The geography term for a flat-topped mountain is a table mountain. These unique geological formations feature steep sides and a relatively flat summit, often rising sharply from the surrounding landscape. Table mountains are typically formed through processes like erosion and volcanic activity. They are prominent features in many geographical regions and can host diverse ecosystems, containing unique flora and fauna. Notable examples include Table Mountain in South Africa and the distinctive mesas found in the southwestern United States. These landscapes are often popular tourist destinations and provide important habitats.