Magnetometry is a geophysical method that measures variations in the Earth's magnetic field. It is often used in archaeology to detect buried features that contain magnetic materials, such as iron objects or kilns.

Ground-penetrating radar (GPR) is a geophysical method that uses radar pulses to image the subsurface. It is often used in archaeology because it can provide high-resolution images of buried features, such as walls, foundations, and artifacts.

Microgravity is a geophysical method that measures small variations in the Earth's gravitational field. It is often used in archaeology to detect buried caves and tunnels, which can cause slight changes in the gravitational field.

Electrical resistivity is a geophysical method that measures the electrical resistance of the subsurface. It is often used in archaeology to detect buried features that have different electrical properties than the surrounding soil. However, electrical resistivity is sensitive to changes in soil moisture, which can make it difficult to interpret the results of a survey.

Seismic reflection is a geophysical method that uses sound waves to image the subsurface. It is often used in archaeology to study the structure of archaeological sites, such as the layout of buildings and the depth of buried deposits.

Magnetic susceptibility is a geophysical method that measures the magnetic properties of the subsurface. It is often used in archaeology to detect buried magnetic materials, such as iron objects or kilns. However, magnetic susceptibility can also provide information about the age of buried features, as the magnetic properties of soil can change over time.

Magnetometry is a geophysical method that measures variations in the Earth's magnetic field. It is often used in archaeology to detect buried metal objects, which can cause disturbances in the magnetic field.

Seismic refraction is a geophysical method that uses sound waves to image the subsurface. It is often used in archaeology to study the structure of archaeological sites, such as the layout of buildings and the depth of buried deposits. However, seismic refraction is limited in its ability to detect small buried features, as the sound waves can only penetrate a few meters into the ground.

Paleomagnetism is a geophysical method that studies the Earth's magnetic field in the past. It is often used in archaeology to study the environmental context of archaeological sites, such as the climate and vegetation during the time the site was occupied.

Electrical resistivity is a geophysical method that measures the electrical resistance of the subsurface. It is often used in archaeology to detect buried features that have different electrical properties than the surrounding soil, such as walls, foundations, and artifacts.

Radiocarbon dating is a scientific method for determining the age of organic materials by using the presence of carbon-14, a radioactive isotope of carbon. It is often used in archaeology to date buried organic materials, such as wood, bone, and leather.

Ground-penetrating radar (GPR) is a geophysical method that uses radar pulses to image the subsurface. It is often used in archaeology to detect buried features, such as walls, foundations, and artifacts. However, GPR is limited in its ability to detect small buried features, as the radar waves can only penetrate a few meters into the ground.

Hydrogeophysics is a geophysical method that studies the movement of water in the subsurface. It is often used in archaeology to study the hydrology of archaeological sites, such as the location of water sources and the flow of groundwater.

Seismic reflection is a geophysical method that uses sound waves to image the subsurface. It is often used in archaeology to study the structure of archaeological sites, such as the layout of buildings and the depth of buried deposits. Seismic reflection can penetrate deep into the ground, which makes it useful for studying buried features that are located at great depths.

Forensic anthropology is a scientific method for studying human remains. It is often used in archaeology to detect and analyze buried human remains, such as skeletons and mummies. Forensic anthropology can provide information about the age, sex, and health of the deceased, as well as the cause of death.