| 1. | The solubility of water is higher in rhyolite than in basaltic magma.
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| 2. | Eruptions of basaltic magma often transition between effusive and explosive eruption patterns.
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| 3. | However early formed crystals in basaltic magma can also form harzburgite within the mantle.
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| 4. | Partial melting of spinel lherzolite is one of the primary sources of basaltic magma.
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| 5. | Basaltic magma rose along these fractures to create effusive eruptions.
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| 6. | Basaltic magma is formed from lherzolites in the mantle.
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| 7. | No non-basaltic magmas have been erupted at Longgang.
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| 8. | The multiple andesite flows were probably derived from basaltic magma by the crystallization of the magma material.
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| 9. | The second time, between 9 225 million years ago, started with basaltic magma eruptions, and ended with pyroclastic eruptions.
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| 10. | Water released from the subducting plate triggers the formation of basaltic magmas that are then injected into the crust.
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