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The Central Pangean Mountains were an extensive northeast–southwest trending mountain range in the central portion of the supercontinent Pangaea during the Carboniferous, Permian and Triassic periods. They were formed as a result of collision between the minor supercontinents Laurussia and Gondwana during the formation of Pangaea. At its greatest elevation during the early part of the Permian period, it was comparable to the present Himalayas. Remnants of this massive mountain range include the Appalachian Mountains and Ouachita Mountains of North America and the Little Atlas of Morocco, Africa.

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  • Central Pangean Mountains (en)
  • Cordillera Central de Pangea (es)
  • Central Pangean Mountains (it)
  • Centraal Pangea Gebergte (nl)
  • Центрально-Пангейські гори (uk)
  • 盤古中央山脈 (zh)
rdfs:comment
  • La Cordillera Central de Pangea fue una extensa cadena montañosa que se extendía en sentido noreste-suroeste en la parte central del supercontinente Pangea durante los períodos Carbonífero, Pérmico y Triásico. Se elevó como resultado de la colisión entre los supercontinentes menores Laurasia y Gondwana que formaron parte en la génesis de Pangea.​ En su mayor elevación, durante la primera parte del período Pérmico, era comparable al actual Himalaya. Los restos actuales de esta enorme cadena montañosa incluyen los Apalaches y las montañas Ouachita en América del Norte, los montes Atlas de Marruecos en África y los macizos Ibérico, Armoricano, Central y gran parte de las Tierras Altas de Escocia, incluido el pico Ben Nevis en Europa. (es)
  • Le Central Pangean Mountains erano una estesa catena montuosa, sviluppata in direzione nordest-sudovest, situata nella parte centrale del supercontinente Pangea durante il Triassico. Si formò come risultato della collisione fra i più piccoli supercontinenti Laurussia e Gondwana durante la formazione di Pangea. Resti di questa imponente catena montuosa sono i monti Appalachi in America del Nord e l'Anti Atlante in Marocco, Nella formazione delle Central Pangean Mountains furono coinvolti vari periodi di formazione delle montagne, compresa l'orogenesi acadiana, la caledoniana e l'alleganiana. (it)
  • Het Centraal Pangea Gebergte was een gebergte in centraal Pangea gedurende het Trias. Het gebergte scheidde Noord- van Zuid-Pangea. De Appalachen, Ouachita Mountains, Anti-Atlas en het grootste deel van de Schotse Hooglanden zijn restanten van dit gebergte. (nl)
  • Центрально-Пангейські гори — колишнє гірське пасмо прямуюче з північного сходу на південний захід в центральній частині суперконтиненту Пангея під час тріасового періоду. Утворилися в результаті континентальної колізії між суперконтинентами Лавразія і Гондвана в процесі утворення Пангеї Сьогоденними рештками Центрально-Пангейських гір є Аппалачі у Північній Америці і Малий Атлас — Марокко, Африка. Центрально-Пангейські гори зазнали , каледонського та орогенезів. (uk)
  • 盤古中央山脈（Central Pangean Mountains）是盤古大陸上一個東北－西南走向的古山脈。該山脈是因為兩個面積較小的超大陸歐美大陸和冈瓦那大陆相碰撞形成盤古大陸的過程中形成。這個巨大山脈的殘餘就是今日北美洲阿巴拉契亚山脉和北非摩洛哥的小阿特拉斯山脈。 盤古中央山脈是一系列造山運動的產物，這些造山運動有阿卡迪亞造山運動、加里東造山運動和阿利根尼造山運動。 (zh)
  • The Central Pangean Mountains were an extensive northeast–southwest trending mountain range in the central portion of the supercontinent Pangaea during the Carboniferous, Permian and Triassic periods. They were formed as a result of collision between the minor supercontinents Laurussia and Gondwana during the formation of Pangaea. At its greatest elevation during the early part of the Permian period, it was comparable to the present Himalayas. Remnants of this massive mountain range include the Appalachian Mountains and Ouachita Mountains of North America and the Little Atlas of Morocco, Africa. (en)
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  • The Central Pangean Mountains were an extensive northeast–southwest trending mountain range in the central portion of the supercontinent Pangaea during the Carboniferous, Permian and Triassic periods. They were formed as a result of collision between the minor supercontinents Laurussia and Gondwana during the formation of Pangaea. At its greatest elevation during the early part of the Permian period, it was comparable to the present Himalayas. Remnants of this massive mountain range include the Appalachian Mountains and Ouachita Mountains of North America and the Little Atlas of Morocco, Africa. A number of mountain building periods were involved in the formation of the Central Pangean Mountains, including the Acadian, Caledonian, Alleghenian, Mauritanide and Variscan orogenies. The eastern portions of the range are also called the Variscan Mountains. (en)
  • La Cordillera Central de Pangea fue una extensa cadena montañosa que se extendía en sentido noreste-suroeste en la parte central del supercontinente Pangea durante los períodos Carbonífero, Pérmico y Triásico. Se elevó como resultado de la colisión entre los supercontinentes menores Laurasia y Gondwana que formaron parte en la génesis de Pangea.​ En su mayor elevación, durante la primera parte del período Pérmico, era comparable al actual Himalaya. Los restos actuales de esta enorme cadena montañosa incluyen los Apalaches y las montañas Ouachita en América del Norte, los montes Atlas de Marruecos en África y los macizos Ibérico, Armoricano, Central y gran parte de las Tierras Altas de Escocia, incluido el pico Ben Nevis en Europa. (es)
  • Le Central Pangean Mountains erano una estesa catena montuosa, sviluppata in direzione nordest-sudovest, situata nella parte centrale del supercontinente Pangea durante il Triassico. Si formò come risultato della collisione fra i più piccoli supercontinenti Laurussia e Gondwana durante la formazione di Pangea. Resti di questa imponente catena montuosa sono i monti Appalachi in America del Nord e l'Anti Atlante in Marocco, Nella formazione delle Central Pangean Mountains furono coinvolti vari periodi di formazione delle montagne, compresa l'orogenesi acadiana, la caledoniana e l'alleganiana. (it)
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