AVO Logo
Site Map | FAQ |
Alaska Volcano Observatory
 
You are here: Home > Samples > 73-ARh-81

SAMPLE INFO : 73-ARh-81
Sample ID:73-ARh-81
Station ID:73-ARh-81
Latitude:62.2853
Longitude:-143.9358
Datum:NAD83
Date Sampled:1973-00-00
Sample Type 1:Lava
Sample Type 2:Flow
Field Lithology:Basalt
Sample Unit:Qob
Text Description:
Wrangell Lava. Olivine basalt and andesite flows (Pleistocene). Flows are 2-6 m thick and exhibit conspicuous reddish-brown scoriaceous flow tops and bottoms. Dense flow interiors are medium to dark gray and sparsely porphyritic containing phenocrysts of plagioclase (2-5%, 3-4 mm) and olivine (1-3%, 0.5 - 1 mm) in an intersertal to pilotaxitic groundmass of plagioclase, pyroxene, opaque minerals, and glass. Rarely, flows contains as much as 3% phenocrystic hypersthene. Flows probably erupted from a rift a few kilometers west in the Gulkana B-1 quadrangle and tend to be more silicic than some of the flows included in the map unit in Gulkana B-1 quadrangle (Richter and others, 1989). Major element chemistry for sample 73-ARh-81 (map locality 2) is shown in table 1. Whole rock K-Ar age of sample 73-ARh-87 (map locality 17) is 0.32 +/- 0.09 Ma. (table 2). Aggregate maximum thickness about 360 m.

References:
Geologic map of the Nabesna B-6 Quadrangle, south-central Alaska

GEOCHEM DATA
StationIDLatitudeLongitudeGeologistDateVisitedVolcanoEruptionLocation DescriptionText DescriptionSample IDMaterialSiO2TiO2Al2O3FeOTMnOMgOCaONa2OK2OP2O5Total-majorsREF majorsMETH majorsFe2O3/Fe203T origFeO/FeOT origVolatiles csvMETH volatilesCsRbBaSrLaCePrNdSmEuGdTbDyHoErTmYbLuYZrNbHfTaPbThUScVCrFeCoNiCuZnGaMoAsNaKRef trace1METH trace1RbBaSrLaCeNdSmEuGdDyErYbLuYZrNbPbThUScTiVCrNiCuZnGaRef trace2METH trace2Light csvHalogen csvother major csvother lile csvother ree csvother hfse csvother hpe csvother tm csvother misc csv
73-ARh-8162.2853-143.9358Richter, D. H.1973-00-00SanfordWrangell Lava; Nabesna B-6 quadrangle. Latitude and longitude derived from paper map.Wrangell Lava. Olivine basalt and andesite flows (Pleistocene). Flows are 2-6 m thick and exhibit conspicuous reddish-brown scoriaceous flow tops and bottoms. Dense flow interiors are medium to dark gray and sparsely porphyritic containing phenocrysts of plagioclase (2-5%, 3-4 mm) and olivine (1-3%, 0.5 - 1 mm) in an intersertal to pilotaxitic groundmass of plagioclase, pyroxene, opaque minerals, and glass. Rarely, flows contains as much as 3% phenocrystic hypersthene. Flows probably erupted from a rift a few kilometers west in the Gulkana B-1 quadrangle and tend to be more silicic than some of the flows included in the map unit in Gulkana B-1 quadrangle (Richter and others, 1989). Major element chemistry for sample 73-ARh-81 (map locality 2) is shown in table 1. Whole rock K-Ar age of sample 73-ARh-87 (map locality 17) is 0.32 +/- 0.09 Ma. (table 2). Aggregate maximum thickness about 360 m.73-ARh-81Whole Rock 56.5 1.26 18.3 6.78 0.11 3.58 7.35 4.03 1.6 0.34 99.752321NN2.614.4H2OP=0.1; H2OM=0.05; CO2=0.01RAPIDA

SAMPLE LOCATION

Contact AVO Privacy Accessibility Information Quality FOIA
URL: www.avo.alaska.edu/samples/sample_info.php
Page modified: July 14, 2014 13:37
Contact Information: AVO Web Team

twitter @alaska_avo
facebook alaska.avo
email Receive volcano updates by email: USGS VNS