Heat Flow and Geothermal Studies

Heat flow refers to the movement of heat from the Earth’s interior to its surface. In tectonophysics, understanding this flow helps scientists study geological processes, such as earthquakes and volcanic activity. Geothermal studies measure subsurface temperatures and analyze how heat transfers through rocks and fluids. This research reveals how tectonic plates interact and shape our planet. By examining heat flow and geothermal activity, scientists gain insights into Earth's evolution, resource potential, and natural hazards, contributing to both environmental understanding and practical applications like geothermal energy production.