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The shape of a volcanic cone is influenced by several factors, including the viscosity of the magma, the type of volcanic eruption, and the composition of the erupting materials. Viscous magma tends to produce steeper, more conical shapes, as it accumulates around the vent, leading to stratovolcanoes. In contrast, low-viscosity magma results in broader, gently sloping shield volcanoes due to the fluid lava spreading over larger areas. Additionally, the presence of pyroclastic materials and the frequency of eruptions can also affect the cone's overall morphology.

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