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Here are a few properties of Basaltic Magma:

  • It is runny (less viscous) when compared to felsic magma
  • It contains Mafic minerals, or the ingredients of mafic minerals
  • It occurs largely at a divergent boundary between two oceanic plates and is the result of the melting of oceanic lithosphere
  • It rarely occurs at a convergent plate boundary between continental and oceanic crust

These things are commonly conceived as true, though there are likely to be exceptions (as mineralogy in rocks of the same type can still vary: even to a reasonably large extent).

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13y ago

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