Midcontinent Rift System

E923856

The Midcontinent Rift System is a billion-year-old, failed continental rift running in a great arc through the central United States and Canada, notable for its thick volcanic rock sequences and associated mineral deposits.

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All labels observed (1)

Label Occurrences
Midcontinent Rift System canonical 1

Statements (49)

Predicate Object
instanceOf Proterozoic tectonic feature
continental rift
failed rift
geological rift
age approximately 1.1 billion years
associatedWith Keweenawan Supergroup NERFINISHED
Lake Superior basin NERFINISHED
continental breakup processes
contains intrusive mafic-ultramafic bodies
thick sequences of flood basalts
discoveredBy geophysical surveys
extendsThrough Iowa NERFINISHED
Kansas NERFINISHED
Kansas-Nebraska region subsurface
Lake Superior region NERFINISHED
Michigan NERFINISHED
Minnesota NERFINISHED
Nebraska NERFINISHED
Oklahoma NERFINISHED
Ontario NERFINISHED
Wisconsin NERFINISHED
formedDuring Mesoproterozoic era
geologicPeriod Mesoproterozoic
hasEconomicResource copper deposits
iron ore deposits
native copper deposits of Keweenaw Peninsula
nickel deposits
platinum-group elements
hasFeature associated sedimentary basins
gravity anomaly
large igneous province characteristics
magnetic anomaly
thick volcanic rock sequences
hasRockType basalt
mafic volcanic rocks
sedimentary rocks
hasShape curved arc
locatedIn Canada
North America
United States of America
surface form: United States
notableFor associated mineral deposits
large gravity and magnetic anomalies
thick volcanic rock sequences
status failed rift
studiedInDiscipline geology
geophysics
tectonics
tectonicSetting intraplate rift
terminatedBy compressional tectonics

Referenced by (1)

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

Keweenaw Peninsula geologicalFeature Midcontinent Rift System