Fissure vent
A fissure vent, also known as a volcanic fissure or eruption fissure, is a kind of volcano through which lava erupts.[1] The crack is usually linear (follows a fairly straight line).[2] It is often a few meters wide and may be many kilometers long. Fissure vents can cause large flood of lava and later lava tubes. After some time the eruption cools down gradually and builds up craters.[3]
Fissure Vent Media
Channel of lava erupted during a fissure eruption of Kīlauea volcano, Hawaii, 2007
Eruption fissure with spatter cones, Holuhraun, Iceland, 2014
Mauna Loa with different lava flows and fissure vent
Foto gemaakt door Hans Oosting.
Eldhraun, a lava field produced by the Laki craters
Fissure on Etna during eruption of 1865
References
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- ↑ "Fissure Vent Volcano". Bioexpedition. Retrieved 28 March 2015.
- ↑ Studies in Volcanology: The Legacy of George Walker, ed. Thor Thordarson (London: Geological Society, 2009), p. 299
- ↑ "Fissure Vents". Smithsonian Institution. Archived from the original on 17 February 2015. Retrieved 28 March 2015.