What causes a phreatic eruption?
A phreatic eruption happens when extreme heat from magma vaporizes ground water or surface water almost instantly. This sudden steam-blast sends out explosions of water, ash, rock, and gas, usually without including liquid lava. These steam explosions can precede larger volcanic events or create broad, low-relief craters known as maars.
What we know
- Phreatic eruptions occur when magma heats ground water or surface water, causing near-instantaneous evaporation. [2]
- The extreme temperature of magma causing these explosions ranges from 500 to 1,170 degrees Celsius, and volcanologists also categorize related steam-blast events under terms like ultravulcanian eruptions. [1, 2]
- Volcanologists classify an event as phreatomagmatic if molten magma is included in the ejected fragments. [2]
- Phreatic explosions can release toxic emissions such as carbon dioxide and hydrogen sulfide gases. [2]
Where to go next
- compared withWhat happens during a phreatomagmatic eruption?
- what followedHow do maars form from steam explosions?
- what caused itWhat triggers a Plinian volcanic eruption?
- whereHow is Mount Mayon's volcanic activity monitored?
- a case in pointWhat was the Oruanui supereruption?
- an unexpected connectionHow can a steam explosion release deadly poisons?While steam and rock are the expected output of water hitting magma, these explosions can also emit lethal concentrations of carbon dioxide and hydrogen sulfide.
Sources
- [1]phreatic eruption (Wikidata Q1067217) · CC0 1.0
- [2]Phreatic eruption · CC BY-SA 4.0
- [3]Mayon · CC BY-SA 4.0
- [4]Oruanui eruption · CC BY-SA 4.0
- [5]Plinian eruption · CC BY-SA 4.0