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]

This lava flow erupted from a fissure vent in El Salvador

References change

↑ "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.

This short article about science can be made longer. You can help Wikipedia by adding to it.

[1] "Fissure Vent Volcano". Bioexpedition. Retrieved 28 March 2015.

[2] Studies in Volcanology: The Legacy of George Walker, ed. Thor Thordarson (London: Geological Society, 2009), p. 299

[3] "Fissure Vents". Smithsonian Institution. Archived from the original on 17 February 2015. Retrieved 28 March 2015.

[1]

[2]

[3]