Bulletin of Volcanology

, 75:726 | Cite as

Shield volcanoes of Marie Byrd Land, West Antarctic rift: oceanic island similarities, continental signature, and tectonic controls

  • Wesley LeMasurierEmail author
Research Article


The Marie Byrd Land volcanic province is largely defined by 18 large (up to ~1,800 km3) alkaline shield volcanoes, each surmounted by a summit section of varied felsic rocks dominated by trachytic flows. They are distributed over a 500 × 800-km block-faulted dome within the West Antarctic rift. The basement contact of volcanic sections is ~500 masl at one site and 3,000 mbsl at another, 70 km away, which illustrates the scale of block faulting but complicates an understanding of volcanic structure. Furthermore, the continental ice sheet buries 16 volcanoes to progressively greater heights inland. However, five are sufficiently exposed to allow meaningful comparisons with alkaline oceanic island volcanoes; these comparisons are used as a guide to estimate the structure of Marie Byrd Land volcanoes. The type example for this study is Mt. Murphy, the most completely exposed volcano. It consists of a 1,400-m section of alkaline basalt overlain by trachyte and benmoreite flows that make up ~7–13 % of the volcano volume. In gross structure and composition, Mt. Murphy is similar to Gran Canaria volcano, Canary Islands, but the percent of felsic rock may be three times that of Gran Canaria, if the estimate is approximately correct. Departures from the oceanic island example are believed to represent the imprint of the Marie Byrd Land lithosphere and tectonic environment on volcano evolution. These include a lack of order in the sequence of felsic rock types, lack of progression toward more silica undersaturated compositions with time, absence of a highly undersaturated mafic resurgent stage, and perhaps, a relatively large volume of felsic rock.


Shield volcanoes Alkaline oceanic islands Evolutionary stages Order of eruption 



I am pleased to acknowledge the support of the National Science Foundation through grant # 536526, administered by the Office of Polar Programs. John Andrews and Cristina de Ignacio San José provided much appreciated critiques of an early draft of the manuscript. Formal reviews by Jim Cole, Valentin Troll, and two anonymous reviewers provided helpful and authoritative critiques of Gran Canaria, Mt. Murphy, and other sections, for which I am very grateful. I am much obliged to Associate Editor Ben van Wyk de Vries for well-balanced reviews and thoughtful editorial oversight that greatly improved the manuscript.

Supplementary material

445_2013_726_MOESM1_ESM.docx (22 kb)
ESM 1 (DOCX 21 kb)


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Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  1. 1.Institute of Arctic and Alpine Research (INSTAAR)University of ColoradoBoulderUSA

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