5 earthquakes occurred near (under) the volcano during 8 hours, the last being recorded quake 9 hours ago. Hypocenter depths ranged between 36.00 and 2.00 km. 2.8 quake Philippine Sea, 5.5 km ...

Ibu is a 1,357 m-high stratovolcano on the northwestern coast of Halmahera, Indonesia. Its summit contains nested craters and a lava dome built during repeated explosive and effusive activity. The ...

Ksudach in Kamchatka, Russia, is distinguished by a complex of five calderas cut into a broad stratovolcano. Three of those calderas formed during approximately the past 12,000 years. A major eruption ...

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Sierra Negra is a broad, frequently active shield volcano at the southern end of Isabela Island in Ecuador's Galápagos archipelago. Its shallow caldera is the largest in the islands, and numerous ...

Two Holocene tuff rings form craters 300 and 66 m wide near the headwaters of Buzzard Creek at the northern foot of the central Alaska Range NE of the town of Healy along the Parks Highway. Both ...

Taal volcano with its lake-filled 15x20 km wide Talisay (Taal) caldera is a beautiful caldera volcano, but also one of the most active and dangerous volcanoes of the Philippines. Taal has had some of ...

Katla volcano, located near the southern end of Iceland's eastern volcanic zone, is hidden beneath the Myrdalsjökull icecap. Katla is one of Iceland's most active and most dangerous volcanoes, ...

Paka, also recorded as Pakka, is a shield volcano in Kenya's Gregory Rift. Its summit is marked by a 1.5-km-wide caldera, while cones, a dome, craters and lava flows record both explosive and effusive ...

Kasbek, also listed as Kazbek, is a 5,004 m glacier-covered stratovolcano in Georgia's Caucasus Mountains, just south of the Russian border. Its broad volcanic complex includes lava cones, domes and a ...

Alcedo is a shield volcano on Isabela Island in Ecuador's Galápagos archipelago. It stands out as the only Galápagos volcano known to have produced rhyolite as well as basalt. Its broad summit ...

Piparo mud volcano is located in the Naparima Fold Belt of the Central Range of Trinidad which is mostly composed of shale sediments up to 1000 m thick. The erupted mud forms an elongated E_W oriented ...