The following sections of this BookRags Literature Study Guide is offprint from Gale's For Students Series: Presenting Analysis, Context, and Criticism on Commonly Studied Works: Introduction, Author Biography, Plot Summary, Characters, Themes, Style, Historical Context, Critical Overview, Criticism and Critical Essays, Media Adaptations, Topics for Further Study, Compare & Contrast, What Do I Read Next?, For Further Study, and Sources.
(c)1998-2002; (c)2002 by Gale. Gale is an imprint of The Gale Group, Inc., a division of Thomson Learning, Inc. Gale and Design and Thomson Learning are trademarks used herein under license.
The following sections, if they exist, are offprint from Beacham's Encyclopedia of Popular Fiction: "Social Concerns", "Thematic Overview", "Techniques", "Literary Precedents", "Key Questions", "Related Titles", "Adaptations", "Related Web Sites". (c)1994-2005, by Walton Beacham.
The following sections, if they exist, are offprint from Beacham's Guide to Literature for Young Adults: "About the Author", "Overview", "Setting", "Literary Qualities", "Social Sensitivity", "Topics for Discussion", "Ideas for Reports and Papers". (c)1994-2005, by Walton Beacham.
All other sections in this Literature Study Guide are owned and copyrighted by BookRags, Inc.
Erosion is the reduction or breakdown of landforms exposed to the forces of weathering (disintegration and decomposition). Weathering and subsequent erosion may be caused by both chemical or mechanical forces. Mechanical weathering agents include wind, water, and ice. Chemical weathering leading to erosion results from bio-organic breakdown, hydration, hydrolysis, and oxidation processes. The process of transportation describes the movements of eroded materials.
Erosion requires a transport mechanism (e.g., gravity, wind, water, or ice). Wind, water, and ice are also agents of erosion that cause the physical breakdown of rock and landforms.
A special form of erosion, mass wasting, describes the transport of material downslope under the influence of gravity. Landslides are a common example of mass wasting.
Erosion processes can also cause indirect landform alteration by breaking down overburden of rock and precipitating a pressure release that can crack and shift rock layers. The cracking process results in peels, exfoliation, or spalling. For example, the erosion of overburden can expose batholiths and these exposed formations can form exfoliation domes.
Organic materials can frequently contribute to erosion by pressure that results in structural cracking or in the formation of acidic compounds that weather rock.
Rapid temperature changes or large diurnal temperature changes (the difference between the highest daytime temperature and the coolest nighttime temperature) can accelerate erosional exfoliation, jointing, and ice wedging.
Acid Rain; Catastrophic Mass Movements; Depositional Environments; Dunes; Eolian Processes; Faults and Fractures; Freezing and Melting; Glacial Landforms; Glaciation; Hydrothermal Processes; Ice Heaving and Ice Wedging; Impact Crater; Landforms; Landscape Evolution; Leaching; Oxidation-Reduction Reaction; Precipitation; Rapids and Waterfalls; Rate Factors in Geologic Processes; Rock; Rockfall; Salt Wedging; Seawalls and Beach Erosion; Soil and Soil Horizons; Talus Pile or Talus Slope.