The main difference between etchplanation and pediplanation is at the second stage of their granite weathering processes.
At the second stage of the etchplanation weathering process, exhumation occurs downwards, weathering granite vertically - resulting in steep sided granite landforms such as inselbergs or tors.
For the pediplanation process however, exhumation occurs laterally, forming usually broad and gently sloping land surfaces. Accompanying the pediplanation process are usually river erosion processes, thus further widening the valley and even forming extensive plains (pediplanes).
Etchplanation is a process of weathering and erosion that involves the chemical dissolution of rocks, while pediplanation is the process of physical erosion and smoothing of rock surfaces due to factors like wind, water, and ice. In other words, etchplanation primarily involves chemical weathering, while pediplanation involves physical weathering.
Pediplanation is the process where wind-blown sand particles erode surfaces by abrasion, smoothing and planing them down over time. On the other hand, etchplanation refers to the chemical dissolution of mineral surfaces by acidic solutions, resulting in the formation of etch pits or grooves on the surface. Both processes play a role in shaping landscapes through surface erosion and dissolution.
The name for the elevation difference between adjacent contour lines is the contour interval.
The difference between 14 degrees and -5 degrees is 19 degrees. If you are calculating the absolute value of the temperature difference, it would be the same as 19 degrees.
To find the difference between -127 degrees Fahrenheit and 136 degrees Fahrenheit, you would subtract -127 from 136. This gives a difference of 263 degrees Fahrenheit.
The temperature difference between -30 degrees and 20 degrees is 50 degrees. Negative 30 degrees is 50 degrees lower than 20 degrees.
Pediplanation is the process where wind-blown sand particles erode surfaces by abrasion, smoothing and planing them down over time. On the other hand, etchplanation refers to the chemical dissolution of mineral surfaces by acidic solutions, resulting in the formation of etch pits or grooves on the surface. Both processes play a role in shaping landscapes through surface erosion and dissolution.
The theory of pediplanation suggests that slopes are developed by the gradual lowering of a land surface due to weathering, erosion, and mass wasting processes. The theory of etchplanation, on the other hand, proposes that slopes are formed through the selective removal of material by chemical weathering and erosion, such as through the dissolution of rocks or minerals. Both theories contribute to our understanding of slope development in different geological contexts.
Etchplanation is the dual process of deep weathering followed by exhumation.
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