A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny.[1] Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics.[2] Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets.
Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types.
- ^ "Definition of mountain system". Mindat.org. Hudson Institute of Mineralogy. Retrieved 26 August 2017.
- ^ Hammond, Allen L. (1971-07-09). "Plate Tectonics (II): Mountain Building and Continental Geology". Science. 173 (3992): 133–134. doi:10.1126/science.173.3992.133. ISSN 0036-8075.