Geophysics in education emphasizes the practical application of geophysical methods to address various challenges and gain insights into the Earth's structure, composition, and processes.

Gravimetry is a geophysical technique that measures variations in the Earth's gravitational field to infer information about the subsurface density distribution and geological structures.

The seismic reflection method involves generating seismic waves and recording their reflections from subsurface layers to create images of geological structures.

Magnetotellurics is a geophysical method that measures natural variations in the Earth's magnetic and electric fields to investigate the electrical conductivity structure of the subsurface.

Electrical resistivity tomography is a geophysical technique that measures the electrical resistivity of the subsurface to create images of geological structures and identify variations in material properties.

Seismic refraction is a geophysical method that analyzes the refraction of seismic waves at subsurface boundaries to determine the velocity and depth of geological layers.

Ground-penetrating radar is a geophysical technique that uses electromagnetic waves to image subsurface structures, commonly employed in archaeological surveys, environmental investigations, and utility mapping.

Gamma-ray spectrometry is a geophysical technique that measures the natural radioactivity of the Earth's materials to determine their elemental composition and identify radioactive isotopes.

Seismic tomography is a geophysical technique that uses seismic waves to create images of the Earth's internal structure, providing insights into geological formations and tectonic processes.

Ground-penetrating radar is a geophysical method that uses electromagnetic waves to image subsurface structures, commonly employed in archaeological surveys, environmental investigations, and utility mapping.

Magnetic resonance imaging is a geophysical technique that uses electromagnetic waves to image subsurface structures, commonly employed in archaeological surveys, environmental investigations, and utility mapping.

Well logging is a geophysical technique that involves measuring various physical properties of the Earth's subsurface, including temperature, electrical conductivity, and density, using instruments lowered into boreholes.

Electrical resistivity tomography is a geophysical technique that measures the electrical resistivity of the subsurface to create images of geological structures and identify variations in material properties.

Seismic refraction is a geophysical method that analyzes the refraction of seismic waves at subsurface boundaries to determine the velocity and depth of geological layers.

Ground-penetrating radar is a geophysical technique that uses electromagnetic waves to image subsurface structures, commonly employed in archaeological surveys, environmental investigations, and utility mapping.