Basin and Range–Colorado Plateau transition

E842017

The Basin and Range–Colorado Plateau transition is a geologic boundary zone in the southwestern United States where the highly extended Basin and Range Province meets the relatively stable, uplifted Colorado Plateau, producing complex faulting, volcanism, and varied topography.

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Statements (46)

Predicate Object
instanceOf geologic boundary zone
tectonic transition zone
associatedWith Cenozoic tectonism
Cenozoic volcanism
lithospheric thinning
uplift of Colorado Plateau
boundedBy Basin and Range Province to the west
Colorado Plateau to the east
characterizedBy complex faulting
varied topography
volcanism
geologicAge primarily Cenozoic
geologicProcess block faulting
crustal extension
normal faulting
hasGradientIn crustal thickness
heat flow
lithospheric strength
hasStructure accommodation zones
high-angle normal faults
listric normal faults
transfer zones
hasTopography basins and ranges
escarpments
high-standing plateaus
steep physiographic gradients
hasVolcanicFeature basaltic lava flows
cinder cones
monogenetic volcanic fields
small stratovolcanoes
importantFor seismic hazard assessment in the southwestern United States
studies of plateau uplift mechanisms
understanding continental extension
influences distribution of sedimentary basins
regional drainage patterns
locatedIn southwestern United States
overprints Paleozoic sedimentary sequences
older Proterozoic basement structures
partOf interior western North America
separates Basin and Range Province
Colorado Plateau
studiedBy structural geologists
tectonophysicists
volcanologists
tectonicStyleContrastBetween highly extended crust of Basin and Range Province
relatively stable Colorado Plateau

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Referenced by (18)

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San Francisco volcanic field relatedTo Basin and Range–Colorado Plateau transition
Piute County, Utah isInPhysiographicRegion Great Basin–Colorado Plateau transition zone
linked to: Basin and Range–Colorado Plateau transition
Plains of San Agustin partOf Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Mount Taylor region Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
northwestern Arizona locatedIn Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Jemez volcanic field geologicalProvince Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Greenlee County locatedIn Colorado Plateau–Basin and Range transition zone
linked to: Basin and Range–Colorado Plateau transition
Shivwits Reservation locatedInRegion Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Huntington Canyon geologicalSetting Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Utah State Route 264 geographicalContext Colorado Plateau–Great Basin transition area
linked to: Basin and Range–Colorado Plateau transition
Utah State Route 143 regionType Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Nacimiento Mountains geologicalProvince Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
White Rock Overlook geographicContext Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Toquerville, Utah region Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Mount Baldy (Arizona) region Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Kanarraville regionType Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Springerville, Arizona locatedInPhysiographicRegion Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition
Mogollon-Datil volcanic field overlies Colorado Plateau margin
linked to: Basin and Range–Colorado Plateau transition