Novarupta - Samples

SAMPLES

Sample has geochemical data available

Sample ID	Date Sampled	Reference
97-ND-1a	1997-00-00	[1]
97-ND-1b	1997-00-00	[1]
97-ND-2	1997-00-00	[1]
97-ND-3	1997-00-00	[1]
97-ND-4	1997-00-00	[1]
97-ND-5	1997-00-00	[1]
97-ND-6	1997-00-00	[1]
97-ND-7	1997-00-00	[1]
97-ND-8i	1997-00-00	[1]
97-ND-8h	1997-00-00	[1]
97-ND-9	1997-00-00	[1]
97-ND-10	1997-00-00	[1]
97-ND-11i	1997-00-00	[1]
97-ND-11h	1997-00-00	[1]
97-ND-12	1997-00-00	[1]
TB-8b	1997-00-00	[1]
1991 VTTS 311	1991-00-00	[2]
1991 VTTS 312	1991-00-00	[2]
1991 VTTS 39	1991-00-00	[2]
K8AA	1988-01-01	[3]
K882-5	1988-01-01	[3]
K882-13	1988-01-01	[3]
88BP1-3	1988-01-01	[3]
88BP1-4	1988-01-01	[3]
88BP1-6	1988-01-01	[3]
88BP4-9	1988-01-01	[3]
88BP6-1	1988-01-01	[3]
K8AC	1988-01-01	[3]
K884-4	1988-01-01	[3]
88BP2-1	1988-01-01	[3]
88BP4-10	1988-01-01	[3]
K882-12	1988-01-01	[3]
K882-15	1988-01-01	[3]
K884-6	1988-01-01	[3]
588		[4]
415		[4]
Kosco_Nova_1light		[5]
Kosco_Nova_1dark		[5]
Kosco_Nova_2		[5]
K-45		[6]
K-123		[6]
K-101		[6]
K-139		[6]
K-42		[6]
K-16		[7] [6]
K-22		[6]
K-18		[6]
K-88		[8]
K-1000-a		[8]
K-1001		[8]
K-1065		[8]
K-1079-a		[8]
K-1190		[8]
K-90-a		[8]
K-90-c		[8]
K-827-a		[8]
K-827-c		[8]
K-827-d		[8]
K-1008-c		[8]
K-1061-a		[8]
K-1061-c		[8]
K-1068-a		[8]
K-1073		[8]
K-1074-a		[8]
K-1158-c		[8]
K-1160-a		[8]
K-1160-c		[8]
K-1194-a		[8]
K-1199-c		[8]
K-1199-d		[8]
K-1200-c		[8]
K-2466		[8]
K-2466-b		[8]
K-2488-a		[8]
K-2488-b		[8]
K-2488-c		[8]
K-2488-d		[8]
K-45-glass		[8]
K-91		[8]
K-1270-a		[8]
K-1270-b		[8]
K-1270-c		[8]
K-1270-d		[8]
K-1270-e		[8]
K-1270-f		[8]
K-1271-a		[8]
K-1271-b		[8]
K-1271-c		[8]
K-1271-d		[8]
K-1271-e		[8]
K-1271-f		[8]
K-1271-g		[8]
K-1271-h		[8]
K-1271-i		[8]
K-2002-a		[8]
K-2002-b		[8]
K-2620-a		[8]
K-2620-b		[8]
K-39-r		[8]
K-55		[8]
K-94-a		[8]
K-94-c		[8]
K-1083-a		[8]
K-1083-c		[8]
K-1268-a		[8]
K-1268-b		[8]
K-1268-c		[8]
K-1268-d		[8]
K-1268-e		[8]
K-1268-f		[8]
K-1269-a		[8]
K-1269-b		[8]
K-1269-c		[8]
K-1269-d		[8]
K-1269-e		[8]
K-1269-f		[8]
K-53		[8]
K-631-b		[8]
K-631-c		[8]
K-1267-a		[8]
K-1267-b		[8]
K-1267-c		[8]
K-1267-d		[8]
K-1267-e		[8]
K-1267-f		[8]
K-1267-g		[8]
K-23		[8]
K-54		[8]
K-107-d		[8]
K-1266-a		[8]
K-1266-b		[8]
K-1266-c		[8]
K-1266-d		[8]
K-1266-e		[8]
K-1266-f		[8]
K-17		[8]
K-622		[8]
K-623		[8]
K-2004		[8]
RLS-214		[8]
K-7A-r		[8]
K-7A-s		[8]
K-11-a-r		[8]
K-11-a-s		[8]
K-12-c		[8]
K-13-c		[8]
K-14-c		[8]
K-15-c		[8]
K-37-c		[8]
K-42-r		[8]
K-42-s		[8]
K-44-r		[8]
K-44-s		[8]
K-57		[8]
K-60		[8]
K-63-c		[8]
K-64-c		[8]
K-66-c		[8]
K-66-d		[8]
K-74-c		[8]
K-75-c		[8]
K-75-d		[8]
K-75-d-glass		[8]
K-75-e		[8]
K-76		[8]
K-78		[8]
K-82-c		[8]
K-82-d		[8]
K-100-a		[8]
K-100-c		[8]
K-100-d		[8]
K-108-c		[8]
K-108-d		[8]
K-113-c		[8]
K-113-d		[8]
K-119D-r		[8]
K-121		[8]
K-122		[8]
K-122-d		[8]
K-123-d-r		[8]
K-131-d-r		[8]
K-135-c		[8]
K-138-glass		[8]
K-139-r		[8]
K-139-s		[8]
K-162		[8]
K-182		[8]
K-184		[8]
K-200		[8]
K-202		[8]
K-203		[8]
K-581		[8]
K-1363		[8]
K-1364		[8]
K-1365		[8]
K-1365-r		[8]
K-1365-s		[8]
K-1365-t		[8]
K-1365-u		[8]
K-1490		[8]
K-1495		[8]
K-1511-c		[8]
K-1518-a		[8]
K-1518-b		[8]
K-1518-c		[8]
K-1518-d		[8]
K-1518-e		[8]
K-1519-b		[8]
K-1525		[8]
K-2582-a		[8]
K-2582-b		[8]
K-2584-b		[8]
K-2588-c		[8]
K-2614-a		[8]
K-2614-b		[8]
K-2614-c		[8]
K-2614-d		[8]
K-2616-a		[8]
K-2616-b		[8]
K-2617-a		[8]
K-2617-b		[8]
K-2618-a		[8]
K-2618-b		[8]
K-2618-c		[8]
K-2618-d		[8]
K-2619		[8]
K-2621-a		[8]
K-2621-b		[8]
K-2621-c		[8]
K-2622-a		[8]
K-2622-b		[8]
K-2623		[8]
K-2624		[8]
K-2625		[8]
K-2626-a		[8]
K-2626-b		[8]
K-2626-c		[8]
K-2626-d		[8]
K-2627-a		[8]
K-2627-b		[8]
K-2649-a		[8]
K-2649-b		[8]
K-2649-c		[8]
K-2650-a		[8]
K-2650-b		[8]
K-2651-a		[8]
K-2651-b		[8]
K-2651-c		[8]
K-2651-d		[8]
K-2651-e		[8]
K-2652-a		[8]
K-2652-b		[8]
K-2652-c		[8]
K-2652-d		[8]
K-2653-a		[8]
K-2653-b		[8]
K-2653-c		[8]
K-2653-d		[8]
K-2654-a		[8]
K-2654-b		[8]
K-2654-c		[8]
K-2654-d		[8]
K-2654-e		[8]
K-2654-f		[8]
K-542		[8]
K-543		[8]
K-721		[8]
K-851		[8]
K-1594-a		[8]
K-1594-b		[8]
K-1595-a		[8]
K-1595-b		[8]
K-1595-c		[8]
K-1596-a		[8]
K-1596-b		[8]
K-1596-c		[8]
K-1596-d		[8]
K-1597-a		[8]
K-1597-b		[8]
K-1597-c		[8]
K-1597-d		[8]
K-2005		[8]
K-2012-a		[8]
K-2012-b		[8]
K-2013-a		[8]
K-2013-b		[8]
K-2013-c		[8]
K-2013-d		[8]
K-2013-e		[8]
K-2015-a		[8]
K-2015-b		[8]
K-2015-c		[8]
K-20V		[8]
K-513-V		[8]
K-2022-a		[8]
K-2022-b		[8]
K-2022-c		[8]
K-2023-a		[8]
K-2023-b		[8]
K-2023-c		[8]
K-135-d		[8]
K-138-r		[8]
K-138-s		[8]
K-2582-c		[8]
K-94-b		[8]
K-18s		[8]
K-623-r		[8]
K-122-d-r		[8]
K-851-r		[8]
K-88-r		[8]
K-88-s		[8]
K-39-s		[8]
K-16-r		[8]
K-16-s		[8]
K-119D-s		[8]
K-123-d-s		[8]
K-123-d-t		[8]
K-131-d-s		[8]
K-1490-glass		[8]
K90And		[9]
K90Dac		[9]
K90Rhy		[9]
K90Nov		[9]
AK7		[10]
AK7G		[10]
AK5		[10]
AK11		[10]
AK11G		[10]
AK11X		[10]
AK11Xa		[10]
AK8		[10]
AK6		[10]
AK4		[10]
AK4G		[10]
AK4X		[10]
AK4Xa		[10]
KAT-1		[11]
K-2585		[12]
K-2583		[12]
K-2584F		[12]
K-2584G		[12]
K-2588D		[12]
UA1364		[13]
K131d		[14]
K1490		[14]

REFERENCES

^[1] Experimental and petrologic constraints on magma movement, storage, and interactions at two volcanoes in Katmai National Park, Alaska, 2001

Coombs, M. L., 2001, Experimental and petrologic constraints on magma movement, storage, and interactions at two volcanoes in Katmai National Park, Alaska: University of Alaska Fairbanks unpublished Ph.D. dissertation, Fairbanks, Alaska, 214 p.

^[2] Late Pleistocene volcanic deposits near the Valley of Ten Thousand Smokes, Katmai National Park, Alaska, 1991

Pinney, D. S., and Beget, J. E., 1991, Late Pleistocene volcanic deposits near the Valley of Ten Thousand Smokes, Katmai National Park, Alaska: in Reger, R. D., (ed.), Short notes on Alaskan geology 1991, Alaska Division of Geological & Geophysical Surveys Professional Report PR 0111, p. 45-53.

^[3] Petrogenetic study of dacite from the 1912 eruption Novarupta, Katmai National Park, Alaska: implications for magma storage locations, 1992

Avery, V. F., 1992, Petrogenetic study of dacite from the 1912 eruption Novarupta, Katmai National Park, Alaska: implications for magma storage locations: University of Alaska Fairbanks unpublished M.S. thesis, 177 p.

^[4] The Katmai magmatic province, 1926

Fenner, C. N., 1926, The Katmai magmatic province: Journal of Geology, v. 34, n. 7, p. 673-772.

^[5] Part I: The Mt. Edgecumbe volcanic field, Alaska: an example of tholeiitic and calc-alkaline volcanism, Part II: Characteristics of andesitic to dacitic volcanism at Katmai National Park, Alaska, 1981

Kosco, D. G., 1981, Part I: The Mt. Edgecumbe volcanic field, Alaska: an example of tholeiitic and calc-alkaline volcanism, Part II: Characteristics of andesitic to dacitic volcanism at Katmai National Park, Alaska: University of California, Berkeley unpublished Ph.D. dissertation, 249 p.

^[6] The compositionally zoned eruption of 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, Alaska, 1983

Hildreth, Wes, 1983, The compositionally zoned eruption of 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, Alaska: Journal of Volcanology and Geothermal Research, v. 18, n. 1-4, p. 1-56.

^[7] The plinian eruptions of 1912 at Novarupta, Katmai National Park, Alaska, 1992

Fierstein, Judy, and Hildreth, Wes, 1992, The plinian eruptions of 1912 at Novarupta, Katmai National Park, Alaska: Bulletin of Volcanology, v. 54, n. 8, p. 646-684.

^[8] The Novarupta-Katmai eruption of 1912: Largest eruption of the twentieth century: Centennial perspectives, 2012

Hildreth, W., and Fierstein, J., 2012, The Novarupta-Katmai eruption of 1912: Largest eruption of the twentieth century: Centennial perspectives: U.S. Geological Survey Professional Paper 1791, 259 p., available at http://pubs.usgs.gov/pp/1791/ .

USGS website with PDF and ebook downloads

^[9] Time-scales of differentiation from mafic parents to rhyolite in North American continental arcs, 2003

Reagan, M. K., Sims, K. W. W., Erich, J., Thomas, R. B., Cheng, H., Edwards, R. L., Layne, G., and Ball, L., 2003, Time-scales of differentiation from mafic parents to rhyolite in North American continental arcs: Journal of Petrology, v. 44, n. 9, p. 1703-1726.

^[10] Evidence for a copper-bearing fluid in magma erupted at the Valley of Ten Thousand Smokes, Alaska, 1993

Lowenstern, J. B., 1993, Evidence for a copper-bearing fluid in magma erupted at the Valley of Ten Thousand Smokes, Alaska: Contributions to Mineralogy and Petrology, v. 114, n. 3, p. 409-421.

^[11] Nd and Sr isotopes in the Aleutians: multicomponent parenthood of island-arc magmas, 1986

von Drach, V., Marsh, B. D., and Wasserburg, G. J., 1986, Nd and Sr isotopes in the Aleutians: multicomponent parenthood of island-arc magmas: Contributions to Mineralogy and Petrology, v. 92, n. 1, p. 13-34.

^[12] Explosive eruptive record in the Katmai region, Alaska Peninsula: an overview, 2007

Fierstein, Judy, 2007, Explosive eruptive record in the Katmai region, Alaska Peninsula: an overview: Bulletin of Volcanology, v. 69, n. 5, p. 469-509, doi:10.1007/s00445-006-0097-y.

http://dx.doi.org/10.1007/s00445-006-0097-y

^[13] Late Pleistocene and Holocene tephrostratigraphy of interior Alaska and Yukon: Key beds and chronologies over the past 30,000 years, 2016

Davies, L. J., Jensen, B. J., Froese, D. G., and Wallace, K. L., 2016, Late Pleistocene and Holocene tephrostratigraphy of interior Alaska and Yukon: Key beds and chronologies over the past 30,000 years: Quaternary Science Reviews, v. 146, p. 28-53.

^[14] Magma storage prior to the 1912 eruption at Novarupta, Alaska, 2002

Hammer, J. E., Rutherford, M. J., and Hildreth, Wes, 2002, Magma storage prior to the 1912 eruption at Novarupta, Alaska: Contributions to Mineralogy and Petrology, v. 144, n. 2, p. 144-162.

Novarupta samples