<p><img src="https://i.sstatic.net/3kQ2b.jpg" alt="Examples of Volcanism"></p>

<p>Most volcanism occurs at three major tectonic features: Subduction Zones, Rifting Centers (Like East Pacific Rise) and under hotspots. </p>

<p>I will start with the most contentious, hotspots. The clearest example of hotspot volcanism is the island chain Hawaii. Underneath the island, there is a chaotic discontinuity caused by the boundary conditions at the core-mantle boundary. This causes highly viscous and hot mantle to upwell rapidly and push through the lithosphere, forming a volcano. The orgin of hotspots is not well known, and it is even a debate if they exist (they do, imo). Some papers worth looking at are by Paul Hall (BU) and Christopher Kincaid(URI), and maybe Dave Stegman (Scripps) who publish on melting caused by mantle plumes.</p>

<p>As a consequence of a subducting slab, at a distance in front of the trench, Arc Volcanoes form. The distance in front of the trench is often thought to be where the overriding plate is 100-120km higher than the suducting slab. The cold, oceanic plate plunges underneath the continental plate in the image above, adding water to the mantle. This water lowers the melting temperature (solidus) of the mantle inside the wedge of the subduction zone, causing  partial melting (4-6%). This melt, more viscous and buoyant than the solid mantle, floats to tho the top of the mantle and eventually penetrates the lithosphere and forms a volcano. This <a href="https://earthscience.stackexchange.com/questions/144/why-is-there-a-line-of-volcanoes-along-the-northwest-coast-of-north-america?rq=1">question</a> is also relevant. </p>

<p>Finally, at divergent plate boundaries, the process is fairly straight forward. A break in the lithosphere caused by rifting plates allows the pressurized mantle to flow towards the opening. This causes and abundance of hot, fertile mantle which can be melted.  This melted mantle creeps through the lithosphere and forms ocean floor volcanoes (sometimes called smokers). </p>

CC BY-SA 3.0
2014-04-17T06:43:07.880Z
Another example of hotspot volcanism is Iceland, although due to different plate movement that doesn't consist of a chain of volcanoes. Hawaii probably is a good argument for the existence of mantle plumes, as that could explain the chain by moving the crust over the mantle plume, with the plume intermittently bursting through the crust to form a new island.
hugovdberg
CC BY-SA 3.0
2014-04-17T16:28:23.950Z
Bathymetry and gravity data is also very suggestive of a plume (or at least a shallow mantle hotspot) - same for Cape Verde/etc. Speaking generally, I have more of a problem with the assignment of all continental intra-plate volcanism to plumes. But that kind of debate is for elsewhere.
winwaed
CC BY-SA 3.0
2014-04-17T02:37:34.410Z
2014-04-17T02:37:34.410Z
2017-04-13T12:50:30.540Z
Neo
<p>Inspired by the question, <a href="https://earthscience.stackexchange.com/questions/57/what-causes-earthquakes">How does one measure what causes earthquakes?</a>, I'd like to know what causes another great geological phenomenon - volcanoes? </p>

CC BY-SA 3.0
2014-04-17T02:08:59.253Z
They are generally a consequence of plate tectonics, can be found here: http://en.wikipedia.org/wiki/Volcano
Neo
CC BY-SA 3.0
2014-04-17T14:14:52.550Z
I think this question is not off-topic or too broad, but it's a poor question because it doesn't show any evidence of prior research.
gerrit
<volcanology>
What causes a volcano?
Kenshin
# What causes a volcano?

(Asked by: username_0 on 2014-04-17)

Inspired by the question, [How does one measure what causes earthquakes?](https://earthscience.stackexchange.com/questions/57/what-causes-earthquakes), I'd like to know what causes another great geological phenomenon - volcanoes?

**Tags:** volcanology

> **Comments:**
> **username_1**: They are generally a consequence of plate tectonics, can be found here: http://en.wikipedia.org/wiki/Volcano  
> **username_2**: I think this question is not off-topic or too broad, but it's a poor question because it doesn't show any evidence of prior research.  

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## 1 answers

### Answer by username_1 on 2014-04-17. Score: 14 | Accepted answer

![Examples of Volcanism](https://i.sstatic.net/3kQ2b.jpg)

Most volcanism occurs at three major tectonic features: Subduction Zones, Rifting Centers (Like East Pacific Rise) and under hotspots.

I will start with the most contentious, hotspots. The clearest example of hotspot volcanism is the island chain Hawaii. Underneath the island, there is a chaotic discontinuity caused by the boundary conditions at the core-mantle boundary. This causes highly viscous and hot mantle to upwell rapidly and push through the lithosphere, forming a volcano. The orgin of hotspots is not well known, and it is even a debate if they exist (they do, imo). Some papers worth looking at are by Paul Hall (BU) and Christopher Kincaid(URI), and maybe Dave Stegman (Scripps) who publish on melting caused by mantle plumes.

As a consequence of a subducting slab, at a distance in front of the trench, Arc Volcanoes form. The distance in front of the trench is often thought to be where the overriding plate is 100-120km higher than the suducting slab. The cold, oceanic plate plunges underneath the continental plate in the image above, adding water to the mantle. This water lowers the melting temperature (solidus) of the mantle inside the wedge of the subduction zone, causing partial melting (4-6%). This melt, more viscous and buoyant than the solid mantle, floats to tho the top of the mantle and eventually penetrates the lithosphere and forms a volcano. This [question](https://earthscience.stackexchange.com/questions/144/why-is-there-a-line-of-volcanoes-along-the-northwest-coast-of-north-america?rq=1) is also relevant.

Finally, at divergent plate boundaries, the process is fairly straight forward. A break in the lithosphere caused by rifting plates allows the pressurized mantle to flow towards the opening. This causes and abundance of hot, fertile mantle which can be melted. This melted mantle creeps through the lithosphere and forms ocean floor volcanoes (sometimes called smokers).

> **Comments:**
> **username_3**: Another example of hotspot volcanism is Iceland, although due to different plate movement that doesn't consist of a chain of volcanoes. Hawaii probably is a good argument for the existence of mantle plumes, as that could explain the chain by moving the crust over the mantle plume, with the plume intermittently bursting through the crust to form a new island.  
> **username_4**: Bathymetry and gravity data is also very suggestive of a plume (or at least a shallow mantle hotspot) - same for Cape Verde/etc. Speaking generally, I have more of a problem with the assignment of all continental intra-plate volcanism to plumes. But that kind of debate is for elsewhere.  

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