San Juan volcanic field

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San Juan volcanic field - Wikipedia

Coordinates: 37°53′36″N 106°46′28″W / 37.89333°N 106.77444°W

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San Juan volcanic field
San Juan volcanic field Location in Colorado
Highest point
Coordinates	37°53′36″N 106°46′28″W / 37.89333°N 106.77444°W / 37.89333; -106.77444
Geography
Location	Colorado, United States
Geology
Mountain type	Volcanic field

The San Juan volcanic field is part of the San Juan Mountains in southwestern Colorado. It consists mainly of volcanic rocks that form the largest remnant of a major composite volcanic field that covered most of the southern Rocky Mountains in the Middle Tertiary geologic time.^[1] There are approximately fifteen calderas known in the San Juan Volcanic Fields; however, it is possible that there are two or even three more in the region.^[1]

The region began with many composite volcanoes that became active between 35 and 40 million years ago, with peak activity in the time period around 35-30 million years ago.^[1] Around this time the activity began to include explosive ash-flow eruptions.^[2] Many of these volcanoes experienced caldera collapse, resulting in the fifteen to eighteen caldera volcanoes in the region today.^[1]

Phases of Volcanism

The San Juan volcanic field experienced two phases of volcanism.^[3]

The earlier volcanism took place during the Oligocene age of the Paleogene Period. It produced largely intermediate composition lavas and breccias, together with ash flow tuffs reflecting differentiation of the original magma.^[3] The precaldera intermediate volcanic rocks include the Conejos Formation in the southeastern part of the field.^[4] Intermediate volcanism did not cease with caldera eruptions, and included such voluminous intermediate volcanic rocks as the Huerto Andesite.^[5]

The later volcanism took place from Miocene to Pliocene in ages of the Neogene Period. It was characterized by bimodal volcanism, producing both low-silica alkaline flows and high-silica rhyolites. It is usually interpreted as a partial melt of the lower crust that was erupted onto the surface.^[3]

Notable calderas

Name	Associated tuff	Coordinates	Age
Lake City	Sunshine Peak Tuff	38°02′N 107°23′W / 38.03°N 107.38°W / 38.03; -107.38^[3]	22.93 ± 0.02 Ma^[6]
Creede Caldera	Snowshoe Mountain Tuff	37°46′N 106°56′W / 37.76°N 106.94°W / 37.76; -106.94^[7]	26.5 ± 0.3 Ma^[8]
Cochetopa	Nelson Mountain Tuff	38°12′N 106°45′W / 38.2°N 106.75°W / 38.2; -106.75^[7]	26.4 ± 0.5 Ma^[8]
San Luis	Cebolla Creek Tuff Rat Creek Tuff	38°01′N 107°58′W / 38.01°N 107.97°W / 38.01; -107.97^[8]	26.9 Ma^[8]
South River	Watson Park Tuff	37°40′N 106°56′W / 37.67°N 106.94°W / 37.67; -106.94^[8]	27.4? Ma^[8]
Bachelor	Carpenter Ridge Tuff	37°49′N 106°55′W / 37.82°N 106.91°W / 37.82; -106.91^[7]	27.45 ± 0.05 Ma^[8]
La Garita	Fish Canyon Tuff	37°46′N 106°56′W / 37.76°N 106.94°W / 37.76; -106.94^[7]	27.45 ± 0.05 Ma^[8]
Uncompahgre-San Juan	Sapinero Mesa Tuff	37°58′N 107°32′W / 37.96°N 107.53°W / 37.96; -107.53^[8]	27.5 ± 0.5 Ma^[8]
Platoro	Treasure Mountain Group^[9]	37°21′N 106°32′W / 37.35°N 106.53°W / 37.35; -106.53^[3]	28.4 Ma^[9]
Unknown	Masonic Park Tuff	37°42′N 106°41′W / 37.70°N 106.69°W / 37.70; -106.69^[3]	28.7 Ma^[10]
North Pass	Saguache Creek Tuff	38°12′N 106°32′W / 38.20°N 106.54°W / 38.20; -106.54^[8]	32.2 Ma^[8]
Bonanza^[11]	Bonanza Tuff	38°19′N 106°05′W / 38.32°N 106.08°W / 38.32; -106.08^[12]	33.12 ± 0.03 Ma
Marshall	Thorn Ranch Tuff	38°20′N 106°14′W / 38.34°N 106.23°W / 38.34; -106.23^[8]	33.6 ± 0.3 Ma^[8]

Economic Impact

The San Juan volcanic field has been a historically important mining district, producing lead, zinc, copper, gold, and silver. The ores were mostly deposited in and near calderas that experienced significant postcaldera activity. Ore veins were concentrated in fractures associated with caldera activity and in postcaldera intrusive bodies. The greatest mineralization took place near the youngest and most silicic intrusions of each caldera cycle.^[13]

References

^ ^a ^b ^c ^d Steven, Thomas A.; Lipman, Peter W. (1976). "Calderas of the San Juan Volcanic Field, Southwestern Colorado". U.S. Geological Survey Professional Papers. Washington, DC: U.S. Government Printing Office. 958: 1–35. Retrieved 2012-05-16.
^ Lipman, Peter W.; Steven, Thomas A.; Mehnert, Harald H. (1970-08-01). "Volcanic History of the San Juan Mountains, Colorado, as Indicated by Potassium–Argon Dating". Geological Society of America Bulletin. 81 (8): 2329–2352. Bibcode:1970GSAB...81.2329L. doi:10.1130/0016-7606(1970)81[2329:VHOTSJ]2.0.CO;2. ISSN 0016-7606.
^ ^a ^b ^c ^d ^e ^f Lipman, P.W.; Doe, B.R.; Hedge, C.E.; Steven, T.A. (1978). "Petrologic evolution of the San Juan volcanic field, southwestern Colorado: Pb and Sr isotope evidence". Geological Society of America Bulletin. 89 (1): 59–82. Bibcode:1978GSAB...89...59L. doi:10.1130/0016-7606(1978)89<59:PEOTSJ>2.0.CO;2. ISSN 0016-7606.
^ Colucci, M. T.; Dungan, M. A.; Ferguson, K. M.; Lipman, P. W.; Moorbath, S. (30 July 1991). "Precaldera lavas of the southeast San Juan Volcanic Field: Parent magmas and crustal interactions". Journal of Geophysical Research: Solid Earth. 96 (B8): 13413–13434. doi:10.1029/91JB00282.
^ Parat, Fleurice; Dungan, Michael A.; Lipman, Peter W. (1 May 2005). "Contemporaneous Trachyandesitic and Calc-alkaline Volcanism of the Huerto Andesite, San Juan Volcanic Field, Colorado, USA" (PDF). Journal of Petrology. 46 (5): 859–891. doi:10.1093/petrology/egi003.
^ Kennedy, Ben; Wilcock, Jack; Stix, John (October 2012). "Caldera resurgence during magma replenishment and rejuvenation at Valles and Lake City calderas". Bulletin of Volcanology. 74 (8): 1833–1847. doi:10.1007/s00445-012-0641-x.
^ ^a ^b ^c ^d 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.
^ ^a ^b ^c ^d ^e ^f ^g ^h ⁱ ^j ^k ^l ^m ⁿ Lipman, Peter W.; McIntosh, William C.; Zimmerer, Matthew J. (2013). "From ignimbrite to batholith, northeastern San Juan Mountains, ColoradoBonanza, Cochetopa Park, and North Pass calderas". Classic Concepts and New DirectionsExploring 125 Years of GSA Discoveries in the Rocky Mountain Region. doi:10.1130/2013.0033(14).
^ ^a ^b Lipman, Peter W.; Dungan, Michael A.; Brown, Laurie L.; Deino, Alan (1 August 1996). "Recurrent eruption and subsidence at the Platoro caldera complex, southeastern San Juan volcanic field, Colorado: New tales from old tuffs". GSA Bulletin. 108 (8): 1039–1055. doi:10.1130/0016-7606(1996)108<1039:REASAT>2.3.CO;2.
^ Sliwinski, J. T.; Bachmann, O.; Dungan, M. A.; Huber, C.; Deering, C. D.; Lipman, P. W.; Martin, L. H. J.; Liebske, C. (May 2017). "Rapid pre-eruptive thermal rejuvenation in a large silicic magma body: the case of the Masonic Park Tuff, Southern Rocky Mountain volcanic field, CO, USA". Contributions to Mineralogy and Petrology. 172 (5): 30. doi:10.1007/s00410-017-1351-3. hdl:20.500.11850/216533.
^ Varga, Robert J.; Smith, Brian M. (1984). "Evolution of the Early Oligocene Bonanza Caldera, northeast San Juan Volcanic Field, Colorado". Journal of Geophysical Research. 89 (B10): 8679. doi:10.1029/JB089iB10p08679.
^ Lipman, Peter W.; Zimmerer, Matthew J.; McIntosh, William J. (2015-12-01). "An ignimbrite caldera from the bottom up: Exhumed floor and fill of the resurgent Bonanza caldera, Southern Rocky Mountain volcanic field, Colorado". Geosphere. 11 (6): 1902–1947. Bibcode:2015Geosp..11.1902L. doi:10.1130/GES01184.1.
^ Steven, Thomas A.; Luedke, Robert G.; Lipman, Peter W. (1974). "Relation of mineralization to calderas in the San Juan volcanic field, southwestern Colorado". J. Res. US Geol. Surv. 2: 405–409.

Phases of Volcanism

Notable calderas

Economic Impact

See also

References