Presentation Transcript
LARAMIDE OROGENY: LARAMIDE OROGENY Cretaceous - Tertiary
LARAMIDE OROGENY: LARAMIDE OROGENY Part of Cordilleran Orogeny
LARAMIDE OROGENY: LARAMIDE OROGENY Part of Cordilleran Orogeny
(Northern Rockies - mostly thrust faulting and folding)
LARAMIDE OROGENY: LARAMIDE OROGENY Part of Cordilleran Orogeny
(Northern Rockies - mostly thrust faulting and folding
Southern Rockies - folds and volcanism)
LARAMIDE OROGENY: LARAMIDE OROGENY Part of Cordilleran Orogeny
(Northern Rockies - mostly thrust faulting and folding
Southern Rockies - folds and volcanism
Central Rockies - (Wyoming, Colorado) faults)
LARAMIDE OROGENY: LARAMIDE OROGENY Causes of Laramide Orogeny?
LARAMIDE OROGENY: LARAMIDE OROGENY Causes of Laramide Orogeny?
Change in angle of convergence of Farallon Plate?
LARAMIDE OROGENY: LARAMIDE OROGENY Causes of Laramide Orogeny?
Change in angle of convergence of Farallon Plate?
Increase in rate of subduction of Farallon Plate?
LARAMIDE OROGENY: LARAMIDE OROGENY Causes of Laramide Orogeny?
Change in angle of convergence of Farallon Plate?
Increase in rate of subduction of Farallon Plate?
Change in angle of subduction of Farallon Plate? (45 degrees to 10 degrees?)
LARAMIDE OROGENY: LARAMIDE OROGENY Causes of Laramide Orogeny?
Change in angle of convergence of Farallon Plate?
Increase in rate of subduction of Farallon Plate?
Change in angle of subduction of Farallon Plate? (45 degrees to 10 degrees?)
'Tightening up' of new land accreted in Mesozoic?
LARAMIDE OROGENY: LARAMIDE OROGENY Includes the Black Hills
LARAMIDE OROGENY: LARAMIDE OROGENY Includes the Black Hills
dome - an uplift or anticline which is circular or elliptical in outline
LARAMIDE OROGENY: LARAMIDE OROGENY Includes the Black Hills
dome - an uplift or anticline which is circular or elliptical in outline
some rock in the Black Hills is old
2.5-2.6 by - Nemo
LARAMIDE OROGENY: LARAMIDE OROGENY Includes the Black Hills
dome - an uplift or anticline which is circular or elliptical in outline
some rock in the Black Hills is old
2.5-2.6 by - Nemo
1.6-1.75 by - Harney Peak area
LARAMIDE OROGENY: LARAMIDE OROGENY Includes the Black Hills
dome - an uplift or anticline which is circular or elliptical in outline
some rock in the Black Hills is old
2.5-2.6 by - Nemo
1.6-1.75 by - Harney Peak area
major uplift with Laramide Orogeny
LARAMIDE OROGENY: LARAMIDE OROGENY Includes the Black Hills
dome - an uplift or anticline which is circular or elliptical in outline
some rock in the Black Hills is old
2.5-2.6 by - Nemo
1.6-1.75 by - Harney Peak area
major uplift with Laramide Orogeny
major uplifts ended by Oligocene
LARAMIDE OROGENY: LARAMIDE OROGENY Includes the Black Hills
dome - an uplift or anticline which is circular or elliptical in outline
some rock in the Black Hills is old
2.5-2.6 by - Nemo
1.6-1.75 by - Harney Peak area
major uplift with Laramide Orogeny
major uplifts ended by Oligocene
minor uplifts to Pleistocene
LARAMIDE OROGENY: LARAMIDE OROGENY Major Black Hills Geologic Units
LARAMIDE OROGENY: LARAMIDE OROGENY Major Black Hills Geologic Units
Cambrian - Deadwood Fm.
LARAMIDE OROGENY: LARAMIDE OROGENY Major Black Hills Geologic Units
Cambrian - Deadwood Fm.
Mississippian - Pahasapa Fm. - Spearfish Canyon
LARAMIDE OROGENY: LARAMIDE OROGENY Major Black Hills Geologic Units
Cambrian - Deadwood Fm.
Mississippian - Pahasapa Fm. - Spearfish Canyon
Triassic - Spearfish Fm.
LARAMIDE OROGENY: LARAMIDE OROGENY Major Black Hills Geologic Units
Cambrian - Deadwood Fm.
Mississippian - Pahasapa Fm. - Spearfish Canyon
Triassic - Spearfish Fm.
Jurassic - Sundance Fm.
LARAMIDE OROGENY: LARAMIDE OROGENY Major Black Hills Geologic Units
Cambrian - Deadwood Fm.
Mississippian - Pahasapa Fm. - Spearfish Canyon
Triassic - Spearfish Fm.
Jurassic - Sundance Fm.
Cretaceous - Pierre Fm.
LARAMIDE OROGENY: LARAMIDE OROGENY Major Black Hills Geologic Units
Cambrian - Deadwood Fm.
Mississippian - Pahasapa Fm.
Triassic - Spearfish Fm.
Jurassic - Sundance Fm.
Cretaceous - Pierre Fm.
Oligocene - White River Gp.
LARAMIDE OROGENY: LARAMIDE OROGENY Cretaceous sea driven eastward by sediments from west
LARAMIDE OROGENY: LARAMIDE OROGENY Cretaceous sea driven eastward by sediments from west
Hell Creek (ss) - terrestrial
Fox Hills (ss) - marine
Pierre Shale - marine
LARAMIDE OROGENY: LARAMIDE OROGENY Sediment accumulation along western shore of Cretaceous Sea
LARAMIDE OROGENY: LARAMIDE OROGENY Sediment accumulation along western shore of Cretaceous Sea
thick vegetation in coastal marshes, along deltas, and behind barrier reefs
LARAMIDE OROGENY: LARAMIDE OROGENY Sediment accumulation along western shore of Cretaceous Sea
thick vegetation in coastal marshes, along deltas, and behind barrier reefs
some deposits 100 km wide
LARAMIDE OROGENY: LARAMIDE OROGENY Sediment accumulation along western shore of Cretaceous Sea
thick vegetation in coastal marshes, along deltas, and behind barrier reefs
some deposits 100 km wide
most Wyoming coal deposits Cretaceous and Paleocene
LARAMIDE OROGENY: LARAMIDE OROGENY Bentonites and volcanism
LARAMIDE OROGENY: LARAMIDE OROGENY Bentonites and volcanism
some volcanism in Idaho and Wyoming produced large volumes of ash (Cenozoic)
LARAMIDE OROGENY: LARAMIDE OROGENY Bentonites and volcanism
some volcanism in Idaho and Wyoming produced large volumes of ash (Cenozoic)
deposits of ash in Montana, Wyoming, South Dakota
LARAMIDE OROGENY: LARAMIDE OROGENY Bentonites and volcanism
some volcanism in Idaho and Wyoming produced large volumes of ash (Cenozoic)
deposits of ash in Montana, Wyoming, South Dakota
usually andlt; 1 m thick, but some up to 8m
LARAMIDE OROGENY: LARAMIDE OROGENY Bentonites and volcanism
some volcanism in Idaho and Wyoming produced large volumes of ash (Cenozoic)
deposits of ash in Montana, Wyoming, South Dakota
usually andlt; 1 m thick, but some up to 8m
partial decomposition of ash produces bentonite which swells when wet
LARAMIDE OROGENY: LARAMIDE OROGENY Laramide continued during Cenozoic
(Tetons in Miocene, Arizona 1200 y)
LARAMIDE OROGENY: LARAMIDE OROGENY Laramide continued during Cenozoic
(Tetons in Miocene, Arizona 1200 y)
Erosion rapidly filling basins in western North America
LARAMIDE OROGENY: LARAMIDE OROGENY Laramide continued during Cenozoic
(Tetons in Miocene, Arizona 1200 y)
Erosion rapidly filling basins in western North America
Colorado Plateau - uplifted sediments surrounded by mountains - (Pliocene-Miocene)
LARAMIDE OROGENY: LARAMIDE OROGENY Laramide continued during Cenozoic
(Tetons in Miocene, Arizona 1200 y)
Erosion rapidly filling basins in western North America
Colorado Plateau - uplifted sediments surrounded by mountains
Columbia Plateau - (Miocene - Pleistocene) Washington and Oregon 200,000 cubic km of basalt
LARAMIDE OROGENY: LARAMIDE OROGENY Laramide continued during Cenozoic
Erosion rapidly filling basins in western North America
Colorado Plateau - uplifted sediments surrounded by mountains
Columbia Plateau - (Miocene - Pleistocene) Washington and Oregon 200,000 cubic km of basalt
Cascades - Andean type uplift (Pliocene to recent) - (Lassen, Shasta, Rainier, St. Helens)
LARAMIDE OROGENY: LARAMIDE OROGENY Laramide continued during Cenozoic
Columbia Plateau - (Miocene - Pleistocene) Washington and Oregon 200,000 cubic km of basalt
Cascades - Andean type uplift (Pliocene to recent) - (Lassen, Shasta, Rainier, St. Helens)
Sierras - Nevadan Orogeny (Jurassic) and again in Pliocene- Pleistocene