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Duration: 8 hours
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Explore Volcanoes
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Explore Coatepeque Caldera, El Salvador
Coatepeque De Coatepeque ("at the snake hill") is a volcanic caldera in El Salvador in Central America. The caldera was formed during a series of major rhyolitic explosive eruptions between about 72,000 and 57,000 years ago. Since then, basaltic cinder cones and lava flows formed near the west edge of the caldera, and six rhyodacitic lava domes have formed. The younge... -
Explore Corcovado National Park (Chile)
Corcovado National Park is an 726,000-acre (2,940 km2) preserved area of Valdivian temperate rainforest, high peaks, alpine lakes, and rivers in Chile's Los Lagos Region. This coastal park borders the same name to the west and includes the iconic volcanoes Corcovado and Yanteles. This preserved area has no public access infrastructure. This wilderness park of approxim... -
Explore Cosigüina Volcano Natural Reserve, Nicaragua
Cosigüina (also spelt Cosegüina) is a stratovolcano located in the western part of Nicaragua. It forms a large peninsula extending into the Gulf of Fonseca. The summit is truncated by a large caldera, 2 x 2.4 km in diameter and 500 m deep, holding a substantial crater lake (Laguna Cosigüina). This cone has grown within an earlier caldera, forming a somm... -
Explore Coso Volcanic Field, California
The Coso Volcanic Field is located in Inyo County, California, at the western edge of the Basin and Range geologic province and northern region of the Mojave Desert. The Fossil Falls are part of the Coso Field, created by the prehistoric Owens River. They are within the Naval Air Weapons Station China Lake and northeast of Little Lake and U.S. Route 395. Initiation o... -
Explore Cotopaxi Volcano, Ecuador
Cotopaxi is a stratovolcano in the Andes Mountains, located about 28 km (17 mi) south of Quito, Ecuador, South America. It is the second highest summit in the country, reaching a height of 5,897 m (19,347 ft) Cotopaxi has an almost symmetrical cone that rises from a highland plain of about 3,800 metres (12,500 ft), with a width at its base of about 23 kilometres (14 m... -
Explore Crater Highlands (Ngorongoro Volcanic Highlands) of Tanzania
The Crater Highlands or Ngorongoro Volcanic Highlands (Milima kasoko ya Ngorongoro, in Swahili) are a geological region along the East African Rift in the Arusha Region and parts of northern Manyara Region in north Tanzania. The Crater Highlands, are made up of several large volcanic complexes, including the 2.4-2.2 Ma Lemagarut and 2.25-2.0 Ma Ngorongoro basalt-trach... -
Explore Crater Lake National Park, Oregon
Crater Lake National Park is a United States National Park located in southern Oregon, whose primary feature is Crater Lake. This National Park was established on May 22, 1902, and it is the sixth oldest National Park in the U.S. This park encompasses the Crater Lake caldera, which rests in the remains of a destroyed volcano (eventually named Mount Mazama) and the sur... -
Summit Crater Mountain (Mono Craters), California
The Mono Craters are a 10.5-mile (17 km) chain of at least 27 volcanic domes, three large glass flows called coulees and various explosion pits and other associated volcanic features.The domes of the chain lie on a roughly north–south-trending arc that is concave to the west and located south of Mono Lake. The highest of the Mono Craters domes is Crater Mountain... -
Explore Craters of Laki, Iceland
Laki or Lakagígar (Craters of Laki) is a volcanic fissure in the south of Iceland, not far from the canyon of Eldgjá and the small village Kirkjubæjarklaustur. Lakagígar is the correct name, as Laki mountain itself did not erupt, but fissures opened up on each side of it. Lakagígar is part of a volcanic system centered on the Gr&iacut... -
Explore Craters of the Moon National Monument, Idaho
Craters of the Moon National Monument and Preserve is a national monument and national preserve located in the Snake River Plain in central Idaho, U.S.A. It is along US 20 (concurrent with US 93 & US 26), between the small cities of Arco and Carey, at an average elevation of 5,900 feet (1,800 m) above sea level. The protected area's features are volcanic and repre... -
Hike Cueva del Viento Lava Tube, Canary Islands
Cueva del Viento-Sobrado (Wind Cave) underground complex is the largest lava tube in the European Union and one of the largest in the world. It is the fifth largest in the world behind a series of caves in Hawaii. It was created by lava flows from Pico Viejo, next to Mt. Teide. The cave is located in the town of Icod de los Vinos in the north of the island of Tenerife... -
Explore Daisetsuzan National Park, Japan
Daisetsuzan National Park, or Taisetsuzan is located in the mountainous center of the northern Japanese island of Hokkaidō. At 2267.64 square kilometers, Daisetsuzan is the largest national park in Japan. The name means "Great Snowy Mountain(s)", an apt description of these peaks — there are 16 peaks over 2000 meters with trails and many more without trails &mda... -
See Daphne Island, Galápagos Islands
Daphne Major is a volcanic island just north of Santa Cruz Island and just west of the Baltra Airport in the Archipelago of Colón, commonly known as the Galápagos Islands. It consists of a tuff crater, devoid of trees, whose rim rises 120 m (394 ft) above the sea. Though easily accessible to most visitors to the Galápagos, the national park servic... -
Visit Devils Throat, Volcanoes National Park, Hawaii
The Devils Throat is a small volcanic pit crater located on the slopes of Kīlauea in Hawaii Volcanoes National Park.It formed in 1912 and is over 165 feet deep and 160 feet in diameter. It is located 150 feet off the Chain of Craters Road at the Hilina Pali Road turn off. -
Explore Diamond Craters, Burns, Oregon
The Diamond Craters is a monogenetic volcanic field about 40 miles (64 km) southeast of Burns, Oregon. The field consists of a 27-square-mile (70 km2) area of basaltic lava flows, cinder cones, and maars. The reexamination of radiocarbon dates from older studies and interpretation of paleomagnetic data and new radiocarbon dates limits the eruption of volca...
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