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Featured researches published by C. P. Mann.


Geological Society of America Special Papers | 2004

Subaqueous intracaldera volcanism, Ilopango Caldera, El Salvador, Central America

C. P. Mann; John Stix; James W. Vallance; Mathieu Richer

The Ilopango Caldera, located 10 km east of San Salvador, has erupted voluminous silicic pyroclastics four times in the last 57,000 years. The present caldera has a quasi-rectangular shape and is fi lled by Lake Ilopango. This paper provides a detailed description of a segment of the intracaldera stratigraphy at Ilopango caldera, with emphasis on the San Agustin Block Unit. Physical volcanology, petrology, and geochemistry establish the depositional environment and eruptive conditions of the intracaldera sequence and help to model the emplacement of the San Agustin Block Unit. The intracaldera stratigraphy comprises a sequence of pyroclastic density currents, unconformably overlain by lacustrine sediments and conformably overlain by the San Agustin Block Unit. A new radiocarbon age on wood near the top of the Lacustrine Unit indicates that a lake was present ≥43,670 years ago. The intracaldera sequence displays abundant evidence of emplacement in a subaqueous environment. The San Agustin Block Unit comprises a basal Fine Ash facies and an overlying Pumice Breccia facies. The basal Fine Ash facies is a hydromagmatic layer containing pumiceous and blocky angular glass shards, aggregates of fi ne ash and phenocryst fragments, and phenocrysts with a fi ne ash coating. The overlying Pumice Breccia facies is composed of pumice clasts up to three meters in length. The pumice clasts display a series of jointing textures indicative of hot emplacement and rapid cooling. These two facies suggest an initial subaqueous explosive eruption in which a vesiculated silicic melt fragmented upon contact with the water. When the magma had degassed suffi ciently, the eruption style evolved to subaqueous dome growth that spalled quenched pumice clasts from a moderately vesiculated carapace.


Geophysics | 2007

Multi-university Internet video-conferencing course provides novel approach to student-directed learning

Adam J. Durant; William I. Rose; C. P. Mann; John Stix

Connecting graduate students with experts in a given discipline is vital to their success but has often been challenging because of logistics, costs, and scheduling. However, advances in Internet video conferencing now allow multiple parties to meet simultaneously and engage in real-time discussion.


Bulletin of Volcanology | 2013

Phenocryst-hosted melt inclusions record stalling of magma during ascent in the conduit and upper magma reservoir prior to vulcanian explosions, Soufrière Hills volcano, Montserrat, West Indies

C. P. Mann; Paul J. Wallace; John Stix


Geological Society of America Special Papers | 2004

Mafic magma injection triggers eruption at Ilopango Caldera, El Salvador, Central America

Mathieu Richer; C. P. Mann; John Stix


Archive | 2006

Volatile Contents of Melt Inclusions From Andesite Pumice at Soufrière Hills volcano, Montserrat, West Indies

C. P. Mann; Paul J. Wallace; James Roberge; Susan C. Loughlin; John Stix


Archive | 2010

Role of mafic enclaves at the Soufriere Hills volcano, Montserrat

C. P. Mann; John Stix; Thomas Christopher


Archive | 2010

Steady-state behavior of the Soufrire Hills volcano, Montserrat

C. P. Mann; John Stix


Archive | 2010

Magmatic evolution of the Ilopango Caldera, El Salvador, Central America

D. Zezin; C. P. Mann; W. Hernandez; John Stix


Archive | 2007

Mechanics of Student-Directed Multi-University Internet Video-Conferencing Course

Adam J. Durant; C. P. Mann; William I. Rose; John Stix


Archive | 2007

Earth Hazards Consortium: a Novel Approach to Student Education in Geoscience

C. P. Mann; Hugo Delgado Granados; R. P. Escobar Wolf; Adam J. Durant; Gerald R. Girard; Edward S. Calder; T. Dominguez; James Roberge; William I. Rose; John Stix; Nicholas Varley; Glyn Williams-Jones; I. Hernandez Javier; S. Salinas Sanchez

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William I. Rose

Michigan Technological University

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Hugo Delgado Granados

National Autonomous University of Mexico

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James W. Vallance

United States Geological Survey

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