geotherm

A geotherm is a graph that shows how temperature increases with depth below the Earth's surface. Generally, as you go deeper, the temperature rises due to heat from the Earth's interior, which is generated by the decay of radioactive elements and residual heat from the planet's formation. This gradient varies depending on location and geological conditions, influencing geothermal energy potential, natural resources, and volcanic activity. Understanding geotherms helps scientists study the Earth's internal processes and assess the feasibility of geothermal energy for sustainable power generation.