Did you know… there is a submarine volcano in Antarctica?
Deception Island, Antarctica is home to an active submarine volcano which has created a large volcanic crater in the middle of the South Shetland Islands.
The total land area of the island is 98.5 km2(~38.0 mi2), with a diameter of 15 km (~9.3 mi). The island rises up to 539 m (~1768.4 ft) above the sea level. More than 57% of the island is covered by permanent glaciers.
The average annual air temperature is -3˚C (26.6˚F); however, temperatures can range from a high of 11˚C to a chilly -28˚C (51.8˚F to -18.4˚F.)
The island’s geothermal heat is found just below the surface. This means visitors can dig a shallow depression into black sand beaches to enjoy the warmth - especially appealing after taking a
Technically, there are no official hot springs on the island, however, along the shoreline of Pendulum Cove, there are thermal springs with temperatures over 70˚C (158˚F). Due to the mixture the cold and hot water, a natural hot tub is created.
But before you jump in, consult a trained expert or experienced expedition guide. They know which areas are safe for a relaxing soak in the steamy water.
Stay tuned to learn about the other active volcano, Erebus.
Did you know… Alaska uses geothermal energy to produce electricity?
It might seem highly unlikely that geothermal energy could be harnessed in the Arctic climate of Alaska considering HOT water is required. However, this is not the case! Geothermal reservoirs can be found almost anywhere in the world. In fact, Alaska has 97 known thermal springs and is one of eight states to use geothermal energy to produce electricity. The first geothermal power plant in Alaska launched in 2006 at Chena Hot Springs and can generate up to 730 kilowatts of power. It is located in the Interior hot springs geothermal region.
The Chena Hot Springs Resort uses geothermal energy in many different ways. The geothermal energy generated supplies power and heat to its greenhouses, swimming pools, and other facilities. In order to produce the power, a binary plant, that runs on the organic Rankine cycle, is used with a generating capacity of 680 kW. The plant runs on 165˚F (~73.9˚C) water meaning the geothermal power plant generates electricity at the lowest temperature in the world. The resort also has a 16-ton absorption chiller, which uses geothermal energy to keep their outdoor ice museum frozen all year round.
Including the Interior hot springs, there are two other active geothermal regions in Alaska – the Southeast hot springs and the “Ring of Fire” volcanoes. The Interior hot springs run from the Yukon Territory in Canada to the Seward Peninsula in Alaska. The “Ring of Fire” volcanoes include the Alaska Peninsula, Mount Edgecumbe, the Aleutians, and the Wrangell Mountains.
Currently, the Alaska Center for Energy and Power, or ACEP, is working with landowners, multiple utilities, and communities to assess resources and evaluate options for the development of geothermal energy in multiple parts of the state.
Did you know... there is a geyser on one of Saturn's moons?
And not just one, but over 100 huge water-vapor geysers occur at the south pole of Saturn’s moon Enceladus. They are believed to come from an ocean beneath the moon’s outer ice crust in which water comes to the surface through cracks in the ice that are called tiger stripes. Due to Enceladus’ tenuous atmosphere, the water vapor re-freezes and forms ice particles that fall back down to the moon’s surface, covering it in fresh ice that makes Enceladus the brightest object amongst all the planets.
More tantalizing is the scale of geysering. The plumes are the tallest known anywhere in the solar system, rising tens of kilometers above the surface of the moon. They are now known to be the source of Saturn’s E-ring, and the eruptions might be triggered by tidal forces. Remarkably, Enceladus is only about 500 km in diameter. The photographs from the Cassini mission from 2006 to 2017 have provided amazing insights about extraordinary geological activity on this small icy moon.
Geyser plumes on Enceladus (Courtesy NASA/JPL-Caltech). https://solarsystem.nasa.gov/resources/806/bursting-at-the-seams-the-geyser-basin-of-enceladus/
Enceladus geysers feed Saturn’s E-ring (Courtesy NASA/JPL-Caltech). https://www.jpl.nasa.gov/images/ghostly-fingers-of-enceladus
Did you know... Pamukkale is a travel HOT spot?
Pamukkale is a western Turkish town known for the mineral-rich thermal waters that cascade over steep, white terraces that reach over 100 meters (~330 feet) high. Across the terraces, there are a total of 17 hot springs, which range in temperature from 35-100 degrees Celsius (95-212 degrees Fahrenheit) year-round. The name in Turkish means “cotton castle” as it resembles the cotton plantations in central Turkey.
However, the white terraces are not cotton – they’re travertine rock! Travertine is a form of limestone that is deposited over time by mineral waters, most commonly, hot springs. The mass of hot springs sources in the area produces high amounts of calcium carbonate in the water so when the water hits the open air, it becomes white travertine rock.
Before it was Pamukkale, the site used to be the lively Greco-Roman city Hierapolis. Hierapolis was a spa city founded in 190 BC. Just like today, it was one of Turkey’s most popular hot springs. The ruins of the city are well preserved and hold what is known as Cleopatra’s pool, who is said to have bathed there, along with many other historically famous people.
The hot springs are open to the public to swim and relax in, and they have been known to be great for healing.
Did you know... that Paris has used geothermal energy to heat the homes of more than 2 million people?
You might not think that Paris, the city of love, would be a major producer of geothermal energy – but it is! Paris has been using geothermal energy to heat houses since 1969.
Under the famous city are two deep aquifers containing hot water. Since 1969, Paris has been working on many geothermal projects. Today, there are around fifty supply networks in the city that heat almost 250,000 homes.
The main aquifer, the Dogger, is about 1,500-2,000 meters (~4,900-6,600 feet) deep. The rock that hosts the aquifer is 150-170 million years old and is made of limestone. It has a temperature of about 60 degrees Celsius. While the Dogger is full of mineral salts that make produced water unfit for consumption, the heat can be used for district heating. This geothermal resource supplies energy to buildings in the northern, eastern, and southern parts of Paris, but to the west it falls below a threshold temperature that makes drilling and production uneconomic.
Currently, SIPPEREC (the Paris intercommunal union for energy and communication networks) is exploring the idea of drilling into the Triassic rock layer, which underlies the Dogger at 2,100 meters (~6,870 feet) depth. The temperature of the water at this level is about 80 degrees Celsius – 20 degrees higher than the Dogger. If successful, utilizing the Triassic layer would allow development in the western part of the Paris region but full-scale exploration awaits approval from regulatory authorities and the state.
As of 2020, drilling into the Dogger costs about 5 million euros per well. Of course, drilling deeper costs more, and the cost of drilling into the Triassic layer is about 9 million euros per well. However, because of the hotter water temperature, production here could be cheaper as less water would be required. SIPPEREC says that network users' charge could be lowered as well.
The new heating networks are scheduled for completion in November of this year with the benefit of conserving annual emissions of 30,000 tonnes of CO2.
Did you know... geothermal wells can be highly deviated too?
Just as in the oil industry, the first geothermal wells were all vertical, which remains common practice mainly because it is cost-effective. The maximum depth is typically about 10,000 feet (3 km). Deviated geothermal wells have been drilled too, extending laterally over horizontal distances up to about 5,000 feet (1.5 km) and dipping at angles of less than 45° as measured from the vertical. In most geothermal fields, the rock formations are made up of volcanic and sedimentary rocks.
New groundbreaking developments are now happening in the geothermal industry borrowing methods used for unconventional hydrocarbon development. Recently, a well having a long horizontal leg was drilled for the DEEP geothermal project in the Williston Basin, Saskatchewan, Canada.
The type of rocks being drilled into for geothermal development are relevant because up until now very few have reservoirs hosted by granitic rock, which is abrasive and hard on wear and tear of downhole equipment. Examples of such wells include 14-2 at Roosevelt Hot Springs, WD-1A at Kakkonda, Habanero 1 in the Cooper Basin, 33A-7 at Coso and OTN-3 in Finland. Of these, WD-1A has the hottest bottom hole temperature (~500°C), and OTN-3 is the deepest, but for this rock type, highly deviated wells are absent.
The new deep well at Utah FORGE, 16A(78)-32 is thus notable. It shows that the drilling of sub-horizontal well trajectories in granitoid are achievable. Such highly deviated wells are required for EGS wells in order to intersect a large number of sub-vertical fractures and to maximize energy production.
Figure showing the geothermal well profiles, host rocks and deviation angles: conventional wells in red; sedimentary basin wells in green (Saskatchewan, Canada; Groß Schönebeck, Germany); metamorphic-plutonic well in blue (Helsinki, Finland); granitoid wells in black (Roosevelt Hot Springs, Utah; Kakkonda, Japan; Cooper Basin, Australia; Soultz-sous-Forêts, France; Coso, California); granitoid well in pink (Utah FORGE).
Ayling et al. 2016, Geothermics 63, 15-26. https://www.sciencedirect.com/science/article/pii/S0375650515000395
Kwiatek et al. 2019, Science Advances,5 (https://advances.sciencemag.org/content/5/5/eaav7224)
Ledésert & Hébert 2012, Heat Exchangers - Basics Design Applications, 447-504, https://doi.org/10.5772/34276
Muraoka et al. 1998, Geothermics, 27:507-535. https://www.sciencedirect.com/science/article/pii/S0375650598000315
Sabin et al 2016, Proceedings Stanford Geothermal Workshop (https://pangea.stanford.edu/ERE/pdf/IGAstandard/SGW/2016/Sabin.pdf)
Zimmerman et al. 2010, Geothermics, 39, 59-69 (https://www.sciencedirect.com/science/article/pii/S0375650509000674)
Did you know that the first wells were drilled over 2000 years ago?
Drilling is an ancient technology and it has long been used to explore for natural resources and to produce fluids such as water, brine, oil and gas that occur underground. The Chinese drilled shallow wells over 2000 years ago to produce brine. The first oil wells were drilled in the 1800s and up through the early 1900s, wells were vertical and limited to depths of a few hundred to a couple of thousand feet. By the 1970s, depth records were being broken starting with Bertha Rogers No. 1 which was drilled to over 31,000 feet (9.5 km) to explore for gas in the Anadarko basin, Oklahoma, USA. In 1979, the Kola Superdeep scientific well in Russia was drilled to over 40,000 feet (12.2 km), making it the deepest well in the world. In 2009, the deepest oil well was completed to 35,000 feet (10.6 km) from the Deepwater Horizon platform in the Gulf of Mexico.
The idea of drilling a slanted deviated well by directional drilling was realized in the 1930s. Today, the drilling of highly deviated wells is commonplace in the exploration and production of oil and gas reservoirs. The Chayvo oil field in Russia is the site of several record-breaking deviated wells that are drilled to depths of about 3,000 feet (0.9 km) with a long horizontal reach exceeding 40,000 feet, the longest of which is O-14. For comparison, geothermal wells are generally drilled to no more than 10,000 feet (3 km), and if deviated, they are done so at modest angles of less than 45°.
There are several reasons for drilling deviated wells such as increasing the section or length of well interval through rocks that are rich in oil (or gas). In some cases, there are obstacles (e.g., town or lake), which means the resource has to be accessed from the side rather than vertically from the surface. In other cases, there are logistical advantages to clustering a number of deviated wells on a single pad as is common in offshore oil platforms.
Figure shows the depth ranges of the deepest and longest wells in comparison to wells that are commonly drilled in geothermal production fields.
Did you know… that Reykjavík is a city of geothermal energy?
Did you know that the city of Reykjavík, the capital of Iceland, is widely recognized for its geothermal energy? Many first think of the word ‘ice’ when hearing Iceland, but surprisingly Iceland is also known for its use of Earth’s heat. Due to its geological location directly on the mid-Atlantic ridge, it is constantly supplied by an enormous amount of underground magmatic and geothermal heat. The literal translation of Reykjavík is “steamy bay” that comes from the steam discharge associated with natural geothermal activity.
Aware of the underground heat available, Icelanders have learned to adapt to their environment. Since the arrival of the first Scandinavian settlers in the late 800s, Icelanders have utilized geothermal sources for bathing and cooking. One of their popular traditional foods, Hverabrauð, is a bread loaf cooked in the steam from a geyser for 24 hours. Up into the early part of the 20th century, coal was the main source of energy and air pollution was a serious problem. To address this, the first geothermal pipelines were installed in 1934, and since then Reykjavík has been continuously expanding geothermal utilization. Reykjavík now has the largest district heating system in the world (700 MWthermal), which is run by Orkuveita, and more than 60 million cubic meters of hot water flow through the distribution system. Hot water supply comes from low temperature geothermal areas around Reykjavik and from high temperature geothermal fields in the Hengill area to the east of the city. These hotter resources are mainly used to generate electricity, but a significant amount of heat also supplies the district heating scheme. The combination of geothermal fields and hydroelectric dams means that more than 99% of all the electricity used in Iceland comes from renewable sources.
Did you know that some species incubate their eggs using geothermal heat?
Megapodes represent a family of birds that are also known as incubator birds. They are found across Australasia, and they are known for their unique strategies to keep their eggs warm and safe. Depending on the local environment, incubating strategies range from building a massive nest with stacks of decaying vegetation to laying eggs in warm ground heated by the sun. Certain species of megapode occurring on volcanic islands in the Bismarck archipelago, Solomon Islands, Vanuatu, Tonga, and Micronesia bury and incubate their eggs in geothermally heated ground. Megapodes originated in Australia, and as they evolved, they spread northward and eastward to tropical islands of the southwest Pacific. The use of thermal ground by just a few species of Megapode to incubate eggs appears to be simply a matter of opportunity.
The incubation of eggs in thermal ground, however, is not just for the birds. Their ancient ancestors, dinosaurs, may have been similarly opportunistic. The recently discovered Sangasta nesting site in northwest Argentina provides definitive evidence that neosaupods used geothermally heated ground to incubate their eggs. Much like humans, some animals have used geothermal heat when and where it is easily available.
Grellet-Tinner, G. and Fiorelli, L.E., 2010, A new Argentinian nesting site showing neosauropod dinosaur reproduction in a Cretaceous hydrothermal environment: Nature Communications, 1:32, DOI: 10.1038/ncomms1031
Harris, R.B., Birks, S.M. and Leaché, A.D., 2014, Incubator birds: biogeographical origins and evolution of underground nesting megapodes (Galliformes: Megapodiidae): Journal of Biogeography, v. 41, p. 2045-2056.
Geothermal energy has great benefits for people, but did you know that there are animals that use natural thermal heat in the form of hot springs and warm ground?
Macaques, better known as snow monkeys, are found throughout the main Japanese Island of Honshu, and they are famous for soaking in local volcanic hot springs. Their bathing habit is a recent phenomenon that was first observed at Korakukan Onsen, a local guest house, in 1962. Snow monkeys seem to have adapted this habit from observing humans in the hot springs. Since then, this behavior has been passed onto rest of their troops, and it has now become a part of their daily routine. Snow monkeys bathe in hot springs to preserve body heat to survive the cold and rigid winters, but recent studies have proven they also do this as a form of stress relief.
Matsuzawa, T., 2918, Hot-spring bathing wild monkeys in Shiga-Heights: origin and propagation of a cultural behavior: Primates, v. 59, p. 209-213.
Takeshita, R.S.C., Bercovitch, F.B., Kinoshita, K. and Huffman, M.A., 2018, Beneficial effect of hot spring bathing on stress levels in Japanese macaques: Primates, v. 59, p. 215-225.