magmatism
Sign in to savethumb|300px|Geological map showing the [[Gangdese batholith, which is a product of magmatic activity about 100 million years ago.]] Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks. It does so through magmatic activity or igneous activity, the production, intrusion and extrusion of magma or lava. Volcanism is the surface expression of magmatism.
Article
14 sectionsContents
- Convergent boundaries
- Subduction-related
- Collision-related
- Post-collision
- Divergent boundaries
- Mid-ocean ridges
- Back-arc basins
- Intraplate
- Hotspots
- Rifts
- Large igneous provinces
- Intruded v. extruded magma
- See also
- References
thumb|300px|Geological map showing the [[Gangdese batholith, which is a product of magmatic activity about 100 million years ago.]] Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks. It does so through magmatic activity or igneous activity, the production, intrusion and extrusion of magma or lava. Volcanism is the surface expression of magmatism.
Magmatism is one of the main processes responsible for mountain formation. The nature of magmatism depends on the tectonic setting. For example, andesitic magmatism is associated with the formation of island arcs at convergent plate boundaries while basaltic magmatism is found at mid-ocean ridges during sea-floor spreading at divergent plate boundaries.