Santiaguito is a volcanic dome that formed as a result of the continuous extrusion of lava at the foot of the active stratovolcano, Santa María, in Guatemala. This dome is a classic example of a lava dome, characterized by its steep sides and relatively small size compared to larger stratovolcanoes. Its formation is primarily due to the accumulation of viscous lava that does not flow far from the vent, leading to a conical structure that often exhibits explosive activity.
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