RHYOLITIC MAGMA Rhyolitic magma is a silica-rich type of magma that typically contains over 70% silica (SiO₂). It is the volcanic equivalent of granite in composition. Because of its high silica content, rhyolitic magma is highly viscous, meaning it flows very slowly compared to basaltic or andesitic magmas. CHARACTERISTICS: Silica content: ~70–77% (very high). Viscosity: Very high, making it resistant to flow. Temperature: Relatively low, around 650–800°C. Gas content: Often rich in dissolved g
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