Western North America is a patchwork is hundreds of terranes, which are crustal pieces or microplates (think of islands), that collided with and attached to North America across hundreds of millions of years -- adding piece-by-piece to the continent's width and building mountains as they produced volcanoes or pushed up sediments and rocks. This posts provides a very simplified timeline of the major orogenies and terranes that affected western North America. For a more in-depth look, see the resources below.
Slideshow
Precambrian
- Passive margin
- Cratonic, continental shelf deposits
Paleozoic
- Antler Orogeny: Late Devonian - Early Mississippian (375 - 300 Ma)
- Poorly understood: involves subduction, accretion of one or more island arcs to the passive margin, and widespread folding and thrust faulting (Roberts Mountain Allochton thrust over passive margin)
- Rocks in Utah; foreland basins form in Neveda
- Sonoma Orogeny - Permian - Triassic (280 - 200 Ma)
- Poorly understood, existence debated: theories include accreting island arcs (McCloud arc); convergent processes throwing oceanic sediments (Havallah terrane) onto crust via Golconda thrust; back-arc thrusting
- Terranes include: Brooke Range (AK), Stikine (BC), Sonoma (NV)
Mesozoic
- Nevadan Orogeny: Jurassic (180 - 140 Ma)
- Oceanic lithosphere subducts along edge of North America
- Subducting plate dehydrates, releases volatiles, causing partial mentling in mantle above plate
- Magma rises to produce Andean-style stratovolcanic arc underlain by large batholiths (Sierra Nevada batholiths)
- Wrangellia: Cretaceous (145 - 66 Ma)
- Large flood basalt terrane, reaching from British Columbia to Alaska, docks to North America
- Sevier Orogeny: Jurassic - Eocene (120 - 50 Ma)
- Subducting oceanic Farallon plate and accreting large terranes cause stacking up and eastward pushing of upper crustal thrust-fault slabs, mainly sedimentary rock
Cenozoic
- Laramide Orogeny: Late Cretaceous - Paleogene (80 - 40 Ma)
- Rapid shallow angle subduction drags Farallon plate along base of North America (flat-slab subduction)
- Many hundreds of miles inland, plate angles down into the deeper mantle
- Friction of dragging plate causes stress, uplifting the Laramide mountain ranges (e.g. the Rocky Mountains)
- Basin and Range: Miocene (17 Ma) - Present
- Extensional event related to transform plate boundary (San Andreas fault)
- Tension across the region pulls crust apart; crust stretches, rifts, and form grabens (rift valleys) with uplifted horsts ("mountains")
- Delamination (lower crust "shaved off") and isostatic uplift from high heat flow from mantle
- Cascadia Orogen: Oligocene (34 Ma) - Present
- Juan de Fuca plate, remnant of Farallon plate, continues to subduct into Cascadia subduction zone
- Coastal ranges, consisting of accreted oceanic and ocean island crust, continue to accrete and uplift along coast
Online Resources
- Tectonic History of North America by Period: https://www2.nau.edu/rcb7/hist_by_period.html; see also: https://www2.nau.edu/rcb7/Text_WUS.html
- Geology of the Pacific Northwest: http://commons.wvc.edu/rdawes/FocusPages/FPindex.html
- North American Orogenies: https://en.wikipedia.org/wiki/List_of_orogenies#North_American_orogenies
- Mesozoic Tectonics of North America: http://www.usouthal.edu/geology/haywick/GY112/ppt/112-pp30.pdf
- Wrangellia Terrane: http://www.eos.ubc.ca/research/wrangellia/background.html
- MIT Field Geology of Western US: http://ocw.mit.edu/courses/earth-atmospheric-and-planetary-sciences/12-114-field-geology-i-fall-2005/lecture-notes/
- Terranes Explained: http://www.virtualmuseum.ca/sgc-cms/expositions-exhibitions/logan/en/index.php?/md/research/platetectonics/TerraneExplained
- Western North American Orogenies: http://www.nsm.buffalo.edu/courses/gly481-581/WC_Intro.pdf
- History of the Western US: http://pages.uoregon.edu/ghump/Lectures_files/_wUS_history.pdf
- Orogeny Illustrations: https://www2.nau.edu/rcb7/geology_illustrated.html
- Paleogeographic and Tectonic History of Western North America: http://cpgeosystems.com/wnampalgeog.html
Looks pretty good