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The Coulees are somewhere between a lava dome and a lava flow. This type of dome usually takes place on the side of a slope and that is why it can run down.
It is rare for this type of dome to be very large but there are a few examples which are over 10 kilometers. Finally you will be able to find what is called an Upheaved Plug which is a very interesting and very rare type of dome.
The lava when it erupts tends to be stronger than that of other domes and because of that the lava is pushed up, almost like a piston. These extrusions can travel very high when compared to the surface.
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Characteristics of lava dome eruptions include shallow, long-period and hybrid seismicity , which is attributed to excess fluid pressures in the contributing vent chamber.
Other characteristics of lava domes include their hemispherical dome shape, cycles of dome growth over long periods, and sudden onsets of violent explosive activity.
Gravitational collapse of a lava dome can produce a block and ash flow. Helens , where the explosive eruption began after a landslide caused the side of the volcano to fall, leading to explosive decompression of the subterranean cryptodome.
A lava spine or lava spire is a growth that can form on the top of a lava dome. A lava spine can increase the instability of the underlying lava dome.
This flow is over 14 kilometres 8. From Wikipedia, the free encyclopedia. Roughly circular protrusion from slowly extruded viscous volcanic lava. Main article: Lava spine.
Main article: List of lava domes. The Encyclopedia of Volcanoes. Journal of Geophysical Research. Bibcode : JGRE.. Earth and Planetary Science Letters.
