Fissures and conduits are both geological features that facilitate the movement of fluids, such as magma or water, within the Earth's crust. They often form as a result of tectonic activity, where cracks or channels develop due to pressure changes or volcanic processes. Both can influence the formation of landforms and impact volcanic eruptions by providing pathways for the release of materials. Ultimately, they share the common function of serving as conduits for the transport of various substances within geological systems.
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