If you want  a copy of these files, please contact us at

Outreach materials

(Español) Hoja de Ruta “Factibilidad de cogeneración geotérmica en Puyuhuapi...

(Español) La Tierra de Fuego. Gente y naturaleza marcadas por el calor profundo...

Does Puyuhuapi need Geothermal Energy? Results of the feasibility study for the insta...

Panguipulli’s greenhouse infograph...

Puyuhuapi’s Green Identity Poster...

Hipólito Muñoz Hot Springs Infographics...

(Español) Infografías Escuela Curacautín...

(Español) Gráficas Liceo Altos del Mackay...

(Español) Infografía Encuesta de Pobreza Energética en Puyuhuapi...

(Español) Folleto Informativo de Cogeneración para Puyuhuapi...

(Español) Libro CEGA AR GEO...

(Español) Libro Acordeón Viaje al Centro del Volcán...

(Español) Bomba de Calor con Realidad Aumentada...

CEGA presents​ new ​ infographic “Feel the energy of the Andes”...

(Español) LIBRO DE ACTIVIDADES EXPLORA CONICYT: Distintos experimentos para aprender...

ARMA TU VOLCÁN: Imagen recortable para profesores de ciencia y público general....

Proyecto EXPLORA CONICYT de Valoración y Divulgación de la Ciencia y la Tecnología...

Libro “La Tierra de Fuego, Gente y Naturaleza marcadas por el calor profundo”...

Geothermal information

Geothermal Energy in Chile

Chile is one of the regions with the highest volcanic activity on the planet, given its privileged position in the so-called "Pacific Ring of Fire", the country has about 20% of continental active volcanoes. This strategic situation also implies a high potential in Chile for the generation of geothermal energy. The ...

Read more

Geothermal purposes of Geothermal Energy in Chile

Through a series of articles, it invites you to find out who is using geothermal energy in Chile and the benefits that injecting clean and reliable energy into their work has brought them. Viña Maquis Escuela Linares de Casma Termas de Puyehue Wellness & Spa Resort Invernadero geotérmico en Lampa ...

Read more

Volcanoes of Chile: Landscape with a lot to be said

Chile is a country of volcanoes.  We are escorted by almost 3,000 of them in our Andes mountain range, 150 of which are considered active. Risky? Maybe, but it's also encouraging. Volcanoes are not only the origin of natural disasters, they have a potential for generating geothermal energy that in our country can repr...

Read more

Serie Documental “La Fuerza de la Tierra”

Serie documental educativa de seis capitulos, La Formación de la Tierra, Volcanes, Energía, Rocas y Minerales, Sismos y Tectónica y Cambio Climático. La serie es una coproducción del Consejo Nacional de Televisión y el Programa Eureka de la Fundación Ciencia para la Vida. Ver video...

Read more


What is Geothermal Energy?

Geothermal energy is what produces the internal heat of the Earth and has been concentrated in the subsoil,  in places known as geothermal reservoirs, which, if well managed, can produce clean energy indefinitely. Yes, Indefinitely

Check the following  video:  “What is geothermal?”

“What is Geothermal Energy?”

How is it formed?

The earth’s crust is not flat.  it is divided into eight large plates and more than 20 smaller plates that with its movement  push each other slowly, at about 5 to 10 centimeters a year, which is about the same speed as your nails grow.


When the plates come together, one can slide under the other, allowing the generation of magma that can sometimes reach the surface generating volcanoes. In most cases, the magma does not go outside, but it is capable of heating large underground areas.


This heat source, magma, is one of the main elements of a geothermal system, but two more are needed to generate a reservoir: an aquifer and a seal. The aquifer is a permeable rock formation, that is, it allows water or other fluids to pass through it. And the seal is another layer of rocks, but waterproof. These three elements must be mounted one on top of the other, the heat source, on top of the aquifer and on top of them, the cover. It’s like a pressure cooker.


So, imagine this. It’s raining. The water slides along the earth’s surface and penetrates into the subsoil through faults and fractured rocks, which function as real pipes. The water is trapped in the aquifers, where it circulates and heats up, but it cannot go outside in its entirety, because it is covered by a layer of impermeable rock that prevents its passage. When these conditions occur, we are facing a geothermal reservoir.


Geysers and hot springs are some examples of what happens when some of this hot water or steam rises to the surface. As in our pot, it is possible that some of the steam escapes from the lid, although at much higher temperatures, above 150°C, and that makes them a huge source of energy.


In some cases, there are no natural water sources (such as rain or snow) to generate this circuit. In that case, the water can be injected artificially, and the phenomenon that will occur is the same.

How we can make use of it?

Geothermal energy can be used directly to heat homes, temper greenhouses and fish farms, dehydrate vegetables, dry wood, among other applications.

This energy can also be used indirectly, to produce electricity. Generally, the force generated by the steam is used to drive a turbine capable of moving an electric generator, for instance.


Revisa video  “Los usos directos de la Geotermia”

Where can it be exploided?

In our planet there are places recognized for their great geothermal activity. The most extensive of them is the so-called “Pacific Ring of Fire”. This is a hughe  40,000-kilometer zone in the shape of an arc that crowns the ocean that gives it its name. Chile is one of the countries that is inserted in this circuit of fire, which place our country as a territory with great potential for the generation of geothermal energy.

Chile has more than 150 active volcanoes and an equal number of dormant volcanic centers that show geothermal activity. There are two main volcanic zones within the Chilean Andes: the North Volcanic Zone (17ºS – 28ºS) and the Center-South Volcanic Zone (33ºS – 46ºS). Today, the Andean Chain represents one of the largest untapped geothermal provinces in the world.

Geothermal energy has been used on a large scale since the beginning of the 20th century in Italy, and mainly in volcanic areas such as Iceland, the Philippines, New Zealand and some regions of California.

In Latin America, geothermal energy has also begun to be explored as a reliable source of energy. To learn more about the projects in the region and their progress, you can check this World Bank site.

Banco Mundial.


What are the stages of development in a geothermal energy plant?

The first stage is Exploration, which can be carried out in territories granted by the Ministry of Energy. During this stage, experts visit the area to take samples (water, temperature, rocks, and minerals) to characterize the resource and locate the exploratory wells.

The second stage is Exploratory drilling, where drilling is carried out to depth (approximately 2,000 m) to determine if the geothermal resource at that location is of commercial importance.

Then it goes to an Evaluation and Confirmation stage, where the size of the resource and the feasibility of its economic development will be determined.

If the results of the previous stage are positive, the Development stage follows, which will consist of the construction of the power plant, transmission lines, surface pipelines, production facilities and well drilling. Subsequently, in the Operation stage, the generation of electricity will soon be produced.

Which countries have developed geothermal energy?

Geothermal energy has been used on a large scale since the beginning of the 20th century in Italy, and mainly in volcanic areas such as Iceland, the Philippines, New Zealand and some regions of California (USA), where classical geothermal systems use the natural water that circulates near hot volcanic chambers or similar bodies.

Chile’s location in the so-called “Pacific Ring of Fire” makes it one of the regions with the highest volcanic activity in the world, which logically implies great potential for generating geothermal energy in our country.

Where do hot springs come from?

Thermal waters correspond to surface emissions of warm to hot water with compositions rich in salts and dissolved gases. These thermal emissions are the result of groundwater heating by: (a) proximity effects with an anomalous heat source, in other words,  rocks heated by subsurface magma, or (b) geothermal gradient effect, which is the warming of groundwater that occurs as we go deeper into the earth’s crust.

Does geothermal energy exploitation affect tourism or recreational hot springs?

Geothermal exploitation does not affect tourism and/or recreational hot springs if it is carried out in a sustainable manner.

Modern geothermal plants use the hot water extracted from geothermal wells in combined cycles to generate steam and drive electricity generation turbines. The extracted water is re-injected into the geothermal reservoir, thus maintaining the hydrological balance.

What are the closest places to Santiago where we can find volcanoes and geysers to visit for tourism?

The closest volcano to Santiago is Tupungatito (5,640 m high), about 75 km east of the capital. It is followed by the San José volcanic complex (5,880 m) 80 km south east of Santiago and next to it, the Marmolejo volcano (6,109 m). A little further down is the Maipo (5,290 m) 110 km from the city. In the surroundings of Santiago there are no geyser-type thermal manifestations.

Is there any relation between geysers and volcanoes?

Both, geysers and volcanoes depends on the presence of a heat source deep on earth. However, the eruption mechanisms are different. Geysers are very rare and superficial singularities, where groundwater is heated to the point of boiling, which produces a violent emission of liquid water and water vapor.

After the eruption of the geyser, which can be periodic or sporadic, a new cycle begins as a result of the entry of cold water that begins its gradual heating process.

Geysers, therefore, do not need to be associated with a volcano, but they do occur in regions where there is intense volcanic activity.

Why are geysers bigger in the morning?

The reason for the larger size of the geysers at dawn, is more apparent than real, and is related to the low temperatures that exist between 4 and 7 AM, which produce greater condensation of the steam emitted by the geysers.

This effect translates into a greater perception of the steam emitted by the geyser, just like when we expel the air from our lungs on the coldest mornings of the year


13 de August 2022

(Español) Chile Conectado: Escuela de Curacautín usa el calor de la tierra para calefaccionar salas

Sorry, this entry is only available in European Spanish....

Read more
09 de August 2022

(Español) Curso Geotermia Somera, Bombas de Calor y Usos Directos, a cargo del CEGA

Sorry, this entry is only available in European Spanish....

Read more
09 de August 2022

(Español) Escuela de Curacautín calefacciona sus salas con geotermia de uso directo

Sorry, this entry is only available in European Spanish....

Read more
01 de August 2022

(Español) Energía Infinita – Geotermia

Sorry, this entry is only available in European Spanish....

Read more

CEGA's Bulletin

(Español) Boletín agosto 2022

August 2022

(Español) Boletín abril 2022

April 2022

(Español) Boletín Mayo-Julio 2021

August 2021

(Español) Boletín Enero-Mayo 2021

May 2021

(Español) BOLETÍN 2° SEMESTRE 2020

January 2021

(Español) BOLETÍN N. 24 MAYO- JULIO 2019

August 2019

(Español) BOLETIN N. 23 MARZO – ABRIL 2019

April 2019

(Español) Boletín Nº 22 NOVIEMBRE y DICIEMBRE 2018

January 2019

(Español) Boletín N. 21 MAYO y JUNIO de 2018

June 2018

(Español) Boletín N. 20. MARZO- ABRIL 2018

April 2018

(Español) Boletín N. 19 ENERO 2018

January 2018

(Español) Boletín N. 18

November 2017

(Español) Boletín N. 13

October 2017

(Español) BOLETÍN N. 12

August 2017

(Español) Boletín N. 11

July 2017

(Español) Boletín N° 10

June 2017

(Español) Boletín N° 9

May 2017

(Español) Boletín n° 8

April 2017

Boletín Nº7

January 2017

(Español) Boletín Nº6

December 2016

(Español) Boletín nº5

November 2016

(Español) Boletín Nº4

October 2016

Boletín N° 3

September 2016

Boletín N° 2

August 2016

Boletín N° 1

July 2016