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You are here: Home > Library > Mount Griggs: A compositionally distinctive Quaternary stratovolcano behind the main volcanic line in Katmai National Park

MOUNT GRIGGS: A COMPOSITIONALLY DISTINCTIVE QUATERNARY STRATOVOLCANO BEHIND THE MAIN VOLCANIC LINE IN KATMAI NATIONAL PARK
citation imageHildreth, Wes, Fierstein, Judy, Lanphere, M. A., and Siems, D. F., 2002, Mount Griggs: A compositionally distinctive Quaternary stratovolcano behind the main volcanic line in Katmai National Park: in Wilson, F. H. and Galloway, J. P., (eds.), Studies by the U.S. Geological Survey in Alaska, 2000, U.S. Geological Survey Professional Paper PP 1662, p. 87-112.
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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.
1063: Chemical analyses of eruptive products from Mount Griggs, Alaska.
View table data :: Download table data (.csv)
* Major-oxides contents in weight percent, normalized to H2O-free totals of 99.6 weight percent (allowing 0.4 weight percent for trace oxides and halogens); determinations by wavelength-dispersive XRF in USGS laboratory at Lakewood CO; D.F. Siems, analyst. Rb, Sr, and Zr (in parts per million) determined by energy-dispersive XRF by D.F. Siems. Precision and accuracy are discussed by 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= weight loss on ignition at 900C). *

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