New Ar-40/Ar-39 dating of the Grande Ronde lavas, Columbia River Basalts, USA: Implications for duration of flood basalt eruption episodes

T. L. Barry, S. Self, S. P. Kelley, S. Reidel, P. Hooper, M. Widdowson

Research output: Contribution to journalArticlepeer-review

Abstract / Description of output

Grande Ronde Basalt (GRB) lavas represent the most voluminous eruptive pulse of the Columbia River-Snake River-Yellowstone hotspot volcanism. With an estimated eruptive volume of 150,000 km(3), GRB lavas form at least 66% of the total volume of the Columbia River Basalt Group. New Ar-40/Ar-39 dates for GRB lavas reveal they were emplaced within a maximum period of 0.42 +/- 0.18 My. A well-documented stratigraphy indicates at least 110 GRB flow fields (or individual eruptions), and on this basis suggests an average intereruption hiatus of less than 4000 years. Isotopic age-dating cannot resolve time gaps between GRB eruptions, and it is difficult to otherwise form a picture of the durations of eruptions because of non-uniform weathering in the top of flow fields and a general paucity of sediments between GR lavas. Where sediment has formed on top of GRB lavas, it varies in thickness from zero to 20-30 cm of silty to fine-sandy material, with occasional diatomaceous sediment. Individual GRB eruptions varied considerably in volume but many were greater than 1000 km(3) in size. Most probably eruptive events were not equally spaced in time: some eruptions may have followed short periods of volcanic repose (perhaps 10(2) to 10(3) of years), whilst others could have been considerably longer (many 1000 s to > 10(4) years). Recent improvements in age-dating for other continental flood basalt (CFB) lava sequences have yielded estimates of total eruptive durations of less than 1 My for high-volume pulses of lava production. The GRB appears to be a similar example, where the main pulse occupied a brief period. Even allowing for moderate to long-duration pahoehoe flow field production, the amount of time the system spends in active lava-producing mode is small - less than c. 2.6% (based on eruption durations of approximately 10,000 years, compared to the duration of the entire eruptive pulse of c. 420,000 years). A review of available Ar-40/Ar-39 data for the major voluminous phases of the Columbia River Basalt Group suggests that activity of the Steens Basalt-Imnaha Basalt-GRB may have, at times, been simultaneous, with obvious implications for climatic effects. Resolving intervals between successive eruptions during CFB province construction, and durations of main eruptive pulses, remains vital to determining the environmental impact of these huge eruptions. (C) 2010 Elsevier B.V. All rights reserved.
Original languageEnglish
Pages (from-to)213-222
Number of pages10
Issue number3-4
Publication statusPublished - 2010


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