-
Orogeny (/ɒˈrɒdʒəni/) is a mountain-building
process that
takes place at a
convergent plate margin when
plate motion compresses the margin. An orogenic...
- The
Alpine orogeny or
Alpide orogeny[dubious – discuss] is an
orogenic phase in the Late
Mesozoic (Eoalpine) and the
current Cenozoic that has formed...
- The
Laramide orogeny was a time
period of
mountain building in
western North America,
which started in the Late Cretaceous, 80 to 70
million years ago...
- The
Variscan orogeny, or
Hercynian orogeny, was a
geologic mountain-building
event caused by Late
Paleozoic continental collision between Euramerica (Laurussia)...
-
Alleghanian orogeny). The
third mountain-building
event was the
Acadian orogeny which occurred between 375 and 359
million years ago. The
Acadian orogeny was...
- The
Acadian orogeny is a long-lasting
mountain building event which began in the
Middle Devonian,
reaching a
climax in the Late Devonian. It was active...
-
Nanga Parbat syntaxis at the
western end, are the
result of an
ongoing orogeny — the
collision of the
continental crust of two
tectonic plates, namely...
- of the Earth's crust),
beginning c. 800 to 650 Ma with the East
African Orogeny, the
collision of
India and
Madagascar with East Africa, and culminating...
-
smaller ocean basins. The
Carpathian mountains were
formed during the
Alpine orogeny in the
Mesozoic and
Cenozoic by
moving the
ALCAPA (Alpine-Carpathian-Pannonian)...
- The
Grenville orogeny was a long-lived
Mesoproterozoic mountain-building
event ****ociated with the ****embly of the
supercontinent Rodinia. Its record...
