Ancestral Rocky Mountains orogeny

E1007892

The Ancestral Rocky Mountains orogeny was a late Paleozoic mountain-building event that created a series of high-standing uplifts and basins in what is now the central and southwestern United States.

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All labels observed (1)

Label Occurrences
Ancestral Rocky Mountains orogeny canonical 1

Statements (47)

Predicate Object
instanceOf geological event
mountain-building event
orogeny
affectedRegion Arizona NERFINISHED
Colorado NERFINISHED
Kansas NERFINISHED
New Mexico NERFINISHED
Oklahoma NERFINISHED
Texas NERFINISHED
Utah NERFINISHED
causedBy assembly of Pangea
far-field stresses from plate collisions
characterizedBy block uplifts
reverse faulting
strike-slip faulting
subsiding basins
thrust faulting
continent Laurentia NERFINISHED
North America
endTime early Permian
followedBy Laramide orogeny
formedStructure Ancestral Front Range NERFINISHED
Ancestral Uncompahgre highlands NERFINISHED
Central Colorado trough NERFINISHED
Delaware Basin NERFINISHED
Midcontinent basins and uplifts NERFINISHED
Paradox Basin NERFINISHED
Uncompahgre uplift NERFINISHED
locatedIn central United States
southwestern United States NERFINISHED
partOf late Paleozoic
precededBy Antler orogeny NERFINISHED
produced alluvial fan deposits
marine shelf deposits in adjacent basins
thick Pennsylvanian sedimentary sequences
relatedTo Alleghanian orogeny NERFINISHED
Ouachita orogeny NERFINISHED
resultedIn Ancestral Rocky Mountains NERFINISHED
high-standing uplifts
intracratonic basins
series of basins
series of uplifts
startTime late Mississippian
tectonicSetting interior of North American craton
intraplate deformation
timePeriod Pennsylvanian
early Permian

Referenced by (1)

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

Wichita Mountains orogeny Ancestral Rocky Mountains orogeny