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The Philippines was then followed by Indonesia, which had 1340 MWe. [6] Early statistics from the Institute for Green Resources and Environment stated that Philippine geothermal energy provides 16% of the country's electricity. [7] By 2005, geothermal energy accounted for 17.5% of the country's electricity production. [8]
At present, geothermal wells are rarely more than 3 km (1.9 mi) deep. [3] Upper estimates of geothermal resources assume wells as deep as 10 km (6.2 mi). Drilling near this depth is now possible in the petroleum industry, although it is an expensive process.
Geothermal systems tend to benefit from economies of scale, so space heating power is often distributed to multiple buildings, sometimes whole communities. This technique, long practiced throughout the world in locations such as Reykjavík , Iceland ; [ 7 ] Boise , Idaho ; [ 8 ] and Klamath Falls , Oregon ; [ 9 ] is known as district heating .
The Tongonan Geothermal Power Station [1] is a 232.5 MW geothermal power plant or an earth steam turbined electric generator—the world's largest geothermal power plant under one roof located in Tongonan, Kananga, Leyte, Philippines. The power plant is one of four operating in the Leyte Geothermal Production Field. [1]
The Bac-Man Geothermal Production Field, also known as the BacMan Geothermal Power Plant, is one of the geothermal power stations operated by Energy Development Corporation in the provinces of Albay and Sorsogon in the Philippines. It is named for its location in the municipalities of Bacon (a district since merged with Sorsogon City) and Manito.
The Mount Apo Geothermal Power Plant is a geothermal power station located in Barangay Ilomavis, Kidapawan, Cotabato. Drawing steam from the Mindanao Geothermal Production Field, [ 3 ] the power station is situated near the foot of Mount Apo and has a power output of 106 MW.
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Geothermal activity is a group of natural heat transfer processes, occurring on Earth's surface, caused by the presence of excess heat in the subsurface of the affected area, usually caused by the presence of an igneous intrusion underground. [1]