Conical mountains are characterized by their steep, conical shape, resembling a pointed peak. These mountains typically form from volcanic activity, where lava accumulates around a vent, creating a symmetrical cone. Examples of conical mountains include Mount Fuji in Japan and Kilimanjaro in Tanzania. The formation of conical mountains often involves explosive eruptions, which can lead to the creation of a crater at the summit. Over time, erosion can shape these mountains, but their distinctive conical profile usually remains. They are often found in volcanic regions and can be significant landmarks in their respective areas.