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These landforms differ only on the steepness of their backslopes and the relative differences in the inclination of their backslopes and frontslopes. These differences depend upon whether the dip of the strata from which they have been eroded are either nearly vertical, moderately dipping, or gently dipping.
Geomorphology (from Ancient Greek γῆ (gê) 'earth' μορφή (morphḗ) 'form' and λόγος 'study') [2] is the scientific study of the origin and evolution of topographic and bathymetric features generated by physical, chemical or biological processes operating at or near Earth's surface.
Because of their gradational nature, the exact angle of dip and slope that separates these landforms is arbitrary and some differences in the specific angles used to define these landforms can be found in the scientific literature. It also can be difficult to distinguish immediately adjacent members of this series of landforms. [3] [5]
Bioerosion is the weathering and removal of abiotic material via organic processes. [10] This can either be passive or active. Moreover, bioerosion is the chemical and or the mechanical weathering of landforms due to organic means. [3] Bioprotection is essentially the effect that organisms have on reducing the action of geomorphic processes.
This type of grading is relatively uncommon but is characteristic of sediments deposited by grain flow and debris flow. [2] A favored explanation for reverse grading in these processes is kinetic sieving. [3] It is also observed in aeolian processes, such as in pyroclastic fall deposits. [4] These deposition processes are examples of granular ...
The geomorphological processes involved with distinct climates can have large impacts on the near-surface geology of the area. [1] However, only some processes and landforms can be associated with particular climates, meaning that they are zonal; processes and landforms not associated with particular climates are labelled azonal. [2]
The boundaries between facies (and corresponding areas on the temperature v. pressure graph) are wide because they are gradational and approximate. [1] The area on the graph corresponding to rock formation at the lowest values of temperature and pressure is the range of formation of sedimentary rocks , as opposed to metamorphic rocks, in a ...
The geographic cycle, or cycle of erosion, is an idealized model that explains the development of relief in landscapes. [1] The model starts with the erosion that follows uplift of land above a base level and ends, if conditions allow, in the formation of a peneplain. [1]
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