The use of geothermal energy dates back thousands of years, with early civilizations employing hot springs for bathing and heating purposes. Modern applications, however, began in the late 19th century, when the first geothermal power plant was constructed in Larderello, Italy, in 1904. Today, geothermal energy is widely utilized in countries like Iceland, the Philippines, Kenya, and the United States, where abundant geothermal resources exist.
There are three primary methods of extracting geothermal energy: direct use, geothermal heat pumps, and power generation. Direct use involves tapping into shallow ground or hot water sources for heating buildings, greenhouses, or industrial processes. Geothermal heat pumps, on the other hand, transfer heat from the relatively stable underground temperature to buildings in colder climates. For electricity generation, deep wells are drilled into high-temperature reservoirs, where steam or hot water drives turbines connected to generators.
Geothermal energy is considered a clean and sustainable resource because it produces minimal greenhouse gas emissions and has a small land footprint compared to other energy sources. However, its development is geographically limited to areas with sufficient heat and permeability near the surface. Challenges also include high initial drilling costs, potential seismic activity from stimulation techniques, and the need for careful resource management to ensure long-term sustainability.
Despite these limitations, geothermal energy plays a significant role in diversifying global energy portfolios and reducing dependence on fossil fuels. Ongoing advancements in drilling technology and enhanced geothermal systems (EGS) aim to expand access to geothermal resources in regions previously considered unsuitable.