List of large volume volcanic eruptions in the Basin and Range Province
Large volume volcanic eruptions in the Basin and Range Province include Basin and Range eruptions in Utah, California, Idaho, Colorado, New Mexico, Texas, Arizona, Nevada, Wyoming and Oregon, as well as those of the Long Valley Caldera geological province and the Yellowstone hotspot.
Volcanic fields
editSome of the volcanic fields within the Basin and Range Province: Northwestern Nevada, the Modoc Plateau, Central Nevada, the Great Basin, Southwestern Nevada, the Mojave Desert, and the Long Valley Caldera region. Named ones include: Coso Volcanic Field, Mono Lake Volcanic Field, Marysvale Volcanic Field, San Juan volcanic field, Indian Peak, Central Colorado volcanic field, Jemez volcanic lineament, Mogollon-Datil volcanic field, Santa Rosa-Calico, and Boot Heel volcanic field.
Geological features
editMany geological features in Western United States have a Northeastern orientation, the North American craton motion has the same orientation as well.[1] For example: the Trans-Challis fault zone, Idaho; the Snake River in Oregon; the Garlock Fault, California; the Colorado River in Utah; the Colorado Mineral Belt; Crater Flat-Reveille Range-Lunar Crater lineament, the Northwestern Nevada volcanic field; the San Juan caldera cluster, Colorado; the Socorro-Magdalena caldera cluster, New Mexico; Jemez Lineament; and the Yellowstone hotspot trail. But the Yellowstone hotspot trail was modified through faults and extension.
Geology
editPrior to the Eocene Epoch (55.8 ± 0.2 to 33.9 ± 0.1 Ma) the convergence rate of the Farallon and North American Plates was fast and the angle of subduction was shallow. During the Eocene the Farallon Plate subduction-associated compressive forces of the Laramide orogeny ended, plate interactions changed from orthogonal compression to oblique strike-slip, and volcanism in the Basin and Range Province flared up. It is suggested that this plate continued to be underthrust until about 19 Ma, at which time it was completely consumed and volcanic activity ceased, in part. Olivine basalt from the oceanic ridge erupted around 17 Ma and extension began.[2][3][4][5][6] The extension resulted in roughly north-south-trending faults, the Great Basin, the Walker trough, the Owens graben, and the Rio Grande rift, for instance.
List of large volume eruptions in the Basin and Range Province
editThe large volume eruptions in the Basin and Range Province include:
- Long Valley Caldera; Mono County, California, USA; 758.9 ± 1.8 ka; VEI 7; 600 km3 (140 cu mi) of Bishop Tuff.[7][8]
- Valles Caldera, New Mexico, USA; around 1.15 Ma; VEI 7; around 600 km3 (140 cu mi) of the Tshirege formation, Upper Bandelier eruption.[8][9][10]
- Valles Caldera, New Mexico, USA; around 1.47 Ma (Lower Bandelier eruption, the Otawi).[8][9][11][12]
- Yellowstone hotspot (?), Lake Owyhee volcanic fields; 15.0 to 15.5 Ma.[13]
- Yellowstone hotspot (?), Northwest Nevada volcanic field, Virgin Valley, High Rock, Hog Ranch, and unnamed calderas; West of the Pine Forest Range, Nevada; 15.5 to 16.5 Ma; Tuffs: Idaho Canyon, Ashdown, Summit Lake, and Soldier Meadow.[14][15][16][17][18]
- Columbia River Basalt Province: Yellowstone hotspot releases a huge pulse of volcanic activity, the first eruptions were near the Oregon-Idaho-Washington border. Columbia River and Steens flood basalts, Pueblo Mountains, Steens Mountain, Washington, Oregon, and Idaho; most vigorous eruptions were from 14 to 17 Ma.[8]
- Columbia River flood basalts, 175,000 km3 (42,000 cu mi)[19][20][21]
- Steens flood basalts, 65,000 km3 (16,000 cu mi)[19][22][23]
- Mount Belknap Caldera (17 km × 12 km (10.6 mi × 7.5 mi)), Marysvale Volcanic Field, southwestern Utah; 19 Ma; 150 km3 (36 cu mi) of tephra (Joe Lott member).[8][24]
- Big John Caldera (10 km × 6 km (6.2 mi × 3.7 mi)), Marysvale Volcanic Field, southwestern Utah; 22 Ma; 50 km3 (12 cu mi) of Delano Peak Tuff member.[8]
- Monroe Peak Caldera (20 km × 16 km (12.4 mi × 9.9 mi)), Marysvale Volcanic Field, southwestern Utah; 23 Ma; 200 km3 (48 cu mi) of Osiris Tuff.[8][24]
- Lake City calderas (20 km (12 mi) wide), San Juan volcanic field, Colorado; 23.1 Ma; 300 km3 (72 cu mi) of Sunshine Peak Tuff.[8][25][26]
- Turkey Creek Caldera (25 km (16 mi) wide), Chiricahua National Monument, Arizona; 25 Ma; 500 km3 (120 cu mi) of Rhyolite Canyon Formation.[8][27]
- Lake City calderas (25 km (16 mi) wide), San Juan volcanic field, Colorado; 25.9 Ma; 200 to 500 km3 (48 to 120 cu mi) of tephra.[8][28]
- Questa Caldera (15 km (9.3 mi) wide), Questa-Latir volcanic locus, Questa, New Mexico; 26 Ma, 400 km3 (96 cu mi) of Amalia Tuff.[8][24]
- Creede Caldera (24 km (15 mi) wide), San Juan Mountains, Wheeler Geologic Area, San Juan volcanic field, Colorado; 26.7 Ma; less than 500 km3 (120 cu mi) of Snowshoe Mountain Tuff.[28][29]
- San Luis caldera complex (18 km (11 mi) wide), Wheeler Geologic Area, San Juan volcanic field, Colorado; 26.8 Ma, 562 km3 (135 cu mi) of Nelson Mountain Tuff.[8][28]
- San Luis caldera complex (18 km (11 mi) wide), Wheeler Geologic Area, San Juan volcanic field, Colorado; 26.9 Ma, 250 km3 (60 cu mi) of Cebola Creek Tuff.[28]
- San Luis caldera complex (18 km (11 mi) wide), Wheeler Geologic Area, San Juan volcanic field, Colorado; 27 Ma, 150 km3 (36 cu mi) of Rat Creek Tuff.[8][28]
- Three Creeks Caldera (8 km (5.0 mi) wide), Marysvale Volcanic Field, Cove Fort-Sulphurdale area, southwestern Utah; 27 Ma; 100 to 200 km3 (24 to 48 cu mi) of Three Creeks Tuff Member of the Bullion Canyon Volcanics.[8][24]
- South River Caldera, Wheeler Geologic Area, San Juan volcanic field, Colorado; 27.1 Ma, more than 500 km3 (120 cu mi) of Wason Park Tuff.[8][28]
- Central San Juan Caldera (concealed), San Juan volcanic field, Colorado; 27.2 Ma, 250 km3 (60 cu mi) of Blue Creek Tuff.[8][28]
- Bachelor Caldera (20 km × 28 km (12 mi × 17 mi)), Wheeler Geologic Area, San Juan volcanic field, Colorado; 27.35 Ma; 1,200 km3 (290 cu mi) of Carpenter Ridge Tuff.[29]
- Silverton Caldera (20 km (12 mi) wide), San Juan volcanic field, Colorado; 27.6 Ma, 50 to 100 km3 (12 to 24 cu mi) of Crystal Lake Tuff.[8][28]
- La Garita Caldera (100 km × 35 km (62 mi × 22 mi)), Wheeler Geologic Area, San Juan volcanic field, Colorado; VEI 8; more than 5,000 km3 (1,200 cu mi) of Fish Canyon Tuff was blasted out in a major single eruption about 27.8 Ma.[29][30][31]
- San Juan Caldera (22 km × 24 km (14 mi × 15 mi)), San Juan volcanic field, Colorado; 28 Ma; more than 1,000 km3 (240 cu mi) of Sapinero Mesa Tuff.[8]
- Uncompahgre Caldera (23 km × 20 km (14 mi × 12 mi)), Uncompahgre National Forest, San Juan volcanic field, Colorado; 28.1 Ma; more than 1,000 km3 (240 cu mi) of Dillon/Sapinero Mesa Tuffs.[8][32]
- Lost Lake Caldera (10 km (6.2 mi) wide), San Juan volcanic field, Colorado; 28.2 Ma, 100 to 500 km3 (24 to 120 cu mi) of Blue Mesa Tuff.[8]
- Platoro calderas, San Juan volcanic field, Platoro, Conejos County, Colorado; 28.2 Ma; 1,000 km3 (240 cu mi) of Chiquito Peak Tuff.[8]
- Central San Juan Caldera (concealed), San Juan volcanic field, Colorado; 28.3 Ma; 500 km3 (120 cu mi) of Masonic Park Tuff.[8][28]
- Ute Creek Caldera, Central Colorado volcanic field, Colorado; 28.3 Ma; 500 km3 (120 cu mi) of Ute Ridge Tuff.[8][33]
Caldera name | State (volcanic field) | age | size |
---|---|---|---|
Black Mountain Caldera (18 km wide) | Nevada (SWNVF) | 7 Ma ±1 | 300 km3 (72 cu mi) of Thirsty Canyon Tuff.[8][24] |
Timber Mountain caldera complex (30 km × 25 km (19 mi × 16 mi)) | Nevada (SWNVF) | 11.45 Ma | 900 km3 (220 cu mi) of Timber Mountain Tuff – Ammonia Tanks member.[8][34] |
Timber Mountain caldera complex | Nevada (SWNVF) | 11.6 Ma | 1,200 km3 (290 cu mi) of Timber Mountain Tuff – Rainer Mesa member.[8][34] |
Paintbrush Caldera (20 km (12 mi) wide) | Nevada (SWNVF) | 12.7 Ma | 1,000 km3 (240 cu mi) of Paintbrush Tuff – Topopah Spring member.[8][34] |
Paintbrush Caldera | Nevada (SWNVF) | 12.8 Ma | 1,200 km3 (288 cu mi) of Paintbrush Tuff – Tiva Canyon member[8][34] |
Silent Canyon Caldera (20 km × 16 km (12.4 mi × 9.9 mi)) | Nevada (SWNVF) | 13 Ma | 200 km3 (48 cu mi).[8][24] |
Crater Flat Group | Nevada (SWNVF) | 13.25 Ma | 650 km3 (156 cu mi) of Belted Range Tuff[8] |
List of Rupelian calderas
editThe Rupelian age/stage (Paleogene period/system, Oligocene epoch/series) spans the time between 33.9 ±0.1 Ma and 28.4 ±0.1 Ma (million years ago).
- Bursum Caldera (size: 40 x 30 km), Mogollon-Datil volcanic field, New Mexico; 28.5 Ma ±0.5; 1,050 cubic kilometres (250 cu mi) of Bloodgood Canyon Tuff.[8][35]
- Bursum Caldera (size: 40 x 30 km), Mogollon-Datil volcanic field, New Mexico; 28.5 Ma ±0.5; 1,200 cubic kilometres (290 cu mi) of Apache Springs Tuff.[8][35]
- San Juan Caldera (size: 24 x 22 km), San Juan volcanic field, Colorado; 28.5 Ma; 900 cubic kilometres (220 cu mi) of tephra.[8][32]
- Summitville Caldera (size: 12 x 8 km), San Juan volcanic field, Colorado; 28.5 Ma; 100 to 500 cubic kilometers (24 to 120 cu mi) of Ojito Creek/ La Jadero Tuffs.[8][36][37]
- Mount Hope (size: 15 km), San Juan volcanic field, Colorado; 29 Ma; 500 cubic kilometres (120 cu mi) of Masonic Park Tuff.[8][25]
- Around White Rock caldera (size: 50 km North-South), White Rock Mountains, Great Basin, Nevada; 29.02 Ma ±0.04; 2,600 cubic kilometres (620 cu mi) of Lund Tuff.[8][38]
- Ute Creek (size: 8 km wide), San Juan volcanic field, Colorado; 29 Ma; 500 cubic kilometres (120 cu mi) of Ute Ridge Tuff.[8][25]
- Platoro calderas (size: 12 x 18 km), San Juan volcanic field, Platoro, Conejos County, Colorado; 29.5 Ma; 500 cubic kilometers (120 cu mi) of Black Mountain Tuff.[8][36][37]
- Indian Peak, Eastern Nevada; 29.5 Ma; more than 3,200 cubic kilometers (768 cu mi) of Wah Wah Springs Tuff.[8][39]
- Platoro calderas (size: 18 x 22 km), San Juan volcanic field, Platoro, Conejos County, Colorado; 30 Ma; 592 cubic kilometers (142 cu mi) of La Jara Canyon Tuff.[8][29][36]
- Goodsight-Cedar Hills volcano-tectonic depression (Bell Top Formation), south-central New Mexico; 30.5 Ma ±1.5, 295 cubic kilometres (71 cu mi) of tephra (Bell Top Formation).[8][40]
- William's Ridge, Central Nevada; 31.4 Ma; 3,500 cubic kilometres (840 cu mi) of Windous Butte Tuff.[8][41]
- North Pass Caldera, Cochetopa Hills, Central Colorado volcanic field; 32.25 Ma; 400 to 500 cubic kilometers (96 to 120 cu mi) of Saguache Creek Tuff.[8][42]
- Organ Caldera (size: 16 km wide), Organ Mountains, New Mexico; 32 Ma, 500 cubic kilometres (120 cu mi) of Cueva Soledad Rhyolite.[8][40]
- Chinati Caldera (size: 30 x 20 km), Chinati Mountains, Texas; 32.5 Ma ±0.5, 1,000 cubic kilometres (240 cu mi) of Mitchel Mesa Rhyolite.[8][43]
- Bonanza (size: 12 km wide), Central Colorado volcanic field; Colorado; 32.5 Ma, more than 100 cubic kilometres (24 cu mi) of Bonanza Tuff.[8][44]
- Cowboy Rim (size: 26 x 18 km), Animas Mountains, Hidalgo County, New Mexico; 33 Ma, 500 cubic kilometres (120 cu mi) of Gillespie Tuff.[8][45]
- Emory Caldera (size: 25 x 55 km), Mogollon-Datil volcanic field, City of Rocks State Park; 33 Ma; VEI 8; 1,310 cubic kilometers (314 cu mi) of Kneeling Nun Tuff.[8][46][47][48][49]
- Socorro Caldera (size: 25 x 35 km), Rio Grande rift, Socorro, New Mexico; 33 Ma, 500 cubic kilometres (120 cu mi) of Hells Mesa Rhyolite.[8][29][50]
- Marshall Creek, Thirtynine Mile volcanic area, Central Colorado volcanic field; Colorado; 33.7 Ma; more than 100 cubic kilometres (24 cu mi) of Thorn Ranch Tuff.[8][51]
- Mount Aetna (size: 10 km wide), Central Colorado volcanic field; Colorado; 33.81 Ma, 100 cubic kilometres (24 cu mi) of Badger Creek Tuff.[8][52]
- Grizzly Peak Caldera (size: 12 km wide), Central Colorado volcanic field; Colorado; 34.31 Ma; 100 cubic kilometres (24 cu mi) of Grizzly Peak Rhyolite.[8][52]
- Juniper Caldera (size: 25 km), Animas Mountains, Hidalgo County, New Mexico; 35 Ma; 500 cubic kilometres (120 cu mi) of Oak Creek Tuff.[8][45]
- Mount Princeton (eroded), Central Colorado volcanic field; Colorado; 35.3 Ma ±0.6; more than 1,000 cubic kilometres (240 cu mi) of Wall Mountain Tuff.[8][44][53]
- Davis Mountains, Texas; 35.35 Ma ±0.6; 210 cubic kilometres (50 cu mi) of tuffs of Wild Cherry, Lavas of Casket Mountain.[8][54]
- Davis Mountains, Texas; 35.61 Ma ±0.09; 200 cubic kilometres (48 cu mi) of Barrel Springs Formation and ash flow tuff.[8][54]
- Quitman Caldera (size: 15 x 10 km), Quitman Mountains, Hudspeth County, Texas; 36 Ma; 300 cubic kilometres (72 cu mi) of Square Peak Volcanics.[8][24]
- Davis Mountains, Texas; 36.2 Ma ±0.6; 300 cubic kilometres (72 cu mi) of Mafic lavas.[8][54]
- Davis Mountains, Texas; 36.33 Ma ±0.13; 150 cubic kilometres (36 cu mi) of tephra (Paisano Volcano).[8][54]
- Davis Mountains, Texas; 36.51 Ma ±0.05; 210 cubic kilometres (50 cu mi) of Adobe Canyon and Limpia Formations.[8][54]
- Davis Mountains (fissures), Texas; 36.82 Ma ±0.08; 1,250 cubic kilometres (300 cu mi) of Flood rhyolites, rhyolite domes, and Gomez Tuff.[8][54]
- Muir Caldera (size: 26 x 18 km wide), Hidalgo County, New Mexico; 37 Ma; 300 cubic kilometres (72 cu mi) of Woodhaul Canyon tephra.[8][24][55]
- Infernito Caldera (size: 12 km wide), Trans-Pecos, Texas; 37.5 Ma ±0.5; 70 to 100 cubic kilometers (17 to 24 cu mi) of Buckshot Tuff.[8][24]
- Thomas Caldera (size: 16 x 25 km wide), Delta, Utah; 39 Ma; 400 cubic kilometres (96 cu mi) of Mount Laird Tuff.[8][24]
- Twin Peaks Caldera (size: 20 km), Challis volcanic field, Custer, Idaho; 45 Ma, 500 cubic kilometres (120 cu mi) of Challis Creek Tuff.[8][56]
- Van Horn cauldron complex (size: 34 x 48 km), Challis volcanic field, Custer, Idaho; 46 Ma ±0.6; unknown amount of Elis Creek Tuff.[8][57]
- Silver Bell Caldera (size: 8 km wide), Arizona; 55.8 Ma; unknown amount of Mount Laird Tuff.[8][58]
- Silver Bell Caldera (size: 8 km wide), Arizona; 68 Ma; 150 cubic kilometres (36 cu mi) of Lithic Tuff.[8][24]
- Tucson Mountain Caldera (size: 25 km wide), Tucson Mountains, Arizona; 73 Ma; 500 cubic kilometres (120 cu mi) of Cat Mountain Tuff.[8][28][59]
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- Korringa, Marjorie K. (December 1973). "Linear vent area of the Soldier Meadow Tuff, an ash-flow sheet in northwestern Nevada". Geological Society of America Bulletin. 84 (12): 3849–3866. Bibcode:1973GSAB...84.3849K. doi:10.1130/0016-7606(1973)84<3849:LVAOTS>2.0.CO;2.
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- Maughan, Larissa L.; Christiansen, Eric H.; Best, Myron G.; Grommé, C. Sherman; Deino, Alan L.; Tingey, David G. (2002). "The Oligocene Lund Tuff, Great Basin, USA: a very large volume monotonous intermediate". J. Volcanol. Geotherm. Res. 113 (1–2): 129–157. Bibcode:2002JVGR..113..129M. doi:10.1016/s0377-0273(01)00256-6. Retrieved 2010-04-01.
- McIntosh, W.C. & Chapin, C.E. (2004). "Geochronology of the central Colorado volcanic field". Bull. New Mexico Bur. Geol. Min. Res. 160: 205–237.
- McKee, E. H. (1971). "Tertiary Igneous Chronology of the Great Basin of Western United States–Implications for Tectonic Models". Geological Society of America Bulletin. 82 (12): 3497–3502. Bibcode:1971GSAB...82.3497M. doi:10.1130/0016-7606(1971)82[3497:ticotg]2.0.co;2. Retrieved 2010-04-09.
- Morgan, L.A.; Doherty, D.J.; Leeman, W.P. (1984). "Ignimbrites of the Eastern Snake River Plain: evidence for major caldera-forming eruptions". J. Geophys. Res. 89 (B10): 8665–8678. Bibcode:1984JGR....89.8665M. doi:10.1029/JB089iB10p08665.
- Moye, F.J.; Hackett, W.R.; Blakley, J.D.; Snider, L.G. (1988). "Regional geologic setting and volcanic stratigraphy of the Challis Volcanic Field, Central Idaho". Idaho Geological Survey Bulletin. 27: 87–97.
- Noble, D.C. (1988), "Cenozoic volcanic rocks of the northwestern Great Basin: an overview", Spring Field Trip Guidebook, Special Publication No. 7, Geological Society of Nevada, pp. 31–42
- Osburn, G.R. & Chapin, C.E. (1983). "Ash-flow tuffs and cauldrons in the northeast Mogollon-Datil volcanic field: A summary". Field Conference Guide of the New Mexico Geological Society. 34: 197–204.
- Min, K.; Reiners, P.W.; Nicolescu, S.; Wolff, J.A.; Mundil, R.; Winters, L.R. (2004). "(U-Th)/He dating of volcanic phenocrysts with high-(U-Th) inclusions, Bandelier Tuff, New Mexico". Eos, Transactions, American Geophysical Union. 85 (Abstract V43E–1450): V43E–1450. Bibcode:2004AGUFM.V43E1450M.
- Sawyer, David A.; R. J. Fleck; M. A. Lanphere; R. G. Warren; D. E. Broxton & Mark R. Hudson (October 1994). "Episodic caldera volcanism in the Miocene southwestern Nevada volcanic field: Revised stratigraphic framework, 40Ar/39Ar geochronology, and implications for magmatism and extension". Geological Society of America Bulletin. 106 (10): 1304–1318. Bibcode:1994GSAB..106.1304S. doi:10.1130/0016-7606(1994)106<1304:ECVITM>2.3.CO;2. Retrieved 2010-03-26.
- Ratté, J.C.; Marvin, R.F.; Naeser, C.W. (1984). "Calderas and ash flow tuffs of the Mogollan Mountains, southwestern New Mexico". J. Geophys. Res. 89 (B10): 8713–8732. Bibcode:1984JGR....89.8713R. doi:10.1029/JB089iB10p08713.
- Rytuba, James J.; John, David A.; McKee, Edwin H. (May 3–5, 2004). "Volcanism Associated with Eruption of the Steens Basalt and Inception of the Yellowstone Hotspot". The Geological Society of America (Abstract). Archived from the original on 2010-12-23. Retrieved 2010-03-26.
- Sarna-Wojcicki, A.M.; Pringle, M.S.; Wijbrans, J. (2000). "New 40Ar/39Ar age of the Bishop Tuff from multiple sites and sediment rate calibration for the Matuyama-Brunhes boundary". J. Geophys. Res. 105 (B9): 21431–21443. Bibcode:2000JGR...10521431S. doi:10.1029/2000JB900901.
- Seager, W.R. (1973). "Resurgent volcano-tectonic depression of Oligocene age, south-central New Mexico". Bull. Geol. Soc. Am. 84 (11): 3611–3626. Bibcode:1973GSAB...84.3611S. doi:10.1130/0016-7606(1973)84<3611:rvdooa>2.0.co;2.
- Seager, W.R. (1981). "Geology of Oregon Mountains and southern San Andreas Mountains, New Mexico". Memoir of the New Mexico Bureau of Mineral Resources. 36: 1–97.
- Sigurdsson, H. (2000), "Volcanic episodes and rates of volcanism", in Sigurdsson, H. (ed.), Encyclopedia of volcanoes, San Diego: Academic Press, pp. 271–279
- Smith, R.L. & Luedke, R.G. (1984). "Potentially active volcanic lineaments and loci in western conterminous United States". Explosive Volcanism: Inception, Evolution, and Hazard. National Research Council, Geophysics Study Committee. pp. 47–66. ISBN 978-0-309-03393-0.
- Steven, T.A. & Ratte, J.C. (1965). "Geology and structural control of ore deposition in the Creede district, San Juan Mountains, Colorado". USGS Professional Paper. 487: 90. Bibcode:1965usgs.rept...10S. doi:10.3133/pp487.
- Varga, R.J. & Smith, B.M. (1984). "Evolution of the early oligocene Bonanza caldera, northeast San Juan volcanic field, Colorado". J. Geophys. Res. 89 (B10): 8679–8694. Bibcode:1984JGR....89.8679V. doi:10.1029/JB089iB10p08679.
- Ward, Peter L. (2 April 2009). "Sulfur Dioxide Initiates Global Climate Change in Four Ways" (PDF). Thin Solid Films. 517 (11): 3188–3203. Bibcode:2009TSF...517.3188W. doi:10.1016/j.tsf.2009.01.005. Archived from the original (PDF) on 20 January 2010. Retrieved 2010-03-19.
- "Supplementary Table to P.L. Ward, Thin Solid Films (2009) Major volcanic eruptions and provinces" (PDF). Teton Tectonics. Archived from the original (PDF) on 2010-01-20. Retrieved 2010-03-16.
- "Supplementary References to P.L. Ward, Thin Solid Films (2009)" (PDF). Teton Tectonics. Archived from the original (PDF) on 2010-01-20. Retrieved 2010-03-16.
Columbia River Basalt Province-sources
edit- Brueseke, M.E.; Heizler, M.T.; Hart, W.K. & S.A. Mertzman (15 March 2007). "Distribution and geochronology of Oregon Plateau (U.S.A.) flood basalt volcanism: The Steens Basalt revisited". Journal of Volcanology and Geothermal Research. 161 (3): 187–214. Bibcode:2007JVGR..161..187B. doi:10.1016/j.jvolgeores.2006.12.004.
- Camp, V.E. & Ross, M.E. (2000). "Mapping the Steens-Columbia River Basalt Connection: Implications for the extent, volume, and magma supply rate of CRB volcanism". Geol. Soc. Am. Abstr. Programs. 32: A159.
- Carson, Robert J.; Pogue, Kevin R. (1996). Flood Basalts and Glacier Floods:Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington. Washington State Department of Natural Resources (Washington Division of Geology and Earth Resources Information Circular 90). ISBN none.
- Jarboe, N.A.; Coe, R.S.; Renne, P.R.; Glen, J.M. (2006). "40Ar/39Ar ages of the Early Columbia River Basalt Group: Determining the Steens Mountain Geomagnetic Polarity Reversal (R0-N0) as the top of the C5Cr Chron and the Imnaha Normal (N0) as the C5Cn.3n Chron". Eos, Transactions, American Geophysical Union. 87 (Abstract V51D–1702): V51D–1702. Bibcode:2006AGUFM.V51D1702J.
- Camp, Victor E.; Martin E. Ross; William E. Hanson (January 2003). "Genesis of flood basalts and Basin and Range volcanic rocks from Steens Mountain to the Malheur River Gorge, Oregon". Geological Society of America Bulletin. 115 (1): 105–128. Bibcode:2003GSAB..115..105C. doi:10.1130/0016-7606(2003)115<0105:gofbab>2.0.co;2. Retrieved 2010-03-30.
- Reidel, Stephen P. (January 2005). A Lava Flow without a Source: The Cohasset Flow and Its Compositional Members. The Journal of Geology, Volume 113, Pp 1 – 21. ISBN none.
- Web citations:
- "Southeast Oregon Basin and Range". SummitPost.org. Retrieved 2010-03-30.
- "Andesitic and basaltic rocks on Steens Mountain". USGS. Retrieved 2010-03-30.
- "Oregon: A Geologic History. 8. Columbia River Basalt: the Yellowstone hot spot arrives in a flood of fire". Oregon Department of Geology and Mineral Industries. Retrieved 2010-03-26.
Peter W. Lipman – sources
edit- Lipman, Peter W. (1969). "Alkalic and tholeiitic basaltic volcanism related to the Rio Grande Depression, Southern Colorado and Northern New Mexico". Geological Society of America Bulletin. 80 (7): 1343–1354. Bibcode:1969GSAB...80.1343L. doi:10.1130/0016-7606(1969)80[1343:aatbvr]2.0.co;2.
- Lipman, Peter W.; Prostka, H.J.; Christiansen, R.L. (1972). "Cenozoic volcanism and plate-tectonic evolution of the Western United States: I. Early and middle Cenozoic". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 271 (1213): 217–248. Bibcode:1972RSPTA.271..217L. doi:10.1098/rsta.1972.0008. JSTOR 74007. S2CID 91504527.
- R. L. Christiansen & P. W. Lipman (1972). "Cenozoic Volcanism and Plate-Tectonic Evolution of the Western United States. II. Late Cenozoic". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 271 (1213): 249–284. Bibcode:1972RSPTA.271..249C. doi:10.1098/rsta.1972.0009. JSTOR 74008. S2CID 91755783.
- Lipman, Peter W.; Steven, T.A.; Luedke, R.G.; Burbank, W.S. (1973). "Revised volcanic history of the San Juan, Uncompahgre, Silverton, and Lake City calderas in the western San Juan Mountains, Colorado". J. Res. U. S. Geol. Surv. 1: 627–642.
- Lipman, Peter W. (1975). "Evolution of the Platoro caldera complex and related volcanic rocks, southeastern San Juan Mountains, Colorado". USGS Professional Paper. 852: 1–128. Bibcode:1975usgs.rept....5L.
- Lipman, Peter W. (1976). "Caldera-collapse breccias in the western San Juan Mountains, Colorado". Geol. Soc. Am. Bull. 87 (10): 1397–1410. Bibcode:1976GSAB...87.1397L. doi:10.1130/0016-7606(1976)87<1397:cbitws>2.0.co;2.
- Steven, T.A. & Lipman, Peter W. (1976). "Calderas of the San Juan volcanic field, southwestern Colorado". USGS Professional Paper. 958: 35.
- Lipman, Peter W. & Mehnert, H.H. (1979), "The Taos Plateau volcanic field, northern Rio Grande rift, New Mexico", in Riecker, R.E. (ed.), Rio Grande rift – Tectonics and magmatism, Washington, D.C.: American Geophysical Union, pp. 289–311
- Sawyer, D.A. & Lipman, Peter W. (1983). "Silver Bell Mountains, Arizona- porphyry copper mineralization in a late Cretaceous caldera". Eos, Transactions, American Geophysical Union. 64: 874.
- Lipman, Peter W. (September 30, 1984). "The Roots of Ash Flow Calderas in Western North America: Windows Into the Tops of Granitic Batholiths" (PDF). Journal of Geophysical Research. 89 (B10): 8801–8841. Bibcode:1984JGR....89.8801L. doi:10.1029/JB089iB10p08801. Retrieved 2010-04-27.
- Lipman, Peter W.; Mehnert, H.H.; Naeser, C.W (1986). "Evolution of the Latir volcanic field, northern New Mexico, and its relation to the Rio Grande rift, as indicated by potassium-argon and fission track dating". Journal of Geophysical Research. 91 (B6): 6329–6345. Bibcode:1986JGR....91.6329L. doi:10.1029/JB091iB06p06329.
- Thompson, R.A.; Dungan, M.A.; Lipman, Peter W. (1986). "Multiple differentiation processes in early-rift calc-alkaline volcanics, northern Rio Grande rift, New Mexico". Journal of Geophysical Research. 91 (B6): 6046–6058. Bibcode:1986JGR....91.6046T. doi:10.1029/JB091iB06p06046.
- Lipman, Peter W. & Reed, J.C. Jr. (1989). "Geologic map of the Latir volcanic field and adjacent areas, northern New Mexico". U.S. Geological Survey Miscellaneous Investigations Series. Map I-1907 (Scale 1:48000): 16. Bibcode:1989usgs.rept...16L. doi:10.3133/i1907.
- Hon, K. & Lipman, Peter W. (1989), "Western San Juan caldera complex", in Lipman, Peter W. (ed.), Excursion 16B: Oligocene-Miocene San Juan volcanic field, Colorado, vol. 46, New Mexico Bureau of Mines and Mineral Resources Memoir, pp. 350–380
- Lipman, Peter W. & W. S. Baldridge (1990), "Taos, New Mexico", in C. A. Wood & J. Kienle (eds.), Volcanoes of North America, Cambridge University Press, pp. 290–292
- Lipman, Peter W. & Glazner, Allen F. (1991), "Introduction to middle Tertiary Cordilleran volcanism—Magma sources and relations to regional tectonics", Journal of Geophysical Research, 96 (B8): 13193–13199, Bibcode:1991JGR....9613193L, doi:10.1029/91JB01397
- Lipman, Peter W.; Dungan, M.A.; Brown, L.L.; Deino, A.L. (1996). "Recurrent eruption and subsidence at the Platoro Caldera complex, southeastern San Juan volcanic field, Colorado; new tales from old tuffs". Geol. Soc. Am. Bull. 108 (8): 1039–1055. Bibcode:1996GSAB..108.1039L. doi:10.1130/0016-7606(1996)108<1039:reasat>2.3.co;2.
- Lipman, Peter W. (2000), "Calderas", in Sigurdsson, H. (ed.), Encyclopedia of volcanoes, San Diego: Academic Press, pp. 643–662, ISBN 978-0-12-643140-7
- Olivier Bachmann; Michael A. Dungan; Peter W. Lipman (2002). "The Fish Canyon Magma Body, San Juan Volcanic Field, Colorado: Rejuvenation and Eruption of an Upper-Crustal Batholith". Journal of Petrology. 43 (8): 1469–1503. Bibcode:2002JPet...43.1469B. doi:10.1093/petrology/43.8.1469.
- Lipman, Peter W. & Calvert, A. (2003). "Southward migration of mid-Tertiary volcanism: Relations in the Cochetopa Area, North-Central San Juan Mountains, Colorado". Geol. Soc. Am. Abstr. Programs. 35: 14.
- Peter W. Lipman; William C. McIntosh (July 2008). "Eruptive and noneruptive calderas, northeastern San Juan Mountains, Colorado: Where did the ignimbrites come from?". Geological Society of America Bulletin. 120 (7–8): 771–795. Bibcode:2008GSAB..120..771L. doi:10.1130/B26330.1.
Maps
edit- Overview map at Basin and Range Province.
- Map of the Basin and Range Province
- Map: Thelin and Pike (1991), Landforms of the conterminous United States – A digital shaded-relief portrayal, USGS Map I-2206
- Global Positioning System (GPS) Time Series
- Great Basin/Nevada
- Steve Ludington; Dennis P. Cox; Kenneth W. Leonard & Barry C. Moring (1996), "Chapter 5, Cenozoic Volcanic Geology in Nevada", in Donald A. Singer (ed.), An Analysis of Nevada's Metal-Bearing Mineral Resources, Nevada Bureau of Mines and Geology, University of Nevada, retrieved 2010-03-23
- Potter, Christopher J.; Dickerson, Robert P.; Sweetkind, Donald S.; Drake, Ronald M. II; Taylor, Emily M.; Fridrich, Christopher J.; San, Carma A. Juan; Day, Warren C. (2002). Geologic map of the Yucca Mountain region, Nye County, Nevada: U.S. Geological Survey Geologic Investigations Series. Vol. I-2755. Denver, Colorado: U.S. Geological Survey. Retrieved 2010-05-02.
- Matthew E. Brueseke & William K. Hart (2008). Geology and Petrology of the Mid-Miocene Santa Rosa-Calico Volcanic Field, northern Nevada (PDF). Reno, Nevada: Mackay School of Earth Sciences and Engineering College of Science, University of Nevada. Archived from the original (PDF) on 2010-06-07. Retrieved 2010-05-04.
- Supplemental material: Columbia River Basalt Group, eruptive loci
- Great Basin/Utah
- Rowley, Peter D.; Cunningham, Charles G.; Steven, Thomas A.; Workman, Jeremiah B.; Anderson, John J.; Theissen, Kevin M. (2002). Geologic Map of the Central Marysvale Volcanic Field, Southwestern Utah: U.S. Geological Survey Geologic Investigations Series. Vol. I-2645-A. Denver, Colorado: U. S. Geological Survey. Retrieved 2010-05-02.
- Colorado
- William C. McIntosh & Charles E. Chapin (2004). "Geochronology of the central Colorado volcanic field". Tectonics, geochronology, and volcanism in the Southern Rocky Mountains and Rio Grande rift (PDF). Socorro, NM: New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology. pp. 205–238. Archived from the original (PDF) on 2010-06-09. Retrieved 2010-04-01.
- Robinson, Joel E.; Dillon R. Dutton; David W. Ramsey; Peter W. Lipman; Tracey J. Felger (2006). Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado: Geologic Investigations Series. Vol. I-2799. U.S. Geological Survey. Retrieved 2010-05-03.
- New Mexico
- "The Taos Plateau Volcanic Field". New Mexico Museum of Natural History and Science. Retrieved 2010-04-01.
- Crumpler, L. S. & Lucas, S. G. (2001). "Volcanoes of New Mexico: An Abbreviated Guide For Non-Specialists" (PDF). Volcanology in New Mexico. New Mexico Museum of Natural History and Science Bulletin. 18: 5–15. Archived from the original (PDF) on 2007-03-21. Retrieved 2010-04-28.
- Mogollon-Datil volcanic field
- "Gila Cliff Dwellings National Monument". New Mexico Bureau of Geology & Mineral Resources. Retrieved 2010-04-29. citing from Chapin, C.E.; McIntosh, W.C. & Chamberlin, R.M. (2004), "The Late Eocene—Oligocene peak of Cenozoic volcanism in southwestern New Mexico", in Mack, G.H. & Giles, K.A. (eds.), The Geology of New Mexico, a Geologic History, vol. 11, New Mexico Geological Society Special Publication, pp. 271–294