Karakoram orogeny

E280248

The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.

All labels observed (1)

Label Occurrences
Karakoram orogeny canonical 1

How this entity was disambiguated

Statements (52)

Predicate Object
instanceOf geological process ⓘ
mountain-building event ⓘ
orogeny ⓘ
actsOn Eurasian Plate margin ⓘ
Karakoram terrane ⓘ
associatedWith Karakoram fault system ⓘ
granitoid intrusions ⓘ
metamorphic core complexes ⓘ
normal faulting at high elevations ⓘ
strike-slip faulting ⓘ
thrust faulting ⓘ
causedBy India–Eurasia continental collision ⓘ
continental collision ⓘ
convergent plate boundary ⓘ
tectonic compression ⓘ
geologicalAge Cenozoic ⓘ
Neogene ⓘ
Quaternary ⓘ
hasFeature deep valleys ⓘ
extreme elevation gradients ⓘ
high, rugged relief ⓘ
steep slopes ⓘ
hasPeak Broad Peak ⓘ
Gasherbrum I ⓘ
Gasherbrum II ⓘ
K2 ⓘ
Masherbrum ⓘ
influences glaciation in the Karakoram Range ⓘ
regional climate ⓘ
river incision ⓘ
sediment supply to surrounding basins ⓘ
isOngoing true ⓘ
locatedIn Asia ⓘ
China ⓘ
Gilgit-Baltistan ⓘ
India ⓘ
Karakoram Range ⓘ
linked to: Karakoram

Ladakh ⓘ
Pakistan ⓘ
Xinjiang ⓘ
western Himalayas ⓘ
partOf Alpine–Himalayan orogenic belt ⓘ
resultsIn crustal shortening ⓘ
crustal thickening ⓘ
exhumation of deep crustal rocks ⓘ
faulting ⓘ
folding ⓘ
high topography ⓘ
magmatism ⓘ
metamorphism ⓘ
mountain uplift ⓘ
startTime Cenozoic era ⓘ
linked to: Cenozoic

How these facts were elicited

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Hispar Glacier → geologicalSetting → Karakoram orogeny ⓘ