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Caldera structure is similar on all of these planetary bodies, though the size varies considerably. The average caldera diameter on Venus is 68 km (42 mi). The average caldera diameter on Io is close to 40 km (25 mi), and the mode is 6 km (3.7 mi); Tvashtar Paterae is likely the largest caldera with a diameter of 290 km (180 mi). The average ...
Santorini caldera is a large, mostly submerged caldera, located in the southern Aegean Sea, 120 kilometers north of Crete in Greece.Visible above water is the circular Santorini island group, consisting of Santorini (classic Greek Thera), the main island, Therasia and Aspronisi at the periphery, and the Kameni islands at the center.
The Yellowstone Caldera is a resurgent caldera and has experienced resurgent doming. [8] The Yellowstone Caldera has two resurgent domes formed by magma upwelling called Sour Creek and Mallard Lakes. [8] The magma chambers under the Yellowstone Caldera provides heat and energy for large hydrothermal systems.
An estimated 400 acres of the caldera floor was covered in lava by 5:30 a.m., according to the Hawaiian Volcano Observatory. ... Another view of the new eruption within the summit caldera of ...
Clockwise from top: Partial panoramic view of Santorini, sunset in the village of Oia, ruins of the Stoa Basilica at Ancient Thera, the Orthodox Metropolitan Cathedral of Ypapanti (it) Cattedrale della Presentazione di Cristo (Fira) at the town of Fira, the Aegean Sea as seen from Oia, and view of Fira from the island of Nea Kameni at the Santorini caldera.
Valles Caldera is the younger of two calderas known at this location, having collapsed over and buried the older Toledo Caldera, which in turn may have collapsed over yet older calderas. The associated Cerros del Rio volcanic field , which forms the eastern Pajarito Plateau and the Caja del Rio , is older than the Toledo Caldera.
Krafla (Icelandic pronunciation: ⓘ) is a volcanic caldera of about 10 km (6.2 mi) in diameter with a 90 km (56 mi) long fissure zone. It is located in the north of Iceland in the Mývatn region and is situated on the Iceland hotspot atop the Mid-Atlantic Ridge, which forms the divergent boundary between the North American Plate and the Eurasian Plate. [1]
View of Koʻolau Range from the top of the ridge, facing northwest. The large town of Kāneʻohe is visible in the center of the photo, located on the narrow coastal plain paralleling the range. The volcano is thought to have first erupted on the ocean floor more than 2.5 million years ago.