Geomorphology is the study of landforms and landform evolution. The topic traditionally has been studied both qualitatively, which is the description of landforms, and quantitatively, which is process-based and describes forces acting on Earth's surface to produce landforms and landform change.
It is the study of the relations between landforms and the underlying rocks i.e. Geological
Geomorphology is concerned with the interactions between denudation processes and the rock strength. Hence, in the precise investigation of the resistance of rocks to denudation, detailed experimental work on rocks must be carried out.
In its second sense, geomorphology is the study of the evolution of landscapes. Such studies have been termed denudation chronology. Such studies attempts to reconstruct succession of pictures of the relief at different times. Alterations of relief are usually believed to have been caused by changes of base level and climate.
The third aspect of geomorphology is the study of the actual process of erosion which give rise to landforms. Unlike the first two aspects of Geomorphology, which are essentially regional in approach, this third aspect is systematic. It aims to understand the action of waste movement of water movement, ice, and wind as well as the processes of weathering
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Geomorphology is the study of landforms and landform evolution. The topic traditionally has been studied both qualitatively, which is the description of landforms, and quantitatively, which is process-based and describes forces acting on Earth's surface to produce landforms and landform change.
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It is the study of the relations betweenlandforms and the underlying rocks i.e.
Geological
Geomorphology is concerned with the
interactions between denudation
processes and the rock strength. Hence, in the precise investigation of the resistance of rocks to denudation, detailed experimental work on rocks must be carried out.
In its second sense, geomorphology is the study of the evolution of landscapes. Such studies have been termed denudation chronology. Such studies attempts to reconstruct succession of pictures of the relief at different times. Alterations of relief are usually believed to have been caused by changes of base level and climate.
The third aspect of geomorphology is the study of the actual process of erosion which give rise to landforms. Unlike the first two aspects of Geomorphology, which are
essentially regional in approach, this third aspect is systematic. It aims to understand the action of waste movement of water movement, ice, and wind as well as the processes of weathering