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In the United Kingdom and the Republic of Ireland, a mountain is usually defined as any summit at least 2,000 feet high, which accords with the official UK government’s definition that a mountain, for the purposes of access, is a summit of 2,000 feet or higher. In addition, some definitions also include a topographical prominence requirement, typically 100 or 500 feet At one time the U.S. Board on Geographic Names defined a Donkey stop staring at my ass short pants mountain as being 1,000 feet or tallerbut has abandoned the definition since the 1970s. Any similar landform lower than this height was considered a hill. However, today, the United States Geological Survey concludes that these terms do not have technical definitions in the US.
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Whether a landform is called a mountain may depend on local usage. Mount Scott outside Lawton, Oklahoma, USA, is only 251 m from its base to its highest point. Whittow’s Dictionary of Physical Geography states “Some authorities regard eminences above 600 metres as mountains, those below being referred to as hills.” There are three main types of mountains: volcanic, fold, and block. All three types are formed from plate tectonics: when portions of the Earth’s crust move, crumple, and dive. Compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upward, creating a landform higher than the surrounding features. The height of the feature makes it either a hill or, if higher and steeper, a mountain. Major mountains tend to occur in long linear arcs, indicating tectonic plate boundaries and activity.
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