G. S. Mattioli

The University of Texas at Arlington

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P. E. Jansma

University of Colorado Denver

B. Voight

Pennsylvania State University

Derek Elsworth

Pennsylvania State University

E. Shalev

Duke University

P. E. Malin

Applied Spectral Imaging (United States)

R. S. J. Sparks

University of Bristol

Richard A. Herd

University of East Anglia

D. Hidayat

Politeknik STMI Jakarta

A. T. Linde

Carnegie Institution for Science

H. L. Turner

University of Arkansas at Fayetteville

Cooperative Institutions

John Wiley & Sons (United States)

Centre National de la Recherche Scientifique

United States Geological Survey

Pennsylvania State University

UNAVCO

Hanover College

Montserrat Volcano Observatory

California Institute of Technology

Planetary Science Institute

Istituto Nazionale di Geofisica e Vulcanologia

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Chapter 7.2 Mount Erebus

Geological Society London Memoirs (2021)

K. W. W. Sims R. C. Aster G. A. Gaetani Janne Blichert‐Toft Erin Phillips

Abstract Erebus volcano, Antarctica, is the southernmost active volcano on the globe. Despite its remoteness and harsh conditions, Erebus volcano provides an unprecedented and unique opportunity to study the petrogenesis and evolution, as well as the passive and explosive degassing, of an alkaline magmatic system with a persistently open and magma-filled conduit. In this chapter, we review nearly five decades of scientific research related to Erebus volcano, including geological, geophysical, geochemical and microbiological observations and interpretations. Mount Erebus is truly one of the world's most significant natural volcano laboratories where the lofty scientific goal of studying a volcanic system from mantle to microbe is being realized.

Mount

Globe

10.1144/m55-2019-8

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Citations (17)

Tectonics (2016)

J. W. Geissman Claudio Faccenna Nathan A. Niemi Jonathan C. Aitchison Christopher L. Andronicos

Key Points Transverse-to-the-orogen faults may also participate in slip partitioning resulting from oblique subduction We implement a forward 3-D model of Andean subduction to simulate interseismic and coseismic deformation We constrain kinematics, slip rate, and seismic hazard associated with differently oriented regional faults

10.1002/tect.v35.9

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Prototype PBO instrumentation of CALIPSO project captures world‐record lava dome collapse on Montserrat Volcano

Eos (2004)

G. S. Mattioli S. R. Young B. Voight R. Steven J. Sparks

This article is an update on the status of an innovative new project designed to enhance generally our understanding of andesitic volcano eruption dynamics and, specifically the monitoring and scientific infrastructure at the active Soufrière Hills Volcano (SHV), Montserrat. The project has been designated as the Caribbean Andesite Lava Island Precision Seismo‐geodetic Observatory known as CALIPSO. Its purpose is to investigate the dynamics of the entire SHV magmatic system using an integrated array of specialized instruments in four strategically located ∼200‐m‐deep boreholes in concert with several shallower holes and surface sites. The project is unique, as it represents the first, and only such borehole volcano‐monitoring array deployed at an andesitic stratovolcano.

Stratovolcano

Lava dome

10.1029/2004eo340001

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Structure and dynamics of the magmatic system of Soufrière Hills Volcano, Montserrat (W.I.)

Stefanie Hautmann Joachim Gottsmann R. S. J. Sparks Antonio Costa Oleg Melnik

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Pyroclastic Flow Generated Tsunami Waves Detected by CALIPSO Borehole Strainmeters at Soufriere Hills, Montserrat During Massive Dome Collapse: Numerical Simulations and Observations

AGUFM (2004)

E. J. van Boskirk B. Voight P. Watts Christina Widiwijayanti G. S. Mattioli

Dome (geology)

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COCONet enhancements to circum-Caribbean tsunami warning, tidal, and sea-level monitoring: update on tide gauge installations

AGUFM (2014)

K. Dausz Sebastian Dittmann K. Feaux C. von Hillebrandt-Andrade G. S. Mattioli

Tide gauge

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The Volcanic Geology of the Mid-Arc Island of Dominica, Lesser Antilles—The Surface Expression of an Island-Arc Batholith

Geological Society of America Special Papers (2013)

Alan L. Smith M. J. Roobol G. S. Mattioli Joan E. Fryxell George E. Daly

The geology of the island of Dominica, at the center of the Lesser Antilles island arc, has been subdivided into four stratigraphic divisions: Division 1 (upper Miocene) is dominated by mafi c volcanism; Division 2 (upper Pliocene‐lower Pleistocene) is characterized by the development of two large stratovolcanoes over a 2 million year period; Division 3 (lower to upper Pleistocene) represents a period of island-wide quiescence except at the north and south of the island where two new centers developed on the fl anks of the older stratovolcanoes; and Division 4 (upper Pleistocene‐ Holocene) characterized by the formation of numerous Pelean centers throughout the island. Three of these centers also produced large-volume pumiceous deposits that resulted in the formation of two calderas (Morne Trois Pitons and Wotten Waven).

Batholith

Island arc

Volcanic arc

10.1130/9780813724966

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Citations (17)

Oblique collision in the northeastern Caribbean from GPS measurements and geological observations

Tectonics (2002)

Paul Mann E. Calais Jean‐Claude Ruegg Charles DeMets P. E. Jansma

Previous Caribbean GPS studies have shown that the rigid interior of the Caribbean plate is moving east‐northeastward (070°) at a rate of 18–20 ± 3 mm/yr relative to North America. This direction implies maximum oblique convergence between the island of Hispaniola on the Caribbean plate and the 22–27‐km‐thick crust of the Bahama carbonate platform on the adjacent North America plate. We present a tectonic interpretation of a 15‐site GPS network which spans the Hispaniola‐Bahama oblique collision zone and includes stable plate interior sites on both the North America and Caribbean plates. Measurements span the time period of 1994–1999. In a North America reference frame, GPS velocities in Puerto Rico, St. Croix, and the Lesser Antilles indicate that these areas move as a single block in an east‐northeast direction (070°) at a rate of 19–20 mm/yr consistent with the movement of the rigid interior of the Caribbean plate. GPS velocities at six sites in central and eastern Hispaniola (Dominican Republic) show drastically different behavior with more eastwardly strikes (080°) and much slower rates (4–17 mm/yr) than areas of the stable Caribbean plate. The boundary between the relatively slower‐moving Hispaniola collisional zone and the relatively faster‐moving, uncollided Puerto Rico‐Virgin Islands area is the Mona Passage where late Neogene rifting occurs in a broad zone. Elastic modeling favors strain partitioning with oblique slip on the outer, low‐angle submarine thrust faults (North Hispaniola, Muertos) and strike slip on the inner, subvertical subaerial, strike‐slip faults (Septentrional, Enriquillo).

Collision zone

North American Plate

10.1029/2001tc001304

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Citations (244)

Simultaneous Strainmeter and Creepmeter Observations of Creep events on the San Andreas Fault near Parkfield: A Framework to Observe and Quantify Creep Events

AGU Fall Meeting Abstracts (2018)

D. Mencin Roger Bilham K. M. Hodgkinson G. S. Mattioli

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PBO Borehole Strainmeters: 2017 Episodic Tremor and Slip Event for Southern Vancouver Island, BC, Canada through Olympia, WA, USA

AGU Fall Meeting Abstracts (2017)

E. J. van Boskirk K. M. Hodgkinson M. H. Gottlieb W. Johnson D. B. Henderson

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