How springs are heated geothermally by underlying?

Springs are heated geothermally by the heat from the Earth's interior, which is transferred to groundwater as it percolates through heated rock formations. This geothermal energy raises the temperature of the water, causing it to rise to the surface as a spring. The heat can originate from various sources, including volcanic activity, hot magma, or the natural decay of radioactive materials in the Earth's crust. As a result, these springs can exhibit warm or hot temperatures, contributing to geothermal features like hot springs and geysers.