mountain-building event
C4520
concept
A mountain-building event is a geological process, typically driven by plate tectonics, in which the Earth's crust is deformed, uplifted, and thickened to form mountain ranges over millions of years.
All labels observed (7)
| Label | Occurrences |
|---|---|
| mountain-building event canonical | 25 |
| Neoproterozoic orogeny | 3 |
| Paleozoic orogeny | 3 |
| Cenozoic orogeny | 1 |
| Mesozoic tectonic event | 1 |
| mountain-building episode | 1 |
| orogenic episode | 1 |
Instances (34)
| Instance | Via concept surface |
|---|---|
| Ancestral Rocky Mountains orogeny | — |
| Pan-African orogeny | Neoproterozoic orogeny |
| Alpine orogeny | — |
| Cascadian orogeny | mountain-building episode |
| Cordilleran orogeny | — |
| Laramide orogeny | — |
| Appalachian orogeny | — |
| Cadomian orogeny | Neoproterozoic orogeny |
| Caledonian orogeny | Paleozoic orogeny |
| Karakoram orogeny | — |
| Yanshanian orogeny | Mesozoic tectonic event |
| Transverse Ranges orogeny | — |
| Marathon orogeny | — |
| Qinling–Dabie orogeny | — |
| Himalayan orogeny | — |
| Blountian tectophase | orogenic episode |
| Brasiliano orogeny | Neoproterozoic orogeny |
| Damara orogeny | — |
| Kuunga orogeny | — |
| Baikal orogeny | — |
| Sevier orogeny | — |
| Columbian Orogeny | — |
| Apennine orogeny | — |
| Insular Orogeny | — |
| Innuitian orogeny | — |
| Namaqua-Natal orogeny | — |
| Kibaran orogeny | — |
| Laurentia–Baltica collision | Paleozoic orogeny |
| Banda orogeny | — |
| Taconic orogeny | — |
| closure of Iapetus Ocean | Paleozoic orogeny |
| Acadian orogeny | — |
| Carpathian orogeny | — |
| Variscan orogeny | — |