Transatlantic distribution of the Alaskan White River Ash

• Published in: Geology (Boulder) 2014-10, Vol.42 (10), p.875-878
• Main Authors: Jensen, Britta J. L, Pyne-O'Donnell, Sean, Plunkett, Gill, Froese, Duane G, Hughes, Paul D. M, Sigl, Michael, McConnell, Joseph R, Amesbury, Matthew J, Blackwell, Paul G, van den Bogaard, Christel, Buck, Caitlin E, Charman, Dan J, Clague, John J, Hall, Valerie A, Koch, Johannes, Mackay, Helen, Mallon, Gunnar, McColl, Lynsey, Pilcher, Jonathan R
• Format: Article
• Language: English
• Subjects: Alaska; Archaeology; Atlantic Ocean; Cenozoic; climate effects; cores; Correlation analysis; eruptions; Freshwater; Geochemistry; Geological time; Geology; Geomorphology; Holocene; ice cores; igneous rocks; major elements; minor elements; Northern Hemisphere; pyroclastics; Quaternary; Quaternary geology; sediments; spatial distribution; tephrostratigraphy; United States; upper Holocene; volcanic ash; volcanic rocks; volcanism; Volcanology; White River Ash
• ISSN: 0091-7613; 1943-2682
• DOI: 10.1130/G35945.1

Volcanic ash layers preserved within the geologic record represent precise time markers that correlate disparate depositional environments and enable the investigation of synchronous and/or asynchronous behaviors in Earth system and archaeological sciences. However, it is generally assumed that only exceptionally powerful events, such as supereruptions (≥450 km3 of ejecta as dense-rock equivalent; recurrence interval of ∼105 yr), distribute ash broadly enough to have an impact on human society, or allow us to address geologic, climatic, and cultural questions on an intercontinental scale. Here we use geochemical, age, and morphological evidence to show that the Alaskan White River Ash (eastern lobe; A.D. 833-850) correlates to the "AD860B" ash (A.D. 846-848) found in Greenland and northern Europe. These occurrences represent the distribution of an ash over 7000 km, linking marine, terrestrial, and ice-core records. Our results indicate that tephra from more moderate-size eruptions, with recurrence intervals of ∼100 yr, can have substantially greater distributions than previously thought, with direct implications for volcanic dispersal studies, correlation of widely distributed proxy records, and volcanic hazard assessment.