ME
Member Since 2009
Megan Eve Newcombe
Assistant Professor, University of Maryland College Park
AGU Research
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3D Diffusion of Water in Melt Inclusion‐Bearing Olivine Phenocrysts
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
04 march 2024
Euan Mutch, Megan E. Newcombe, John F. Rudge

Olivine‐hosted melt inclusions are an important archive of pre‐eruptive processes such as magma storage, mixing and subsequent ascent t...

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Efficiency and timing of water loss during heating of early-formed planetesimals
EXPLORING ROCKY BODY EVOLUTION IN THE SOLAR SYSTEM AND BEYOND II ORAL
study of earth's deep interior | 15 december 2023
Megan E. Newcombe, Liam Peterson, Sumedha Desikama...
The timing of delivery and the types of bodies that contributed volatiles to the terrestrial planets remain highly debated. For example, it is unknown...
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Using Microlite Number Density to Understand Variation in Magma Decompression Throughout a Single Eruption at Cinder Cone, Lassen Volcanic National Park, CA
UNDER PRESSURE: MEASUREMENT AND INTERPRETATION OF PRESSURE-DEPENDENT PARAMETERS AND DECOMPRESSION RATES IN MAGMAS II POSTER
volcanology, geochemistry and petrology | 12 december 2023
Claire Rowan-Arnett, Kristina J. Walowski, Megan E...
Cinder Cone, located in Lassen Volcanic National Park in Northern California, erupted in 1666 CE and had three main eruptive phases, producing explosi...
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Exploring the Magmatic Plumbing System of Pavlof Volcano, Alaska over Time with Olivine-Hosted Melt Inclusions
UNDER PRESSURE: MEASUREMENT AND INTERPRETATION OF PRESSURE-DEPENDENT PARAMETERS AND DECOMPRESSION RATES IN MAGMAS II POSTER
volcanology, geochemistry and petrology | 12 december 2023
Valerie Kelly K. Wasser, Taryn M. Lopez, Jessica F...
Pavlof Volcano, Alaska is frequently active and often erupts with little to no precursory unrest. Prior petrologic work at Pavlof suggests that magma ...
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Relieving the Pressure: Low Pressure (30-100 MPa) Olivine/Melt Partitioning of H2O
ORIGIN, DISTRIBUTION, AND TRANSPORT OF VOLATILES IN EARTH AND TERRESTRIAL PLANETS I POSTER
volcanology, geochemistry and petrology | 11 december 2023
Liam Peterson, Megan E. Newcombe, Philip M. Piccol...
Mineral-melt H2O (total H quantified as H2O) partition coefficients are frequently used to estimate the H2O contents of parental melts in volcanic sys...
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Influence of Pumice Texture on Magma Decompression Rate Estimates Using Bubble Number Density: Application to the Largest Known Plinian Eruption of Cerro Machin Volcano, Colombia
THE STORAGE, TRANSPORT, AND ERUPTION OF MAGMA USING FIELD OBSERVATIONS, LABORATORY APPROACHES, AND MODELING IV POSTER
volcanology, geochemistry and petrology | 14 december 2022
MaKayla Etheredge, Silvia Castilla , Philip M. Pi...
Bubble size and number in pumice is related to the decompression rate of magma during syneruptive ascent. Rapid magma decompression leads to a high de...
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Crystals and Melt Inclusions Record Deep Storage of Superhydrous Magma Prior to the Largest Known Plinian Eruption of Cerro Machin Volcano, Colombia
THE STORAGE, TRANSPORT, AND ERUPTION OF MAGMA USING FIELD OBSERVATIONS, LABORATORY APPROACHES, AND MODELING II ORAL
volcanology, geochemistry and petrology | 13 december 2022
Silvia Castilla , Philip M. Piccoli, Megan E. New...
Measurements of magmatic volatiles and mineral chemistry provide vital insights on the history of magma storage and ascent beneath volcanic systems [1...
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Water-in-Plagioclase Hygrometry: New Partitioning Experiments and Evidence for Superhydrous Magma Beneath Cerro Machin Volcano, Colombia
CHEMISTRY, MECHANICS, GEOPHYSICS, AND TIMESCALES OF MAGMATIC PROCESSES I ORAL
volcanology, geochemistry and petrology | 12 december 2022
Megan E. Newcombe, Liam Peterson, Silvia Castilla...
The slower diffusion of water in plagioclase relative to other nominally anhydrous minerals [1] means that plagioclase has great potential as a hygrom...
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