Shaping of Landscape: A primer on weathering and erosion
Landscape as process, beautifully illustrated. Students with Marli Miller as instructor are fortunate indeed
Most of us love landscapes –and many of us find ourselves wondering how they came to look the way they do. In most cases, landscapes take their shape through the combined processes of weathering and erosion. While weathering and erosion constitute entire fields of study unto themselves, this primer outlines some of the basics—which pretty much underlie all the further details of how natural processes shape landscapes.
Aerial view of incised meanders of Green River, Utah.
Two definitions: weathering describes the in-place breakdown of rock material whereas erosion is the removal of that material. Basically, weathering turns solid rock into crud while erosion allows that crud to move away.
Weathering processes fall into two categories: physical and chemical. Physical weathering consists of the actual breakage of rock; any process that promotes breakage, be it enlargement of cracks, splitting, spalling, or fracturing, is a type of physical weathering. Common examples…
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Posted on December 1, 2018, in Geology and tagged cementation, dolomite, erosion, feldspar, limestone, Marli Miller, sandstone, siltstone, undercutting, weathering. Bookmark the permalink. Leave a comment.