However, it's important to note that this range can vary depending on:

* Composition: Magma with a higher silica content (felsic) tends to have lower melting points, while magma with a lower silica content (mafic) has higher melting points.

* Depth: Magma at greater depths experiences higher pressures, which increases its melting point.

* Presence of volatiles: Water and other volatiles lower the melting point of magma.

Here's a more specific breakdown:

* Felsic magma (granitic): 650°C to 850°C (1,202°F to 1,562°F)

* Intermediate magma (andesitic): 800°C to 1,000°C (1,472°F to 1,832°F)

* Mafic magma (basaltic): 1,000°C to 1,200°C (1,832°F to 2,192°F)

It's also worth noting that magma can become superheated, meaning its temperature is higher than its typical melting point. This can occur due to the presence of dissolved gases or other factors.

Overall, the temperature of magma is a complex factor influenced by its composition, depth, and other conditions.