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Calderas

A caldera is a collapse feature typically found on the summits of large volcanoes. Calderas form when magma is removed from deep within a volcano due to a large eruption or intrusion. When the magma is suddenly removed the summit of the volcano becomes partially unsupported. The part of the volcano above the magma chamber then collapses downward, sliding along curved faults that bound the collapse region. At Axial Volcano, the caldera walls are up to 100 m high. The magma reservoir beneath Axial lies about 2-4 km below the summit. It is not clear whether Axial's caldera was caused by a sudden collapse during a particularly large eruption or by a series of smaller events over a longer period of time.

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Related panoramas:
Axial Seamount in QTVR | Axial caldera in QTVR

Other NeMO-related concepts:
Mid-ocean ridges | seafloor spreading | seamounts & hot spots | calderas | Axial volcano
Hydrothermal vents | fluid paths | focused vents | diffuse vents | sulfide | anhydrite
Animal Gallery | chemosynthesis | biological colonization of new lava

Lava morphology | sheets | pillows | lava contacts | skylights | pillars | the 1998 flow
NeMO at Axial | the 1998 eruption | the rumbleometer story | lava flow animation

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