Alaska Volcano Observatory - The Novarupta-Katmai eruption of 1912: Largest eruption of the twentieth century: Centennial perspectives

THE NOVARUPTA-KATMAI ERUPTION OF 1912: LARGEST ERUPTION OF THE TWENTIETH CENTURY: CENTENNIAL PERSPECTIVES

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/ .

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DATA TABLES *Not all tables in a publication may be listed. Not all tables from a publication have data entered in the database.

1393: Major-element chemical analyses of eruptive products, Novarupta 1912

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* The 10 major oxides (reported in weight percent) are normalized to H2O-free totals of 99.6 weight percent (allowing 0.4 wt % for trace oxides and halogens); determinations by wavelength-dispersive x-ray fluorescence in US Geological Survey laboratory at Lakewood, CO; supervised by JE Taggart. Precision and accuracy are discussed by Baedecker (1987) and Bacon and Druitt (1988). FeO* is total iron calculated as FeO. "Original total" is the volatile-free sum of the 10 oxides, as analyzed, before normalization, with total iron calculated as Fe2O3. LOI is weight loss on ignition at 900C. *

1403: Trace-element chemical analyses of eruptive products, Novarupta 1912

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* Determinations (in ppm) by energy-dispersive x-ray fluorescence in U.S. Geological Survey laboratory at Lakewood, CO; D.F. Siems, analyst. Precision and accuracy are discussed by Baedecker (1987) and Bacon and Druitt (1988). Additional data are given by Turner and others (2010). *

1413: Trace-element analyses of 1912 eruptive products by Instrumental neutron activation analysis (INAA).

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* Determination (in ppm) by INAA in U.S. Geological Survey laboratories. Methods and precision discussed by Baedecker (1987). *

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