What is an effusive eruption?
An effusive eruption is a volcanic event where lava steadily flows out onto the ground rather than exploding violently. These eruptions are typically characterized by low-viscosity, high-temperature basaltic magmas with low gas content. Hawaiian eruptions are a common example of this style of volcanic activity.
What we know
- An effusive eruption is a type of volcanic eruption in which lava steadily flows out of a volcano onto the ground. [1, 2]
- Hawaiian eruptions are typically effusive eruptions featuring basaltic magmas of low viscosity, low gas content, and high temperature. [4]
- Effusive eruptions produce very small amounts of volcanic ash. [4]
Where to go next
- a case in pointWhat causes a Hawaiian eruption?
- the bigger pictureHow do volcanic eruptions differ in type?
- how it workedWhat is the Volcanic Explosivity Index?
- what caused itHow do basaltic magmas affect lava flow?
- whereWhich volcanoes are famous for effusive activity?
- an unexpected connectionHow do hotspot volcanoes create gentle lava flows?Hotspot volcanoes like Kīlauea are widely known for dramatic tectonic settings, yet they commonly produce gentle effusive eruptions with low-viscosity basalt.
Sources
- [1]effusive eruption (Wikidata Q1296340) · CC0 1.0
- [2]Effusive eruption · CC BY-SA 4.0
- [3]List of volcanic eruptions in the 21st century · CC BY-SA 4.0
- [4]Hawaiian eruption · CC BY-SA 4.0
- [5]Volcanic eruption · CC BY-SA 4.0