Geomorphology-online-journals
Geomorphology (from Ancient Greek: γῆ, gê, "earth"; μορφή, morphḗ, "form"; and λÏŒγος, lógos, "study") is that 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 layer. Geomorphologists seek to know why landscapes look the way they are doing, to know landform
history and dynamics and to predict changes through a mix of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines like physiography, geology, geodesy, engineering geology, archaeology, climatology and geotechnical engineering. This broad base of interests contributes to several research styles and interests within the sphere.
Earth's surface is modified by a mixture of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the
coastal geography. Surface processes comprise the action of water, wind, ice, fire, and living things on the surface of the world, together with chemical reactions that form soils and alter material properties, the steadiness and rate of change of topography under the force of gravity, and other factors, like (in the very recent past) human alteration of the landscape. Many of those factors are strongly mediated by climate.
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