Branches of geology :
Geology can be divided into several fields, which can be mainly grouped under physical and historical geology.
Physical Geology
Physical geology includes:
Mineralogy - the study of the chemical composition and structure of minerals.
Petrology - the study of the composition and origin of rocks.
Geomorphology - the study of the origin of landforms and their modification by dynamic processes.
Geochemistry - the study of the chemical composition of earth materials and the chemical changes that occur within the earth and on its surface.
Geophysics - the study of the behavior of rock materials in response to stresses and according to the principles of physics.
Geophysics - the study of the behavior of rock materials in response to stresses and according to the principles of physics.
Sedimentology - the science of the erosion and deposition of rock particles by wind, water, or ice.
Structural geology - the study of the forces that deform the earth's rocks and the description and mapping of deformed rock bodies.
Economic geology - the study of the exploration and recovery of natural resources, such as ores and petroleum.
Engineering geology - the study of the interactions of the earth's crust with human-made structures such as tunnels, mines, dams, bridges, and building foundations.
Engineering geology - the study of the interactions of the earth's crust with human-made structures such as tunnels, mines, dams, bridges, and building foundations.
Historical geology deals with the historical development of the earth from the study of its rocks. Historical geology includes :
Paleontology - the systematic study of past life forms.
Stratigraphy, of layered rocks and their interrelationships.
Paleogeography, of the locations of ancient land masses and their boundaries; and
Geologic mapping - the superimposing of geologic information upon existing topographic maps.
Paleontology - the systematic study of past life forms.
Stratigraphy, of layered rocks and their interrelationships.
Paleogeography, of the locations of ancient land masses and their boundaries; and
Geologic mapping - the superimposing of geologic information upon existing topographic maps.
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