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Geophysics (/ ˌ dʒ iː oʊ ˈ f ɪ z ɪ k s /) is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis.
Geophysics is: The subsurface site characterization of the geology, geological structure, groundwater, contamination, and human artifacts beneath the Earth's surface, based on the lateral and vertical mapping of physical property variations that are remotely sensed using non-invasive technologies.
Geophysics deals with a wide array of geologic phenomena, including the temperature distribution of the Earth’s interior; the source, configuration, and variations of the geomagnetic field; and the large-scale features of the terrestrial crust, such as rifts, continental sutures, and mid-oceanic ridges.
Geophysics basically consists of the application of physics and mathematics to study the Earth, the oceans, the atmosphere and the near-Earth space. It is a very broad branch of geology that is supported by several other sciences such as: physics, astronomy, geology, environmental sciences, oceanography and meteorology.
Geophysics is the application of physics to study the Earth, oceans, atmosphere and near-Earth space. It is a broad subject that encompasses many of the major sciences – physics, astronomy, planetary science, geology, environmental science, oceanography, and meteorology.
Geophysics is a field of earth sciences that uses the methods of physics to investigate the complex physical properties of the Earth and the natural processes that have determined and continue to govern its evolution.
Geophysics is a quantitative natural science that examines the physical processes and properties of the Earth. Geophysicists aim to understand the shape, gravitational and magnetic fields, internal structure and composition, and the surficial processes of the Earth.