Hill range in the context of "Namcha Barwa Himal"

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⭐ Core Definition: Hill range

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. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. 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.

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Hill range in the context of Hill chain

A hill chain, sometimes also hill ridge, is an elongated line of hills that usually includes a succession of more or less prominent hilltops, domed summits or kuppen, hill ridges and saddles and which, together with its associated lateral ridges and branches, may form a complex topographic structure. It may occur within a hill range, within an area of low rolling hill country or on a plain. It may link two or more otherwise distinct hill ranges. The transition from a hill chain to a mountain chain is blurred and depends on regional definitions of a hill or mountain. For example, in the UK and Ireland a mountain must officially be 600 m (2,000 ft) or higher, whereas in North America mountains are often (unofficially) taken as being 1,000 ft (300 m) high or more.

The chain-like arrangement of hills in a chain is a consequence of their collective formation by mountain building forces or ice age earth movements. Hill chains generally have a uniform geological age, but may comprise several types of rock or sediment.

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Hill range in the context of Margalla Hills

The Margalla Hills is a hill range of subtropical moist broadleaf forest ecoregion in the Indomalayan realm within the Margalla Hills National Park in the northwestern Punjab region in Pakistan, forming the northern edge of the Islamabad Capital Territory, just south of Haripur District, Khyber Pakhtunkhwa. They are part of the Himalayan foothills on the Himalayan biodiversity hotspot. The Margalla range has an area of 12,605 hectares. It is a range with many valleys and rainforests as well as high mountains.

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Hill range in the context of Kleiner Odenwald

The Kleiner Odenwald (“Little Odenwald”) is the southern part of the central German hill range, the Odenwald, and is up to 567.8 m above sea level (NHN). It is also part of the natural region of Sandstein-Odenwald in the north of the state of Baden-Württemberg. Lying east-southeast of Heidelberg and south of the River Neckar, which separates the Kleiner Odenwald from the rest of the Odenwald, its landscape is shaped by the underlying sandstone that also dominates the northern Odenwald.

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Hill range in the context of Wiehengebirge

The Wiehen Hills (German: Wiehengebirge, pronounced [ˈviːənɡəˌbɪʁɡə] , also locally, just Wiehen) are a hill range in North Rhine-Westphalia and Lower Saxony in Germany. The hills run from west to east like a long finger away from the main upland area of the Lower Saxon Hills, beginning at the Weser River near Minden and terminating in the vicinity of Osnabrück.It is the northernmost of the German Central Upland ranges extending into the Northern Lowlands.Their highest hill is the Heidbrink near Lübbecke with an altitude of 320 metres (1,050 ft).

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