
The study of the Earth's physical properties and processes, including gravity field mapping.Geophysics is the branch of physics that studies the Earth's physical properties and processes — its gravity field, magnetic field, seismic waves, heat flow, and internal structure. It bridges geology and physics, using quantitative methods to probe what lies beneath the surface without direct observation. From mapping the ocean floor to monitoring volcanic activity, geophysics provides a window into the planet's dynamic interior and its evolution over billions of years.
The field emerged in the late 19th century with the development of precise instruments for measuring gravity and magnetism, and it gained major momentum after the 1906 San Francisco earthquake, which spurred systematic seismological research. The theory of plate tectonics, confirmed in the 1960s, was a triumph of geophysical data synthesis.
Geophysicists measure physical fields and signals that propagate through or emanate from the Earth. For example, gravity mapping detects variations in the gravitational pull caused by density differences in the subsurface; seismology uses the travel times of earthquake-generated waves to infer the layering of the crust and mantle; and electromagnetic surveys measure conductivity to locate water or mineral deposits. These measurements are inverted mathematically to build models of the Earth's interior.
Geophysics is used in natural resource exploration (oil, gas, minerals), earthquake hazard assessment, groundwater mapping, and even planetary science — the same techniques are applied to study other planets and moons.
Neutrino tomography, a cutting-edge geophysics technique, uses particles that pass through the entire Earth to create 3D images of the planet's interior, much like X-rays image the human body.









