The Nevadan orogeny occurred along the western margin of North America during the Middle Jurassic to Early Cretaceous time which is approximately from 155 Ma to 145 Ma. Throughout the duration of this orogeny there were at least two different kinds of orogenic processes occurring. During the early stages of orogenesis an "Andean type" continental magmatic arc developed due to subduction of the Farallon oceanic plate beneath the North American Plate. The latter stages of orogenesis, in contrast, saw multiple oceanic arc terranes accreted onto the western margin of North America in a "Cordilleran type" accretionary orogen. Deformation related to the accretion of these volcanic arc terranes is mostly limited to the western regions of the resulting mountain ranges (Klamath Mountain range and S
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| - Nevadan orogeny (en)
- Orogenia do Nevada (pt)
- 內華達造山運動 (zh)
- Невадійська складчастість (uk)
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| - Невадійська (невадська) складчастість (рос. невадийская (невадская) складчатость; англ. Nevadian folding, Nevadian orogeny; нім. nevadische Faltung f) — одна з епох мезозойської складчастості, яка проявилася в Західних Кордильєрах Північної Америки. Від штату Невада в США й на захід. (uk)
- A Orogenia do Nevada foi uma grande orogenia que ocorreu no oeste da América do Norte entre a época Jurássica Média e a Jurássica Superior do período Jurássico (há aproximadamente cerca de 180 a 140 milhões de anos). (pt)
- 內華達造山運動是在侏羅紀中期到白堊紀早期（1.55億到1.45億年前）發生於今天的北美洲西部的一系列造山運動。期間至少發生過兩次不同類型的造山運動。第一次是由於法拉龍板塊向北美大陸板塊下俯衝、產生大陸岩漿弧的碰撞造山，第二次則是由多個洋内弧在北美大陸板塊上增生導致的增生造山。內華達造山運動總共只持續了1000萬年，這在造山運動中較為罕見。 (zh)
- The Nevadan orogeny occurred along the western margin of North America during the Middle Jurassic to Early Cretaceous time which is approximately from 155 Ma to 145 Ma. Throughout the duration of this orogeny there were at least two different kinds of orogenic processes occurring. During the early stages of orogenesis an "Andean type" continental magmatic arc developed due to subduction of the Farallon oceanic plate beneath the North American Plate. The latter stages of orogenesis, in contrast, saw multiple oceanic arc terranes accreted onto the western margin of North America in a "Cordilleran type" accretionary orogen. Deformation related to the accretion of these volcanic arc terranes is mostly limited to the western regions of the resulting mountain ranges (Klamath Mountain range and S (en)
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| - The Nevadan orogeny occurred along the western margin of North America during the Middle Jurassic to Early Cretaceous time which is approximately from 155 Ma to 145 Ma. Throughout the duration of this orogeny there were at least two different kinds of orogenic processes occurring. During the early stages of orogenesis an "Andean type" continental magmatic arc developed due to subduction of the Farallon oceanic plate beneath the North American Plate. The latter stages of orogenesis, in contrast, saw multiple oceanic arc terranes accreted onto the western margin of North America in a "Cordilleran type" accretionary orogen. Deformation related to the accretion of these volcanic arc terranes is mostly limited to the western regions of the resulting mountain ranges (Klamath Mountain range and Sierra Nevada) and is absent from the eastern regions. In addition, the deformation experienced in these mountain ranges is mostly due to the Nevadan orogeny and not other external events such as the more recent Sevier and Laramide Orogenies. It is noted that the Klamath Mountains and the Sierra Nevada share similar stratigraphy indicating that they were both formed by the Nevadan orogeny. In comparison with other orogenic events, it appears that the Nevadan Orogeny occurred rather quickly taking only about 10 million years as compared to hundreds of millions of years for other orogenies around the world (ex. Trans-Hudson orogeny). (en)
- Невадійська (невадська) складчастість (рос. невадийская (невадская) складчатость; англ. Nevadian folding, Nevadian orogeny; нім. nevadische Faltung f) — одна з епох мезозойської складчастості, яка проявилася в Західних Кордильєрах Північної Америки. Від штату Невада в США й на захід. (uk)
- A Orogenia do Nevada foi uma grande orogenia que ocorreu no oeste da América do Norte entre a época Jurássica Média e a Jurássica Superior do período Jurássico (há aproximadamente cerca de 180 a 140 milhões de anos). (pt)
- 內華達造山運動是在侏羅紀中期到白堊紀早期（1.55億到1.45億年前）發生於今天的北美洲西部的一系列造山運動。期間至少發生過兩次不同類型的造山運動。第一次是由於法拉龍板塊向北美大陸板塊下俯衝、產生大陸岩漿弧的碰撞造山，第二次則是由多個洋内弧在北美大陸板塊上增生導致的增生造山。內華達造山運動總共只持續了1000萬年，這在造山運動中較為罕見。 (zh)
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