They are typically steep-sided, symmetrical cones of large dimension built of alternating layers of lava flows, volcanic ash, cinders, blocks, and bombs and may rise as much as 8,000 feet above their bases. A conduit system through which magma from a reservoir deep in the Earth's crust rises to the surface and is built up by the accumulation of material erupted through the conduit and increases in size as lava, cinders, ash, etc. are added to its slopes.