Plateau in the context of Volcano


Plateau in the context of Volcano

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⭐ Core Definition: Plateau

In geology and physical geography, a plateau (/pləˈt, plæˈt, ˈplæt/; French: [plato]; pl.: plateaus or plateaux), also called a high plain or a tableland, is an area of highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones.

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Plateau in the context of East European Plain

The East European Plain (also called the Russian Plain, or historically the Sarmatic Plain) is a vast interior plain extending east of the North European Plain, and comprising several plateaus stretching roughly from 25 degrees longitude eastward. It includes Volhynian-Podolian Upland on its westernmost fringe, the Central Russian Upland, and, on the eastern border, encompasses the Volga Upland. The plain includes also a series of major river basins such as the Dnieper Lowland, the Oka–Don Lowland, and the Volga Basin. At the southeastern point of the East European Plain are the Caucasus and Crimean mountain ranges. Together with the North European Plain (covering much of Belgium, the Netherlands, Denmark, Germany and Poland), and covering the Baltic states (Estonia, Latvia and Lithuania), European Russia, Belarus, Ukraine, Moldova, southeastern Romania, and, at its southernmost point, the Danubian Plain in Northern Bulgaria (including Ludogorie and Southern Dobruja), it constitutes the majority of the Great European Plain (European Plain), the greatest mountain-free part of the European landscape. The plain spans approximately 4,000,000 km (2,000,000 sq mi) and averages about 170 m (560 ft) in elevation. The highest point of the plain (480 metres (1,574.8 ft)) is in the Bugulma-Belebey Upland, in the Eastern part of the plain, in the elevated area by the Ural Mountains (priyralie).

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Plateau in the context of Dobruja Plateau

The Dobruja Plateau or Dobrogea Plateau (Romanian: Podișul Dobrogei) is a plateau in eastern Romania located in the Dobruja (Romanian: Dobrogea) region, surrounded to the north and west by the Danube and to the east by the Danube Delta and the Black Sea.

Its average altitude is around 200–300 metres, higher in the northern part. The highest point is the Țuțuiatu/Greci Peak in the Măcin Mountains, at a height of 467 m.

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Plateau in the context of Kirchberg, Luxembourg

Kirchberg (German pronunciation: [ˈkɪʁçbɛʁk] ; Luxembourgish: Kierchbierg, pronounced [kiːɐ̯ɕˈbiːɐ̯ɕ] ; lit.'church hill') is a district in north-eastern Luxembourg City, in southern Luxembourg. It consists of a plateau overlooking the north-east of the historical city center, Ville Haute, connected to the rest of the elevated city by the Grand Duchess Charlotte Bridge, which spans the Pfaffenthal valley. It is often referred to, in reference to the geographical feature it inhabits, as the Kirchberg plateau by Luxembourgish residents. Kirchberg is the predominant location of the European Union institutions and bodies based within Luxembourg, and is sometimes used as a metonym for the EU's judiciary, which occupies the district. It is thus the central business district of Luxembourg.

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Plateau in the context of Armenian highland

The Armenian highlands (Armenian: Հայկական լեռնաշխարհ, romanizedHaykakan leṙnašxarh; also known as the Eastern Anatolian highlands, Armenian upland, Armenian plateau, or Armenian tableland) comprise the most central and the highest of the three plateaus that together form the northern sector of West Asia. Clockwise starting from the west, the Armenian highlands are bounded by the Anatolian plateau, the Caucasus, the Kura-Aras lowlands, the Iranian Plateau, and Mesopotamia. The highlands are divided into western and eastern regions, defined by the Ararat Valley where Mount Ararat is located. Since the turn of the 20th century, Western Armenia has been relabeled as "Eastern Anatolia" by Ottoman and Turkish authorities. Eastern Armenia is part of Lesser Caucasus, which was historically known by some as the Anti-Caucasus, meaning "opposite of the Caucasus".

During the Iron Age, the region was known by variations of the name Ararat (Urartu, Uruatri, Urashtu). Later, the Highlands were known as Armenia Major, a central region to the history of Armenians, and one of the four geopolitical regions associated with Armenians, the other three being Armenia Minor, Sophene, and Commagene. The highlands are primarily defined by the geographical dispersal of its native inhabitants, the Armenians. Prior to the appearance of nominally Armenian people in historical records, historians have hypothesized that the region must have been home to various ethnic groups who became homogenous when the Armenian language came to prominence. The population of the Armenian highlands has had a high level of regional genetic continuity for over 6,000 years. Recent studies indicate that the Armenian people descend from the indigenous people of the Armenian highlands and form a distinct genetic isolate in the region. The region was also inhabited during Antiquity by minorities such as Assyrians, Georgians, Greeks, Jews, and Iranians. During the Middle Ages, Arabs and particularly Turkmens and Kurds settled in large numbers in the Armenian highlands.

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Plateau in the context of Andes

The Andes (/ˈændz/ AN-deez), Andes Mountains or Andean Mountain Range (Spanish: Cordillera de los Andes; Quechua: Anti) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is 8,900 km (5,500 mi) long and 200 to 700 km (120 to 430 mi) wide (widest between 18°S and 20°S latitude) and has an average height of about 4,000 m (13,000 ft). The Andes extend from south to north through seven South American countries: Argentina, Chile, Bolivia, Peru, Ecuador, Colombia, and Venezuela.

Along their length, the Andes are split into several ranges, separated by intermediate depressions. The Andes are the location of several high plateaus—some of which host major cities such as Arequipa, Bogotá, Cali, Medellín, El Alto, La Paz, Mérida, Santiago and Sucre. The Altiplano Plateau is the world's second highest after the Tibetan Plateau. These ranges are in turn grouped into three major divisions based on climate: the Tropical Andes, the Dry Andes, and the Wet Andes.

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Plateau in the context of Mexico City

Mexico City is the capital and largest city of Mexico, as well as the most populous city in North America. It is one of the most important cultural and financial centers in the world, and is classified as an Alpha world city according to the Globalization and World Cities Research Network (GaWC) 2024 ranking. Mexico City is located in the Valley of Mexico within the high Mexican central plateau, at an altitude of 2,240 meters (7,350 ft). The city has 16 boroughs or demarcaciones territoriales, which are in turn divided into neighborhoods or colonias.

The 2020 population for the city proper was 9,209,944, with a land area of 1,495 square kilometers (577 sq mi), making it the second largest Spanish-speaking city proper in the world. According to the most recent definition agreed upon by the federal and state governments, the population of Greater Mexico City is 21,804,515, which makes it the world's sixth-largest metropolitan area and the second-largest urban agglomeration in the Western Hemisphere (behind São Paulo, Brazil). Greater Mexico City has a GDP of $411 billion in 2011, which makes it one of the most productive urban areas in the world. The city was responsible for generating 15.8% of Mexico's GDP, and the metropolitan area accounted for about 22% of the country's GDP. If it were an independent country in 2013, Mexico City would be the fifth-largest economy in Latin America.

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Plateau in the context of Plain

In geography, a plain, commonly known as flatland, is a flat expanse of land that generally has few rapid or steep changes in elevation. Natural vegetation in plains can include prairies/grasslands, forests, savanah, tundra, and desert biomes, among others. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or uplands. Plains are one of the major landforms on earth, being present on all continents and covering more than one-third of the world's land area. Plains in many areas are important for agriculture. There are various types of plains, and biomes on them.

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Plateau in the context of Balochistan, Pakistan

Balochistan (/bəˈlɒɪstɑːn, bəˌlɒɪˈstɑːn, -stæn/; Balochi: بلۏچستان, romanised: Balòcestàn, Balochi pronunciation: [baˈloːt͡ʃest̪ɑːn]; Urdu: بلوچستان, romanisedBalocistān, Urdu pronunciation: [bəloːt͡ʃɪst̪ɑːn] ) is a province of Pakistan. Located in the southwestern region of the country, Balochistan is the largest province of Pakistan by land area but is the least populated one. It is bordered by the Pakistani provinces of Khyber Pakhtunkhwa to the north-east, Punjab to the east, and Sindh to the southeast; shares international borders with Iran to the west and Afghanistan to the north; and is bound by the Arabian Sea to the south. Balochistan is an extensive plateau of rough terrain divided into basins by ranges of sufficient height and ruggedness. It has a large deep-sea port, the Port of Gwadar, lying in the Arabian Sea.

Although it constitutes approximately 44% of Pakistan's land area, only 5% of it is arable, and it is noted for an extremely dry desert climate. Despite this, agriculture and livestock make up about 47% of Balochistan's economy.

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Plateau in the context of Mountain

A mountain is an elevated portion of the surface of a planet, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 600 metres (2,000 ft) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges.

Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers.

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Plateau in the context of Northern Bulgaria

Northern Bulgaria (Bulgarian: Северна България, romanizedSeverna Bylgarija), also called Moesia (Bulgarian: Мизия, Mizija) is the northern half of Bulgaria, located to the north of the main ridge of the Balkan Mountains which conventionally separates the country into a northern and a southern part. Besides the Balkan Mountains, Northern Bulgaria borders the Timok River and Serbia to the west, the Danube River and Romania to the north, and the Bulgarian Black Sea Coast to the east.

Geographically, the region's terrain is relatively uniform, dominated by the hilly Danubian Plain, with some low plateaus to the east. Northern Bulgaria covers an area of 48,596 square kilometres and has a population of 2,674,347 according to the 2011 census (36% of Bulgaria's entire population), with a population density of 55 people per km². The three largest cities are Varna, Rousse and Pleven.

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Plateau in the context of Danubian Plain (Bulgaria)

The Danubian Plain (Bulgarian: Дунавска равнина, romanizedDunavska ravnina) constitutes the northern part of Bulgaria, situated north of the Balkan Mountains and south of the Danube. Its western border is the Timok River, and to the east it borders the Black Sea. The plain has an area of 31,523 square kilometres (12,171 sq mi). It is about 500 kilometres (310 mi) long and 20 to 120 kilometres (12 to 75 mi) wide.

The Danubian Plain is contiguous with the Wallachian Plain (forming the Lower Danubian Plain), but its elevation is slightly higher and the relief is more hilly and rolling, featuring numerous plateaux and river valleys. The climate is markedly temperate continental with a weak Black Sea influence in the east. Precipitation is on average 450–650 mm a year. Important rivers include the Danube, the Iskar, the Yantra, the Osam, the Vit, the Rusenski Lom, the Ogosta, and the Lom.

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Plateau in the context of Golan Heights

The Golan Heights, or simply the Golan, is a basaltic plateau at the southwest corner of Syria. It is bordered by the Yarmouk River in the south, the Sea of Galilee and Hula Valley in the west, the Anti-Lebanon mountains with Mount Hermon in the north and Wadi Raqqad in the east. It hosts vital water sources that feed the Hasbani River and the Jordan River. Two thirds of the area was depopulated and occupied by Israel following the 1967 Six-Day War and then effectively annexed in 1981. The international community largely considers the area Israeli-occupied Syrian territory. The United States recognized it as part of Israel in 2019 during the first Trump administration. In 2024, Israel occupied parts of the remaining one third of the area.

The earliest evidence of human habitation on the Golan dates to the Upper Paleolithic period. It was home to the biblical Geshur, and was later incorporated into Aram-Damascus, before being ruled by several foreign and domestic powers, including the Assyrians, Babylonians, Persians, Itureans, Hasmoneans, Romans, Ghassanids, several caliphates, and the Mamluk Sultanate. It was ruled by the Ottoman Empire from the 16th century until its collapse, and subsequently became part of the French Mandate in Syria and the State of Damascus in 1923. When the mandate terminated in 1946, it became part of the newly independent Syrian Arab Republic, spanning about 1,800 km (690 sq mi).

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Plateau in the context of Pothohar Plateau

The Pothohar Plateau (Punjabi: پوٹھوہار پَٹھوار, romanized: Pо̄ṭhoā̀r Paṭhwār; Urdu: سطح مرتفع پوٹھوہار, romanized: Satāh Murtafā Pо̄ṭhohār), also known as the Northern Punjab Plateau, is a plateau within the Sagar Doab of north-western Punjab in Pakistan. It is located between the Indus and Jhelum rivers.

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Plateau in the context of Volcanic plateau

A volcanic plateau is a plateau produced by volcanic activity. There are two main types: lava plateaus and pyroclastic plateaus.

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Plateau in the context of Stageira Chalkidikis

Stagira (Greek: Στάγειρα, also: Στάγιρα - Stagira) is a Greek village lying on a plateau on the Chalcidice peninsula, at the foot of the Argirolofos hill. The village stands approximately 18 kilometers southwest of the ruins of ancient Stageira, the birthplace of Aristotle.

A modern statue of Aristotle and small theme park is located next to the modern town. It is part of the municipal unit Stagira-Akanthos within the municipality Aristotelis.

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Plateau in the context of Val di Noto

Val di Noto (lit.'Province of Noto') is a historical and geographical area encompassing the south-eastern third of Sicily; it is dominated by the limestone Hyblaean plateau. Historically, it was one of the three valli of Sicily.
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Plateau in the context of Harare

Harare (/həˈrɑːr/ hə-RAR-ay), formerly known as Salisbury, is the capital and largest city of Zimbabwe. The city proper has an area of 982.3 km (379.3 sq mi), a population of 1,849,600 as of the 2022 census, and an estimated 2,487,209 people in its metropolitan province. The city is situated in north-eastern Zimbabwe in the country's Mashonaland region. Harare Metropolitan Province incorporates the city and the municipalities of Chitungwiza, Epworth and Ruwa. The city sits on a plateau at an elevation of 1,483 metres (4,865 feet) above sea level, and its climate falls into the subtropical highland category.

The city was founded in 1890 by the Pioneer Column, a small military force of the British South Africa Company, and was named Fort Salisbury after the British Prime Minister Lord Salisbury. Company administrators demarcated the city and ran it until Southern Rhodesia achieved responsible government in 1923. Salisbury was thereafter the seat of the Southern Rhodesian (later Rhodesian) government and, between 1953 and 1963, the capital of the Central African Federation. It retained the name Salisbury until 1982 when it was renamed Harare on the second anniversary of Zimbabwe's independence from the United Kingdom. The national parliament moved out of Harare upon completion of the New Parliament of Zimbabwe in Mount Hampden in April 2022.

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