Overlapping volcanoes: The origin of Hilo Ridge, Hawaii

R. T. Holcomb, B. K. Nelson, P. W. Reiners, N. L. Sawyer

Research output: Contribution to journalArticle

28 Scopus citations

Abstract

The submarine Hilo Ridge has been interpreted as a part of Mauna Kea volcano, but is crossed at ~1100 m depth by a submerged shoreline terrace composed of basalts that are isotopically distinct from those of Mauna Kea and similar to those of Kohala volcano. This terrace evidently is a product of Kohala instead of Mauna Kea. Almost all of Hilo Ridge below the terrace therefore must predate the principal growth of Mauna Kea, which has superficially isolated the ridge from its Kohala source by overlapping its proximal segment. The Mauna Kea section penetrated by the Hawaii Scientific Drilling Project is predicted to be thinner than expected previously, owing to the overlap. Similar overlaps are suspected among other volcanoes and may cause significant changes in the understanding of Hawaiian volcanism.

Original languageEnglish (US)
Pages (from-to)547-550
Number of pages4
JournalGeology
Volume28
Issue number6
StatePublished - Jan 1 2000
Externally publishedYes

Keywords

  • Hilo Ridge
  • Isotope ratios
  • Kohala
  • Mauna Kea
  • Volcanoes

ASJC Scopus subject areas

  • Geology

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    Holcomb, R. T., Nelson, B. K., Reiners, P. W., & Sawyer, N. L. (2000). Overlapping volcanoes: The origin of Hilo Ridge, Hawaii. Geology, 28(6), 547-550.