El Tatio is a geyser field located within the Andes Mountains of northern Chile along the border between of Bolivia. Before the sun starts to rise, early morning more than 60 geysers, hot springs, mud pools, mud volcanoes and many fumaroles spew hot waters and steam. The largest geyser in the southern hemisphere is 4.320 meters above sea level. El Tatio is also third largest geyser field in the world, (after Yellowstone in the U.S. and the Valley of Geysers on the Kamchatka Peninsula in Russia) covers an area of 12 square miles seeping steam across its surreal expanse. The El Tatio geyser field is a spectacular sight, a dreamlike high-altitude location surrounded by stratovolcanoes that form part of the local geothermal system. Geothermal power is the energy that comes from the internal heat of the Earth, and where the heat flow from the interior of the globe is sufficiently high can be used both for heating purposes and for the generation of electrical power.
El Tatio has extremophile microorganisms, which is possible of analogous example of life on early Earth and potential past life on Mars. The exclusive environment of El Tatio “provides a better environmental analog for Mars than those of Yellowstone National Park and other well-known geothermal sites on Earth.” Depending on the season, the hot springs yield 0.25–0.5 cubic meters per second of water at temperatures reaching the local boiling point. The Chilean government and private companies are looking the idea of harnessing the geothermal energy, but could not succeed due to El Tatio’s remote location and environmental concerns have stalled any geothermal power projects. In 2010, the site was declared a protected area, however tourism remains the main business at El Tatio. The el Tatio, geyser field is also known as the Copacoya geysers.
The first geothermal prospecting of the field occurred in the 1920s particularly noticeable in cold weather. The field once numbered 67 geysers and more than 300 hot springs, as some geyser fountains reached heights of over 10 meters usually however they do not exceed 1 meter. The hydrothermal activities are main reason of discoloring the several volcanoes of El Tatio volcanic group. El Tatio is a tourism destination, with substantial amounts of travelers both from Chile and other countries play an integral part of economic resource for the region, as more than 400 daily visitors comes here to see these exclusive geysers.
The water is rich in minerals, especially sodium chloride, rubidium, strontium, bromine, magnesium, cesium, lithium, arsenic, sulfate, boron, potassium, silica and calcium. Hydrothermal alteration at El Tatio, has also yielded large deposits of alteration minerals such as illite, nobleite, smectite, teruggite and ulexite. Moreover, El Tatio and a number of other geothermal fields have been dominated by andesitic volcanism producing lava flows until the late Miocene, large scale ignimbrite activity took place between 10 and 1 million years ago. The toxic minerals like arsenic which pollutes a numbers of waters in this area, causing health issues in the population. The climate is dry falling between December and March, rather windy, which influences the hot springs by enhancing evaporation. This region has extreme temperature variations between day and night. El Tatio lies at high altitude, regularly leading to altitude sickness, and the cold dry climate creates further danger.
Further El Tatio area has exposure to the hot gases and water can result in burn injuries, and both sudden eruptions of geysers and fountains and fragile ground above vents and above boiling water, concealed beneath thin covers of solid ground, increase the risk to unwary travelers. The hot spring waters enter the ground east and south east of El Tatio is controlled by the permeability of the volcanic material. Unlike geothermal fields in wetter parts of the world, given the dry climate of the area local precipitation does have little influence on the hot springs hydrology at El Tatio. The time the water takes to traverse the whole path from precipitation to the springs is about 15 years.
The water travels through a number of aquifers which correspond to permeable rock formations through faults and fractures in the rock. Magmatic brine is mixed into this water and the mixture ultimately becomes the water that emerges at El Tatio. This area dry grassland vegetation are Tussock grasses like Anatherostipa, Festuca, Stipa while rosette and cushion plants, Azorella, Chaetanthera, Mulinum, Senecio, Lenzia, Pycnophyllum and Valeriana. El Tatio geyser field, one of San Pedro de Atacama’s most popular surrounding attractions, so don’t miss whenever you go Chile. The natural marveling at the geothermal wonders provides breathtaking views for taking pictures.