A tube-shaped structure carved by magma is called a "dike." Dikes form when magma intrudes into existing fractures in the surrounding rock and solidifies, creating a vertical or near-vertical wall of igneous rock. Alternatively, if magma fills a space and solidifies in a horizontal manner, it is referred to as a "sill." These geological formations are important for understanding volcanic activity and the movement of magma within the Earth's crust.
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