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Novarupta samples

NOVARUPTA LINKS

SAMPLES
SAMPLES
Sample has geochemical data available
Sample IDDate SampledReference
97-ND-1a1997-00-00[1]
97-ND-1b1997-00-00[1]
97-ND-21997-00-00[1]
97-ND-31997-00-00[1]
97-ND-41997-00-00[1]
97-ND-51997-00-00[1]
97-ND-61997-00-00[1]
97-ND-71997-00-00[1]
97-ND-8i1997-00-00[1]
97-ND-8h1997-00-00[1]
97-ND-91997-00-00[1]
97-ND-101997-00-00[1]
97-ND-11i1997-00-00[1]
97-ND-11h1997-00-00[1]
97-ND-121997-00-00[1]
TB-8b1997-00-00[1]
K8AA0000-00-00[2]
K882-50000-00-00[2]
K882-130000-00-00[2]
88BP1-30000-00-00[2]
88BP1-40000-00-00[2]
88BP1-60000-00-00[2]
88BP4-90000-00-00[2]
88BP6-10000-00-00[2]
K8AC0000-00-00[2]
K884-40000-00-00[2]
88BP2-10000-00-00[2]
88BP4-100000-00-00[2]
K882-120000-00-00[2]
K882-150000-00-00[2]
K884-60000-00-00[2]
AK70000-00-00[3]
AK7G0000-00-00[3]
AK110000-00-00[3]
AK11G0000-00-00[3]
AK11X0000-00-00[3]
AK11Xa0000-00-00[3]
AK80000-00-00[3]
AK40000-00-00[3]
AK4G0000-00-00[3]
AK4X0000-00-00[3]
AK4Xa0000-00-00[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[6]
K-22[6]
K-18[6]
K-88[7]
K-1000-a[7]
K-1001[7]
K-1065[7]
K-1079-a[7]
K-1190[7]
K-90-a[7]
K-90-c[7]
K-827-a[7]
K-827-c[7]
K-827-d[7]
K-1008-c[7]
K-1061-a[7]
K-1061-c[7]
K-1068-a[7]
K-1073[7]
K-1074-a[7]
K-1158-c[7]
K-1160-a[7]
K-1160-c[7]
K-1194-a[7]
K-1199-c[7]
K-1199-d[7]
K-1200-c[7]
K-2466[7]
K-2466-b[7]
K-2488-a[7]
K-2488-b[7]
K-2488-c[7]
K-2488-d[7]
K-45-glass[7]
K-91[7]
K-1270-a[7]
K-1270-b[7]
K-1270-c[7]
K-1270-d[7]
K-1270-e[7]
K-1270-f[7]
K-1271-a[7]
K-1271-b[7]
K-1271-c[7]
K-1271-d[7]
K-1271-e[7]
K-1271-f[7]
K-1271-g[7]
K-1271-h[7]
K-1271-i[7]
K-2002-a[7]
K-2002-b[7]
K-2620-a[7]
K-2620-b[7]
K-39-r[7]
K-55[7]
K-94-a[7]
K-94-c[7]
K-1083-a[7]
K-1083-c[7]
K-1268-a[7]
K-1268-b[7]
K-1268-c[7]
K-1268-d[7]
K-1268-e[7]
K-1268-f[7]
K-1269-a[7]
K-1269-b[7]
K-1269-c[7]
K-1269-d[7]
K-1269-e[7]
K-1269-f[7]
K-53[7]
K-631-b[7]
K-631-c[7]
K-1267-a[7]
K-1267-b[7]
K-1267-c[7]
K-1267-d[7]
K-1267-e[7]
K-1267-f[7]
K-1267-g[7]
K-23[7]
K-54[7]
K-107-d[7]
K-1266-a[7]
K-1266-b[7]
K-1266-c[7]
K-1266-d[7]
K-1266-e[7]
K-1266-f[7]
K-17[7]
K-622[7]
K-623[7]
K-2004[7]
RLS-214[7]
K-7A-r[7]
K-7A-s[7]
K-11-a-r[7]
K-11-a-s[7]
K-12-c[7]
K-13-c[7]
K-14-c[7]
K-15-c[7]
K-37-c[7]
K-42-r[7]
K-42-s[7]
K-44-r[7]
K-44-s[7]
K-57[7]
K-60[7]
K-63-c[7]
K-64-c[7]
K-66-c[7]
K-66-d[7]
K-74-c[7]
K-75-c[7]
K-75-d[7]
K-75-d-glass[7]
K-75-e[7]
K-76[7]
K-78[7]
K-82-c[7]
K-82-d[7]
K-100-a[7]
K-100-c[7]
K-100-d[7]
K-108-c[7]
K-108-d[7]
K-113-c[7]
K-113-d[7]
K-119D-r[7]
K-121[7]
K-122[7]
K-122-d[7]
K-123-d-r[7]
K-131-d-r[7]
K-135-c[7]
K-138-glass[7]
K-139-r[7]
K-139-s[7]
K-162[7]
K-182[7]
K-184[7]
K-200[7]
K-202[7]
K-203[7]
K-581[7]
K-1363[7]
K-1364[7]
K-1365[7]
K-1365-r[7]
K-1365-s[7]
K-1365-t[7]
K-1365-u[7]
K-1490[7]
K-1495[7]
K-1511-c[7]
K-1518-a[7]
K-1518-b[7]
K-1518-c[7]
K-1518-d[7]
K-1518-e[7]
K-1519-b[7]
K-1525[7]
K-2582-a[7]
K-2582-b[7]
K-2584-b[7]
K-2588-c[7]
K-2614-a[7]
K-2614-b[7]
K-2614-c[7]
K-2614-d[7]
K-2616-a[7]
K-2616-b[7]
K-2617-a[7]
K-2617-b[7]
K-2618-a[7]
K-2618-b[7]
K-2618-c[7]
K-2618-d[7]
K-2619[7]
K-2621-a[7]
K-2621-b[7]
K-2621-c[7]
K-2622-a[7]
K-2622-b[7]
K-2623[7]
K-2624[7]
K-2625[7]
K-2626-a[7]
K-2626-b[7]
K-2626-c[7]
K-2626-d[7]
K-2627-a[7]
K-2627-b[7]
K-2649-a[7]
K-2649-b[7]
K-2649-c[7]
K-2650-a[7]
K-2650-b[7]
K-2651-a[7]
K-2651-b[7]
K-2651-c[7]
K-2651-d[7]
K-2651-e[7]
K-2652-a[7]
K-2652-b[7]
K-2652-c[7]
K-2652-d[7]
K-2653-a[7]
K-2653-b[7]
K-2653-c[7]
K-2653-d[7]
K-2654-a[7]
K-2654-b[7]
K-2654-c[7]
K-2654-d[7]
K-2654-e[7]
K-2654-f[7]
K-542[7]
K-543[7]
K-721[7]
K-851[7]
K-1594-a[7]
K-1594-b[7]
K-1595-a[7]
K-1595-b[7]
K-1595-c[7]
K-1596-a[7]
K-1596-b[7]
K-1596-c[7]
K-1596-d[7]
K-1597-a[7]
K-1597-b[7]
K-1597-c[7]
K-1597-d[7]
K-2005[7]
K-2012-a[7]
K-2012-b[7]
K-2013-a[7]
K-2013-b[7]
K-2013-c[7]
K-2013-d[7]
K-2013-e[7]
K-2015-a[7]
K-2015-b[7]
K-2015-c[7]
K-20V[7]
K-513-V[7]
K-2022-a[7]
K-2022-b[7]
K-2022-c[7]
K-2023-a[7]
K-2023-b[7]
K-2023-c[7]
K-135-d[7]
K-138-r[7]
K-138-s[7]
K-2582-c[7]
K-94-b[7]
K-18s[7]
K-623-r[7]
K-122-d-r[7]
K-851-r[7]
K-88-r[7]
K-88-s[7]
K-39-s[7]
K-16-r[7]
K-16-s[7]
K-119D-s[7]
K-123-d-s[7]
K-123-d-t[7]
K-131-d-s[7]
K-1490-glass[7]
K90And[8]
K90Dac[8]
K90Rhy[8]
K90Nov[8]
AK5[3]
AK6[3]
KAT-1[9]

REFERENCES
citation imageCoombs, 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.

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.

citation imageLowenstern, 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.

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

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.

citation imageHildreth, 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.

citation imageHildreth, 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/ .
Download USGS website with PDF and ebook downloads

citation imageReagan, 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.

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.
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Page modified: May 1, 2014 14:16
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