Without access to the specific diagram B you mentioned, I can provide a general answer. If the diagram illustrates a shield volcano, it forms primarily from the eruption of low-viscosity basaltic lava that flows over long distances, creating a broad, gently sloping profile. Over time, repeated eruptions build up the volcano's layers, resulting in its characteristic shape. If the diagram depicts a stratovolcano, it forms through alternating layers of lava flow and explosive volcanic ash, creating a steeper, conical structure.
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