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Avachinsky (also known as Avacha or Avacha Volcano or Avachinskaya Sopka) (Russian: Авачинская сопка, Авача) is an active stratovolcano on the Kamchatka Peninsula in the far east of Russia. It lies within sight of the capital of Kamchatka Krai, Petropavlovsk-Kamchatsky. Together with neighboring Koryaksky volcano, it has been designated a Decade Volcano, worthy of par...
The Banda Islands are a volcanic group of ten small volcanic islands in the Banda Sea, about 140 km (87 mi) south of Seram Island and about 2,000 km (1,243 mi) east of Java, and are part of the Indonesian province of Maluku. The main town and administrative centre is Bandanaira, located on the island of the same name. They rise out of 4–6 km deep ocean and have ...
Bárðarbunga, is a stratovolcano located under Vatnajökull, Iceland's most extensive glacier. The second highest mountain in Iceland, 2,009 metres (6,591 ft) above sea level, Bárðarbunga is also part of a volcanic system that is approximately 200 kilometres (120 mi) long and 25 kilometres (16 mi) wide.
Bárðarbunga is a subglacial s...
Bassin Blanc crater has been filled with water, it is a crater lake volcano. It is extinct. When it erupted long ago, it created the valleys of La Vallee des Couleurs Nature Park.
At a mere 1300 years old, the Big Obsidian Flow is the youngest lava flow in Oregon. A one-mile interpretive trail climbs up and onto this impressive lava flow of obsidian (black glass) and pumice. The Newberry Crater Trail also passes through this site, which connects to the Lost Lake Trail.
This is also the location of the Big Obsidian Flow Ampitheater wherer rang...
Bioko (spelled also Bioco, in Europe traditionally called Fernando Pó) is an island 32 km off the west coast of Africa, specifically Cameroon, in the Gulf of Guinea. It is the northernmost part of Equatorial Guinea with a population of 124,000 and an area of 2,017 km2 (779 sq mi). It is volcanic with its highest peak the Pico Basile at 3,012 m (9,882 ft).
Malab...
Black Butte is a stratovolcano (not a cinder cone) 5.5 miles (8.9 km) west of Sisters, Oregon in Deschutes National Forest.
Black Butte looks young, as it is barely eroded (except for little gullies a little bit above the base that were carved by long-gone streams). Mount Washington, which is visible from the summit of Black Butte, looks much more eroded, and older, t...
Black Crater is a shield volcano in the Western Cascades in Deschutes County, Oregon. Located near McKenzie Pass, the volcano has a broad conical shape with gentle slopes. The volcano likely formed during the Pleistocene and has not been active within the last 50,000 years. Eruptive activity at the volcano produced mafic lava flows made of basaltic andesite and olivin...
Bláhnjúkur is a volcano in the south of Iceland. Its height is about 940 m.
Its name translates toblue peakin English. This comes from the blue-black colour of its sides. The colour is due to volcanic ash and lava flows.
The mountain is situated in Landmannalaugar, a natural park near Hekla. It lies next to the volcano Brennisteinsalda.
A hiking trail le...
Poás Volcano National Park is a National Park that covers an area of approximately 16,000 acres (65 km²); the summit is 8,900 feet (2,708 m). One of the attractive features about Poás is that you can get all the way to the edge of the crater.
The main crater is 950 feet (289 m) deep and is quite active with frequent small geyser and lava eruptions, ...
Cabeço Gordo (Portuguese for "fat mountain") is the highest mountain, massive stratovolcano and the largest geomorphological structure that forms the island of Faial. The mountain/volcano is 1,043 meters above sea level, consisting of a two kilometer wide caldera, that is 400 m in depth below the crater rim. From Cabeço Gordo, on a clear day, the islands...
Flores has several inactive volcanoes and in many situations where water collected in volcanic calderas (or caldeiras in Portuguese), lakes formed: there are seven of these lakes on the island, including Caldeira Negra, Caldeira Comprida, Caldeira Seca and Caldeira Branca.
It's part of the UNESCO Azores Geopark.
The island is located on the North American Plate, west of the Mid-Atlantic Ridge on a sea-mount of approximately 1.5-1.0 million years age. The islands of Corvo and Flores emerged from a submarine mount oriented along a north-northeast to south-southwest line, while Corvo is controlled by faults oriented north to south, parallel to the mid-Atlantic Ridge, and transfo...
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