 36
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Author:
Publisher:
ISBN:
Category : Forests and forestry
Languages : en
Pages : 236
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Author:
Publisher:
ISBN:
Category : Rangelands
Languages : en
Pages : 444
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Author: Dennis H. Knight
Publisher: Yale University Press
ISBN: 0300185928
Category : Science
Languages : en
Pages : 417
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Book Description
Many changessome discouraging, others hopefulhave occurred in the Rocky Mountain region since the first edition of this widely acclaimed book was published. Wildlife habitat has become more fragmented, once-abundant sage grouse are now scarce, and forest fires occur more frequently. At the same time, wolves have been successfully reintroduced, and new approaches to conservation have been adopted. For this updated and expanded Second Edition, the authors provide a highly readable synthesis of research undertaken in the past two decades and address two important questions: How can ecosystems be used so that future generations benefit from them as we have? How can we anticipate and adapt to climate changes while conserving biological diversity?
Author: Ann L. Hild
Publisher:
ISBN:
Category : Germination
Languages : en
Pages : 240
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Author: Birgit Terhorst
Publisher: Newnes
ISBN: 0080932193
Category : Science
Languages : en
Pages : 315
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Slope deposits are common in any inclined relief. So-called cover beds may veil entire landscapes, in which case they are commonly overlooked or confused with soil horizons. This book focuses on these widespread deposits and discusses their properties, genesis, and age mainly in subdued mountains of Central Europe, where to date most research on the matter has been conducted. The ecological consequences of such slope deposits on soils, slope water dynamics, and slope failures are addressed. Finally, transfer of the cover-bed concept to other mid-latitude regions is attempted for the reconstruction of landscape evolution. This unique compilation, covering several decades of a facies-oriented approach to slope-deposit research, delivers deep insight into the wide field of research on cover beds and encourages researchers all over the world to take an in-depth look at the critical zone as to its possible stratified nature. - Unique compilation of several decades of slope-deposit research - Facies-oriented approach - Addresses ecological consequences on soils, slope water dynamics, and slope failures
Author: A. Kleber
Publisher: Elsevier Inc. Chapters
ISBN: 0128079428
Category : Science
Languages : en
Pages : 80
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Slope deposits, which veil entire slopes or large parts of them in a rather uniform manner (cover beds), are ubiquitous in the subdued mountains of Central Europe (e.g., ). Here, we show that successions of cover beds are not restricted to this area but occur in many other regions of rather different natural inventories, such as the European Alps, the Russian Plain, south-central Turkey, and the western USA (Great Basin and Rocky Mountains). Cover beds usually form sequences of two or more distinct layers, and their distribution depends on the geomorphic, climate-driven processes of their formation. As they influence pedogenesis, they contribute to the understanding of soil properties and soil distribution: horizon boundaries occur at depths where cover-bed properties change. The properties of the layers and of the soils developed in them are different per region: in humid areas layers free of admixed loess components, thus being solely influenced by weathered local materials, are frequent, whereas in dry regions such layers have not yet been reported. In several areas studied in this chapter, paleosols either occur within cover-bed successions or have been reallocated and incorporated into the cover beds. This provides handles to the ages of layers. The layer successions slowly change with elevation but show a drastic break at around the timberline where Holocene rather than Pleistocene periglacial slope processes gained supremacy.
Author: Geological Survey of Wyoming
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 48
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Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 374
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Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 230
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