The landform typically associated with volcanoes is a volcanic cone. This structure is formed by the accumulation of volcanic materials, such as lava, ash, and tephra, ejecting during eruptions. Over time, these materials build up to create a mound or hill-like shape, often with a crater at the summit. There are several types of volcanic cones, including cinder cones, composite cones (stratovolcanoes), and shield volcanoes, each with distinct characteristics based on their eruption style and the materials involved. Volcanic cones are crucial in understanding volcanic activity and the geological processes shaping our planet.