Magnetometryðum
Magnetometry is a non-invasive geophysical technique used to detect and map variations in the Earth's magnetic field. These variations are caused by differences in the magnetic properties of subsurface materials, such as rocks and man-made objects. Essentially, magnetometry measures the strength and direction of the magnetic field at various points to create a map.
The primary tool used in magnetometry is the magnetometer, which can measure very small changes in the
These anomalies can indicate the presence of a variety of subsurface features. For instance, in archaeology,