Highland (geography) in the context of "Bugulma-Belebey Upland"

⭐ In the context of the Bugulma-Belebey Upland, a highland geography feature, what significant hydrological role does it play in the surrounding region?

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⭐ Core Definition: Highland (geography)

Highlands or uplands are areas of high elevation such as a mountainous region, elevated mountainous plateau or high hills. Generally, upland refers to a range of hills, typically from 300 m (980 ft) up to 600 m (2,000 ft), while highland is usually reserved for ranges of low mountains. However, the two terms are interchangeable and also include regions that are transitional between hilly and mountainous terrain.

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👉 Highland (geography) in the context of Bugulma-Belebey Upland

Bugulma-Belebey Upland (Russian: Бугульминско-Белебеевская возвышенность; Bashkir: Бөгөлмә-Бәләбәй ҡалҡыулығы; Tatar: Бөгелмә-Бәләбәй калкулыгы) is an upland in the eastern part of Eastern European Plain, west of the Urals, in Tatarstan, Bashkortostan and Orenburg Oblast, Russia. It forms the drainage divide of the Volga, Kama and Belaya rivers. The upper point of the upland is 418 m height. Romashkino field is placed there.

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Highland (geography) in the context of Central Russian Upland

The Central Russian Upland (also: Middle Russian Upland (Russian: Среднерусская возвышенность, romanizedSrednerusskaya vozvyshennost') and East European Upland) is an upland area of the East European Plain and is an undulating plateau with an average elevation of 230–250 m (750–820 ft). Its highest peak is measured at 293 m (961 ft). The southeastern portion of the upland known as the Kalach Upland [ru]. The Central Upland is built of Precambrian deposits of the crystalline Voronezh Massif.

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Highland (geography) in the context of Rímac River

The Rímac River [ˈri.mak] is located in western Peru and is the most important source of potable water for the Lima and Callao Metropolitan Area. It belongs to the Pacific Slope, into which it flows after bathing the cities of Lima and Callao, together with the Chillón River, to the north, and the Lurín River, to the south. It is 204 km long and has a basin of 3,312 km², of which 2,237.2 km² is a humid basin. The basin has a total of 191 lagoons, of which only 89 have been studied. The river begins in the highlands of the Huarochirí Province in the Lima Region and its mouth is located in Callao, near Jorge Chávez International Airport.

The river runs through the Rímac Valley (Spanish: Valle del Rímac), one of three valleys in the city of Lima. The city of Lima is located on the delta-shaped valley, as are various towns such as Matucana, Ricardo Palma, Chosica, Chaclacayo and Vitarte, small cities that function as strategic points between the coast and central mountains of Peru. It has a total surface of 3,700 km.

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Highland (geography) in the context of Intermontane

Intermontane is a physiographic adjective formed from the prefix "inter-" (signifying among, between, amid, during, within, mutual, reciprocal) and the adjective "montane" (inhabiting, or growing in mountainous regions, especially cool, moist upland slopes below the timberline).

The corresponding physiographic noun is intermountain, while the noun intermontane is an ecologic noun meaning among, between, amid, or within "flora and fauna of a montane habitat." As an example, an alpine region would be an intermontane for a species that migrates between a glacial region and a subalpine region.

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Highland (geography) in the context of Hill farming

Hill farming or terrace farming is an extensive farming in upland areas, primarily rearing sheep, although historically cattle were often reared extensively in upland areas. Fell farming is the farming of fells, a fell being an area of uncultivated high ground used as common grazing. It is a term commonly used in Northern England, especially in the Lake District and the Pennine Dales. Elsewhere, the terms hill farming or pastoral farming are more commonly used.

Cattle farming in the hills is usually restricted by a scarcity of winter fodder, and hill sheep, grazing at about two hectares per head, are often taken to lowland areas for fattening.

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Highland (geography) in the context of Moorland

Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and the biomes of montane grasslands and shrublands, characterised by low-growing vegetation on acidic soils. Moorland today generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on the exact distinction between these types of vegetation. Generally, moor refers to highland and high rainfall areas, while heath refers to lowland zones which are more likely to be the result of human activity.

Moorland habitats are found mainly in tropical Africa, northern and western Europe, and South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland is also related to tundra (where the subsoil is permafrost or permanently frozen soil), appearing as the tundra and the natural tree zone. The boundary between tundra and moorland constantly shifts with climatic change.

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Highland (geography) in the context of Cape Breton Highlands

The Cape Breton Highlands (French: Plateau du Cap-Breton, Scottish Gaelic: Àrd-thalamh Cheap Bhreatainn), commonly called the Highlands, refer to a highland or mountainous plateau across the northern part of Cape Breton Island in the Canadian province of Nova Scotia.

Considered a subrange of the Appalachian mountain chain, the Highlands comprise the northern portions of Inverness and Victoria Counties.

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Highland (geography) in the context of Silesian Upland

Silesian Upland or Silesian Highland (Polish: Wyżyna Śląska) is a highland located in Silesia and Lesser Poland, Poland.

Its highest point is the St. Anne Mountain (406 m).

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Highland (geography) in the context of Norfolk and Suffolk Broads Act 1988

The Norfolk and Suffolk Broads Act 1988 is an Act of the Parliament of the United Kingdom which created the Broads Authority. It is the framework for the creation of Broads, an area qualifying for special conservation on account of its ecological value and giving the Broads a similar status, in part, and funding to the national parks of England and Wales.

The first ten British national parks were designated as such in the 1950s under the National Parks and Access to the Countryside Act 1949 in mostly poor-quality agricultural upland and designations subsequent to the Broads are also under the auspices of the 1949 Act. The Broads required separate legislation to give special consideration to the needs of navigation. The Act requires the Broads Authority to take account of the area's national importance and the need to protect it. It must promote public enjoyment, preserve natural amenity and maintain, improve and develop the navigation area.

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