List of orogenies

• Pan-African orogeny – series of major Neoproterozoic orogenic events which related to the formation of the supercontinents Gondwana and Pannotia (550 Ma) (Neoproterozoic)
• Damara orogeny – Mountain building event at the intersection of the Congo and the Kalahari cratons.
• Kibaran orogeny – mountain building event in what is now Africa
• Eburnean orogeny – A mountain building event in what is now West Africa
• East African Orogeny – The main stage in the Neoproterozoic assembly of East and West Gondwana
• Mauritanide Orogeny – An ancient orogen parallel to the west coast of Africa from Morocco to Guinea-Bissau
• Mozambique Orogeny – A band in the earth's crust from East Antarctica through East Africa up to the Arabian-Nubian Shield
• Zambezian Orogeny – Area of mountain building now in southern Zambia and northern Zimbabwe

Orogenies affecting Antarctica include:[1]

• Napier orogeny (4000 ± 200 Ma)
• Rayner orogeny (~ 3500 Ma)
• Humboldt orogeny – Geologic formation in Antarctica (~ 3000 Ma)
• Insel orogeny (2650 ± 150 Ma)
• Early Ruker orogeny (2000–1700 Ma)
• Late Ruker orogeny (Also known as the Nimrod orogeny)(1000 ± 150 Ma)
• Beardmore orogeny (633–620 Ma)
• Ross orogeny (~550 to ~480 Ma)
• Borchgrevink orogeny
• Peninsula orogeny

Persia–Tibet–Burma orogeny in Eurasian Plate

• The Aravalli-Delhi Orogen (precambrian)
• The Altaid Orogeny (Paleozoic)
• The Cimmerian and Cathaysian orogenies
  • Active through Triassic and Jurassic Periods along south and southeast Asia.
• Persia–Tibet–Burma orogeny (Cenozoic), caused by the continuing collision of the Arabian and Indian Plates with the Eurasian Plate, encompassing:
  • The Himalayan orogeny, forming the Himalaya Mountains, as a result of the ongoing collision of the Indian Plate with the Eurasian Plate.
• The Dabie-Sulu orogeny (Mesozoic)
• Uralian orogeny – the long series of linear deformation and mountain building events that raised the Ural Mountains Formation of the Ural Mountains, Eurasia, during the Permian Period.

• Saamian orogeny Formation of an extensive area of tonalitic-trondhjemitic crust in Fennoscandia, from 3.1 Ga to 2.9 Ga
• Lopian orogeny – Archean orogeny Formation of two different types of terrain compatible with plate tectonic concepts. One is a belt of high-grade gneisses formed in a regime of strong mobility, while the other is a region of granitoid intrusions and greenstone belts surrounded by the remnants of a Saamian substratum, from 2.9 Ga to 2.6 Ga.
• Svecofennian orogeny, also known as Svecokarelian orogeny – A series of related orogenies that resulted in the formation of much of the continental crust in what is today Sweden and Finland plus some minor parts of Russia, from 2.0 Ga to 1.75 Ga.
• Gothian orogeny Formation of tonalitic-granodioritic plutonic rocks and calc-alkaline volcanites (like the Svecofennian orogeny) from 1.75 Ga to 1.5 Ga.
• Sveconorwegian orogeny Essentially reworking of previously formed crust, from 1.25 Ga to 900 Ma.
• Timanide orogeny affecting the northern Baltic Shield during the Neoproterozoic Era, from 620 Ma to 550 Ma.
• Cadomian orogeny on the north coast of Armorica in the Ediacaran/Cambrian from 660 Ma to 540 Ma.
• Caledonian orogeny Deformation of the western Scandinavian Peninsula, Britain and Ireland in the Ordovician Grampian phase and the Silurian Scandian phase.[2]
• Uralian orogeny – the long series of linear deformation and mountain building events that raised the Ural Mountains, during the Permian Period.
• Variscan orogeny, also known as Hercynian orogeny – Collision of tectonic plates resulting in the creation of mountains Deformation in western Iberia, SW Ireland, SW England, central and western France, southern Germany and Czech Republic during the Devonian and Carboniferous Periods.
• Alpine orogeny – Formation of the Alpine mountain ranges of Europe, the Middle East and northwest Africa, encompassing:
  • the Formation of the Alps during the Eocene through Miocene Periods.
  • Carpathian orogeny building the Carpathian Mountains of eastern Europe during the Jurassic-Cretaceous to Miocene Period.
  • Hellenic orogeny in Greece and the Aegean area during Eocene through Miocene Periods.
• Mediterranean Ridge

Taconic orogeny

• Algoman orogeny, also known as Kenoran orogeny – Late Archaean episode of mountain building in what is now North America, Superior province, South Dakota to Lake Huron, Late Archean 2700-2500 Ma.
• Wopmay orogeny, Along western edge of Canadian shield, 2100–1900 Ma.
• Trans-Hudson orogeny, also known as Hudsonian orogeny, Extends from Hudson Bay west into Saskatchewan then south through the western Dakotas and Nebraska. Result of the collision of the Superior craton with the Hearne craton and the Wyoming craton during the Proterozoic. Lasted from 2000–1800 Ma.
• Nagssugtoqidian orogeny – A late Paleoproterozoic mountain-building event in Greenland, 1910–1770 Ma.
• Ketilidian orogeny, late Paleoproterozoic collision at the southern margin of the North Atlantic Craton, 1850–1720 Ma
• Penokean orogeny Wisconsin, Minnesota, and Michigan, U. S. A. and southern Ontario, Canada, 1850-1840 Ma.
• Great Falls orogeny (Also known as the Big Sky orogeny) Proterozoic collision between the Hearne craton and the Wyoming craton in southwest Montana, 1770 Ma.
• Ivanpah orogeny Mojave province, south western USA
• Yavapai orogeny – Mountain building event 1.7 billion years ago in the southerwestern United States, mid to south western USA, 1710-1700 Ma.
• Mazatzal orogeny, mid to south western USA, 1675-1650 Ma.
• Picuris orogeny, mid to south western USA, 1430-1300 Ma.
• Grenville orogeny Worldwide during the late Proterozoic, 1300–1000 Ma. Associated with the assembly of the supercontinent Rodinia. Formed folded mountains in Eastern North America from Newfoundland to North Carolina, 1100–1000 Ma.
• Caledonian orogeny, including:
  • East Greenland Orogen, formed from Cryogenian to Devonian
  • Taconic phase – A mountain building period that affected most of New England in the NE U.S. and Canada during the Ordovician Period.
  • Acadian phase – North American orogeny in the Eastern U.S. during Silurian and Devonian Periods.
• Appalachian orogeny, usually seen as the same as the Variscan orogeny in Europe.
  • Appalachian Mountains is a well studied orogenic belt resulting from a late Paleozoic collision between North America and Africa.
  • Taconic orogeny – A mountain building period that affected most of New England
  • Acadian orogeny – North American orogeny
  • Alleghanian orogeny
• Ouachita orogeny, Ouachita Mountains of Arkansas and Oklahoma is an orogenic belt that dates from the late Paleozoic Era and is most likely a continuation of the Appalachian orogeny west across the Mississippi embayment - Reelfoot Rift zone.
• Antler orogeny, Ancestral Sierra Nevada western United States. Late Devonian - early Mississippian.
• Innuitian orogeny, also known as Ellesmerian orogeny, Innuitian Mountains, Canadian Arctic, extending from Ellesmere Island to Melville Island, Mississippian 345 Ma.
• Sonoma orogeny, Rocky Mountains, western North America, 270–240 Ma.
• Nevadan orogeny, Developed along western North America during the Jurassic Period.
• Sevier orogeny, Rocky Mountains, western North America, 140–50 Ma.
• Laramide orogeny – A period of mountain building in western North America, which started in the Late Cretaceous, Rocky Mountains, western North America, 40–70 Ma.
• Pasadena orogeny, Transverse Ranges, western North America, Pleistocene to present day

• Transamazonian orogeny, (Paleoproterozoic)[3]
• Guriense orogeny
• Sunsás orogeny
• Cariri Velhos orogeny
• Brasiliano-Pan African orogeny, Brasilia Belt
  • Pampean orogeny, Paraguai Belt
• Chonide orogeny
• Terra Australis Orogeny
  • Pampean orogeny
  • Famatinian orogeny
• San Rafael orogeny
• Gondwanide orogeny – Permian mountain forming tectonic evsnt, Sierra de la Ventana
• Toco orogeny, Chilean Coast Range 300–330 Ma.[4]
• Andean orogeny – Ongoing mountain-forming process in South America, Andes Mountains, 0–200 Ma.