Kendra J. Lynn, Ph.D.
My research leverages petrology and geochemistry to investigate the timescales of geologic processes operating in Earth’s mantle and volcanic systems – from the generation of magma during melting to its eruption. Understanding the timing and duration of magma storage and transport is critical for constraining the dynamic evolution of our planet and volcanic eruption scenarios.
A bit more about me: I am a first-generation college student who grew up in a small farm town in rural Minnesota and I have always loved volcanoes. As an undergraduate student at Winona State University, I did two senior thesis projects: one on soil chemistry for an organic farm and the second on structural geology and metamorphic petrology of a shear zone in Maine.
Professional Experience
CONVERSE H-SAC (Community Network for Volcanic Eruption Response Hawai'i Scientific Advisory Committee, HVO Representative), Volcano Science Center Seminar Series Committee (HVO Representative)
Research Geologist, US Geological Survey Hawaiian Volcano Observatory (2020-present) - Petrologic and geochemical studies of Hawaiian volcanoes
Postdoctoral Researcher, Department of Earth Sciences, University of Delaware (2017-2020) - Aqueous fluid-rock and silicate melt-rock interactions that re-equilibrate hydrogen in peridotite nominally anhydrous minerals; high temperature hydrothermal alteration in Gakkel Ridge abyssal peridotites
Research Associate, National Museum of Natural History, Smithsonian Institution (2017-2020) - Redox and source heterogeneity of the arctic Gakkel Ridge
Research Fellow, East Asia and Pacific Summer Institutes, Earth Observatory of Singapore, Nanyang Technological University (2015) - Investigating magma ascent rate and eruption style at Kīlauea Volcano using diffusion modeling of element zoning in olivine crystals
Research Assistant, Department of Geology and Geophysics, University of Hawai‘i at Mānoa (2012-2017) - Compositional Zoning in Kīlauea Olivine: A geochemical tool for investigating magmatic processes at Hawaiian Volcanoes
Education and Certifications
University of Hawai‘i at Mānoa, Ph.D. (2017) - Geology and Geophysics
University of Hawai‘i at Mānoa, M.S. en route (2015) - Geology and Geophysics
Winona State University, B.S. (2012) - Geology
Affiliations and Memberships*
American Geophysical Union
Geological Society of America
Mineralogical Society of America
Earth Science Women's Network
Honors and Awards
PI, Evaluating the causes of protracted explosive eruptions at Kīlauea Volcano, Hawai‘i, National Science Foundation, EAR-1939964 ($255,595). Co-PI Jessica M. Warren
Abstracts and Presentations
Selected Conference Presentations
2021 (Invited, Session Keynote) - Lynn, K.J. Big changes at Kilauea Volcano: The impact of 2018 summit collapse on magmatic processes recorded by the 2020 eruption. Geological Society of America Annual Meeting, Abstracts with Programs, 53(6), doi: 10.1130/abs/2021AM-366992.
2020 (Invited, Early Career Innovative Session on Petrology and Volcanism) - Lynn, K.J., Swanson, D.A., Rose, T., Trusdell, F.A. Leveraging geochemistry and petrology to explore the origins of explosive vs. effusive eruptive periods at Kīlauea Volcano (HI). Abstract INV10d-0003, AGU Virtual Fall Meeting.
2020 (Invited) - Lynn, K.J., Rose, T., Swanson, D.A. Olivine and glass chemistry record cycles of plumbing system evolution after summit collapse at Kīlauea Volcano, Hawai‘i. Virtual Goldschmidt Conference. doi: 10.46427/gold2020.1670.
2019 (Invited) - Lynn, K.J., Garcia, M.O., Shea, T. Phosphorus coupling obfuscates lithium geospeedometry in olivine. Abstract V43A-06, AGU Fall Meeting, San Francisco, CA.
Science and Products
Mauna Loa 2022 Eruption Lava and Tephra Chemistry by Wavelength Dispersive X-ray Fluorescence (WD-XRF) Mauna Loa 2022 Eruption Lava and Tephra Chemistry by Wavelength Dispersive X-ray Fluorescence (WD-XRF)
Samples of the Mauna Loa 2022 eruption were collected throughout the 15 days of the eruption, and from all eruptive vents, by the U.S. Geological Survey. Emphasis was placed on obtaining water-quenched flow samples, spatter and volcanic bombs wherever possible. This was not possible for the early Moku‘āweoweo, Southwest Rift Zone and upper Northeast Rift Zone vents which erupted during...
Sample details and near-real-time ED-XRF data collected during the 2020-2023 Halema‘uma‘u eruptions of Kīlauea volcano, Island of Hawaiʻi Sample details and near-real-time ED-XRF data collected during the 2020-2023 Halema‘uma‘u eruptions of Kīlauea volcano, Island of Hawaiʻi
A limited suite of samples for the 2020–2023 Kīlauea eruptions within Kaluapele (the summit caldera) were collected by the U.S. Geological Survey’s Hawaiian Volcano Observatory (HVO) field teams from within a publicly closed area of Hawai‘i Volcanoes National Park in cooperation with the National Park Service. This data release presents sample metadata, whole rock ED-XRF, whole rock WD...
Colorimeter data for the summit water lake at Kīlauea Volcano, Island of Hawaiʻi, 2020 Colorimeter data for the summit water lake at Kīlauea Volcano, Island of Hawaiʻi, 2020
In 2018, a large effusive eruption on the lower flank of Kīlauea Volcano was associated with collapse and subsidence of the summit caldera floor (Neal and others, 2019). The bottom of Halemaʻumaʻu, a crater nested within the summit caldera, subsided by more than 500 m. In July 2019, water was observed ponding on the deepest part of the Halemaʻumaʻu crater floor and the water rose and...
Sample details and near-real-time ED-XRF, grain size, and grain shape data collected during the November – December 2022 eruption of Mauna Loa volcano, Island of Hawaiʻi Sample details and near-real-time ED-XRF, grain size, and grain shape data collected during the November – December 2022 eruption of Mauna Loa volcano, Island of Hawaiʻi
At 11:21 p.m. (Hawaii Standard Time [HST]) on November 27, 2022, Mauna Loa volcano on the Island of Hawaiʻi started erupting from fissures at its summit caldera, Mokuʻāweoweo. This was followed shortly afterwards by the opening of a segment of fissures in the direction of the Southwest Rift Zone. These were mostly within the structural boundary of the caldera, so their location is...
Olivine and glass analyses for select eruptions of Kilauea Volcano, Hawai'i Olivine and glass analyses for select eruptions of Kilauea Volcano, Hawai'i
Olivine and glass major and minor element chemistry for select eruptions of Kilauea Volcano, Hawai'i as measured by electron microprobe, with secondary standard analyses.
Water-level data for the crater lake at the summit of Kilauea Volcano, Island of Hawai'i, 2019-2020 Water-level data for the crater lake at the summit of Kilauea Volcano, Island of Hawai'i, 2019-2020
During 2018, Kilauea Volcano, on the Island of Hawaiii, had a large effusive eruption (~1 cubic kilometer of lava) on the lower East Rift Zone that caused widespread destruction (Neal and others, 2019; Dietterich and others, 2021). This lower flank eruption was accompanied by one of the largest collapses of the summit caldera in two hundred years, with portions of the caldera floor...
Filter Total Items: 19
Crustal to mantle melt storage during the evolution of Hawaiian volcanoes Crustal to mantle melt storage during the evolution of Hawaiian volcanoes
As the Pacific Plate migrates over the mantle plume below Hawaiʻi, magma flux decreases, resulting in changes in eruptive volume, style, and composition. It is thought that melt storage becomes deeper and ephemeral with the transition from highly voluminous tholeiitic (shield stage) to the less voluminous alkaline (post-shield and rejuvenation stages) magmatism. To quantitatively test...
Authors
Esteban Gazel, Kyle Dayton, Wenwei Liang, Junlin Hua, Kendra J. Lynn, Julia E. Hammer
Rhenium-osmium and oxygen isotope homogeneity during the 2022 Mauna Loa eruption and implications for basaltic magma storage Rhenium-osmium and oxygen isotope homogeneity during the 2022 Mauna Loa eruption and implications for basaltic magma storage
Mauna Loa is one of the largest and most active volcanoes on Earth. The most recent eruption of Mauna Loa started on 27 November 2022, lasted for 13 days, and was preceded by the longest repose time of 38 years in its modern history. In this contribution, new trace- and highly siderophile-element (HSE: Os, Ir, Ru, Pt, Pd, Re) abundances, 187Re-187Os, and 18O/16O data are reported for the...
Authors
Emily A. Rhoads, Anton Kutyrev, Ilya N. Bindeman, Kendra J. Lynn, Frank A. Trusdell, Drew T. Downs, Hunter R. Edwards, Geoffrey W. Cook, James M.D. Day
Chemical and isotopic fractionation during melt inclusion formation Chemical and isotopic fractionation during melt inclusion formation
Melt inclusions are used to study the origin and evolution of magmas. The extent to which they represent equilibrium melt compositions, however, critically hinges on the ratio of crystal growth rate to diffusion rate in melts. If the rate of crystal growth is limited by the supply of nutrients and the dissipation of unwanted components, the trapped melt will be depleted in compatible...
Authors
Bruna da Silva Ricardo, Martin Oeser, Kendra J. Lynn, Neil Bennett, Xu Chu, Grace Henderson, Y. Liu, Stephan Weyer, Corliss Kin I Sio
The progression of basaltic–rhyolitic melt storage at Yellowstone Caldera The progression of basaltic–rhyolitic melt storage at Yellowstone Caldera
Yellowstone Caldera is one of the largest volcanic systems on Earth, hosting three major caldera-forming eruptions in the past two million years, interspersed with periods of less explosive, smaller-volume eruptions1. Caldera-forming eruptions at Yellowstone are sourced by rhyolitic melts stored within the mid- to upper crust. Seismic tomography studies have suggested that a broad region...
Authors
Ninfa Lucia Bennington, Adam Schultz, Paul A. Bedrosian, Esteban Bowles-Martinez, Kendra J. Lynn, Mark E. Stelten, Xiaolei Tu, Clifford Thurber
Considerations and perspectives on pregnancy and fieldwork Considerations and perspectives on pregnancy and fieldwork
Fieldwork is integral to geoscience but can come with risks that increase for fieldworkers who are pregnant. Consultation with medical staff and completion of risk assessments are essential steps, but pregnant individuals also benefit from supportive colleagues, reasonable accommodations, and the freedom to adapt plans as pregnancy progresses.
Authors
Jennifer L. Jenkins, Beth A. Johnson, Kendall Valentine, Kendra J. Lynn
Awakening of Maunaloa linked to melt shared from Kilauea’s mantle source Awakening of Maunaloa linked to melt shared from Kilauea’s mantle source
Maunaloa—the largest active volcano on Earth—erupted in 2022 after its longest known repose period (~38 years) and two decades of volcanic unrest. This eruptive hiatus at Maunaloa encompasses most of the ~35-year-long Puʻuʻōʻō eruption of neighboring Kīlauea, which ended in 2018 with a collapse of the summit caldera and an unusually voluminous (~1 km3) rift eruption. A long-term pattern...
Authors
Aaron J. Pietruszka, Daniel E. Heaton, Jared P. Marske, Marc D. Norman, Mahinaokalani G. Robbins, Reed B. Mershon, Kendra J. Lynn, Drew T. Downs, Arron R. Steiner, J. Michael Rhodes, Michael O. Garcia
Triggering the 2022 eruption of Mauna Loa Triggering the 2022 eruption of Mauna Loa
Distinguishing periods of intermittent unrest from the run-up to eruption is a major challenge at volcanoes around the globe. Comparing multidisciplinary monitoring data with mineral chemistry that records the physical and spatio-temporal evolution of magmas fundamentally advances our ability to forecast eruptions. The recent eruption of Mauna Loa, Earth’s largest active volcano...
Authors
Kendra J. Lynn, Drew T. Downs, Frank A. Trusdell, Penny E. Wieser, Berenise Rangel, Baylee Rose McDade, Alicia J. Hotovec-Ellis, Ninfa Lucia Bennington, Kyle R. Anderson, Dawn Catherine Sweeney Ruth, Charlotte DeVitre, Andria P. Ellis, Patricia A. Nadeau, Laura E. Clor, Peter J. Kelly, Peter Dotray, Jefferson Chang
Depths in a day - A new era of rapid-response Raman-based barometry using fluid inclusions Depths in a day - A new era of rapid-response Raman-based barometry using fluid inclusions
Rapid-response petrological monitoring is a major advance for volcano observatories, allowing them to build and validate models of plumbing systems that supply eruptions in near-real-time. The depth of magma storage has recently been identified as high-priority information for volcanic observatories, yet this information is not currently obtainable via petrological monitoring methods on...
Authors
Charlotte DeVitre, Penny E. Wieser, Alexander T. Bearden, Araela Richie, Berenise Rangel, Matthew Gleeson, John Grimsich, Kendra J. Lynn, Drew T. Downs, Natalia I. Deligne, Katherine M. Mulliken
Reexamining the Honolulu Volcanics: Hawai‘i's classic case of rejuvenation volcanism Reexamining the Honolulu Volcanics: Hawai‘i's classic case of rejuvenation volcanism
Rejuvenated volcanism is a worldwide phenomenon occurring on many oceanic islands in all of the major ocean basins. This plume-related volcanism follows the main edifice-building stage after a hiatus of variable duration (e.g. 0.6–2 Myrs in Hawai'i). The Honolulu Volcanics (HV), the classic case of rejuvenated volcanism, involved monogenetic eruptions from at least 48 vent areas...
Authors
Michael O. Garcia, Marc D. Norman, Brian Jicha, Kendra J. Lynn, Peng Jiang
Olivine diffusion constrains months-scale magma transport within Kīlauea volcano’s summit reservoir system prior to the 2020 eruption Olivine diffusion constrains months-scale magma transport within Kīlauea volcano’s summit reservoir system prior to the 2020 eruption
The unprecedented 2018 summit collapse at Kīlauea and subsequent 2020–2021 eruption within the newly deepened Halema‘uma‘u Crater provide an unparalleled opportunity to understand how collapse events impact a volcano’s shallow reservoir system and magmatic processes. Glass and olivine from tephra ejected by lava fountains and several explosions on 20–21 December, within a few hours of...
Authors
Kendra J. Lynn, Patricia A. Nadeau, Dawn Catherine Sweeney Ruth, Jefferson Chang, Peter Dotray, Ingrid A. Johanson
Dynamics of magma mixing and magma mobilization beneath Mauna Loa – Insights from the 1950 AD Southwest Rift Zone eruption. Dynamics of magma mixing and magma mobilization beneath Mauna Loa – Insights from the 1950 AD Southwest Rift Zone eruption.
Eruptions from Mauna Loa’s Southwest Rift Zone (SWRZ) pose a significant threat to nearby communities due to high eruption rates and steep slopes resulting in little time for evacuation. Despite the large body of research done on Mauna Loa, knowledge of the timing and duration of magma residence and transfer through its internal plumbing system is still poorly constrained. This study...
Authors
Maren Kahl, Daniel J. Morgan, Carl Thornber, Richard Walshaw, Kendra J. Lynn, Frank A. Trusdell
Creating oriented and precisely sectioned mineral mounts for in situ chemical analyses—An example using olivine for diffusion chronometry studies Creating oriented and precisely sectioned mineral mounts for in situ chemical analyses—An example using olivine for diffusion chronometry studies
Diffusion chronometry is now a widely applied methodology for determining the rates and timescales of geologic processes from the chemical zoning observed in minerals. Despite the popularity of the method, several challenges still remain during its application, including: (1) the random sectioning of minerals either in thin sections or grain mounts in which both off-center and oblique...
Authors
Kendra J. Lynn, Liliana G. Desmither
Baydiff: Bayesian diffusion chronometry for volcanic systems Baydiff: Bayesian diffusion chronometry for volcanic systems
Diffusion chronometry is a powerful tool for estimating the time scales of magmatic processes. This MATLAB software can be used to estimate diffusion time scales using the forsterite content of olivine crystals. Estimates are obtained probabilistically, using a Bayesian framework, and account for uncertainties in data as well as any independent (prior) information.
Science and Products
Mauna Loa 2022 Eruption Lava and Tephra Chemistry by Wavelength Dispersive X-ray Fluorescence (WD-XRF) Mauna Loa 2022 Eruption Lava and Tephra Chemistry by Wavelength Dispersive X-ray Fluorescence (WD-XRF)
Samples of the Mauna Loa 2022 eruption were collected throughout the 15 days of the eruption, and from all eruptive vents, by the U.S. Geological Survey. Emphasis was placed on obtaining water-quenched flow samples, spatter and volcanic bombs wherever possible. This was not possible for the early Moku‘āweoweo, Southwest Rift Zone and upper Northeast Rift Zone vents which erupted during...
Sample details and near-real-time ED-XRF data collected during the 2020-2023 Halema‘uma‘u eruptions of Kīlauea volcano, Island of Hawaiʻi Sample details and near-real-time ED-XRF data collected during the 2020-2023 Halema‘uma‘u eruptions of Kīlauea volcano, Island of Hawaiʻi
A limited suite of samples for the 2020–2023 Kīlauea eruptions within Kaluapele (the summit caldera) were collected by the U.S. Geological Survey’s Hawaiian Volcano Observatory (HVO) field teams from within a publicly closed area of Hawai‘i Volcanoes National Park in cooperation with the National Park Service. This data release presents sample metadata, whole rock ED-XRF, whole rock WD...
Colorimeter data for the summit water lake at Kīlauea Volcano, Island of Hawaiʻi, 2020 Colorimeter data for the summit water lake at Kīlauea Volcano, Island of Hawaiʻi, 2020
In 2018, a large effusive eruption on the lower flank of Kīlauea Volcano was associated with collapse and subsidence of the summit caldera floor (Neal and others, 2019). The bottom of Halemaʻumaʻu, a crater nested within the summit caldera, subsided by more than 500 m. In July 2019, water was observed ponding on the deepest part of the Halemaʻumaʻu crater floor and the water rose and...
Sample details and near-real-time ED-XRF, grain size, and grain shape data collected during the November – December 2022 eruption of Mauna Loa volcano, Island of Hawaiʻi Sample details and near-real-time ED-XRF, grain size, and grain shape data collected during the November – December 2022 eruption of Mauna Loa volcano, Island of Hawaiʻi
At 11:21 p.m. (Hawaii Standard Time [HST]) on November 27, 2022, Mauna Loa volcano on the Island of Hawaiʻi started erupting from fissures at its summit caldera, Mokuʻāweoweo. This was followed shortly afterwards by the opening of a segment of fissures in the direction of the Southwest Rift Zone. These were mostly within the structural boundary of the caldera, so their location is...
Olivine and glass analyses for select eruptions of Kilauea Volcano, Hawai'i Olivine and glass analyses for select eruptions of Kilauea Volcano, Hawai'i
Olivine and glass major and minor element chemistry for select eruptions of Kilauea Volcano, Hawai'i as measured by electron microprobe, with secondary standard analyses.
Water-level data for the crater lake at the summit of Kilauea Volcano, Island of Hawai'i, 2019-2020 Water-level data for the crater lake at the summit of Kilauea Volcano, Island of Hawai'i, 2019-2020
During 2018, Kilauea Volcano, on the Island of Hawaiii, had a large effusive eruption (~1 cubic kilometer of lava) on the lower East Rift Zone that caused widespread destruction (Neal and others, 2019; Dietterich and others, 2021). This lower flank eruption was accompanied by one of the largest collapses of the summit caldera in two hundred years, with portions of the caldera floor...
Filter Total Items: 19
Crustal to mantle melt storage during the evolution of Hawaiian volcanoes Crustal to mantle melt storage during the evolution of Hawaiian volcanoes
As the Pacific Plate migrates over the mantle plume below Hawaiʻi, magma flux decreases, resulting in changes in eruptive volume, style, and composition. It is thought that melt storage becomes deeper and ephemeral with the transition from highly voluminous tholeiitic (shield stage) to the less voluminous alkaline (post-shield and rejuvenation stages) magmatism. To quantitatively test...
Authors
Esteban Gazel, Kyle Dayton, Wenwei Liang, Junlin Hua, Kendra J. Lynn, Julia E. Hammer
Rhenium-osmium and oxygen isotope homogeneity during the 2022 Mauna Loa eruption and implications for basaltic magma storage Rhenium-osmium and oxygen isotope homogeneity during the 2022 Mauna Loa eruption and implications for basaltic magma storage
Mauna Loa is one of the largest and most active volcanoes on Earth. The most recent eruption of Mauna Loa started on 27 November 2022, lasted for 13 days, and was preceded by the longest repose time of 38 years in its modern history. In this contribution, new trace- and highly siderophile-element (HSE: Os, Ir, Ru, Pt, Pd, Re) abundances, 187Re-187Os, and 18O/16O data are reported for the...
Authors
Emily A. Rhoads, Anton Kutyrev, Ilya N. Bindeman, Kendra J. Lynn, Frank A. Trusdell, Drew T. Downs, Hunter R. Edwards, Geoffrey W. Cook, James M.D. Day
Chemical and isotopic fractionation during melt inclusion formation Chemical and isotopic fractionation during melt inclusion formation
Melt inclusions are used to study the origin and evolution of magmas. The extent to which they represent equilibrium melt compositions, however, critically hinges on the ratio of crystal growth rate to diffusion rate in melts. If the rate of crystal growth is limited by the supply of nutrients and the dissipation of unwanted components, the trapped melt will be depleted in compatible...
Authors
Bruna da Silva Ricardo, Martin Oeser, Kendra J. Lynn, Neil Bennett, Xu Chu, Grace Henderson, Y. Liu, Stephan Weyer, Corliss Kin I Sio
The progression of basaltic–rhyolitic melt storage at Yellowstone Caldera The progression of basaltic–rhyolitic melt storage at Yellowstone Caldera
Yellowstone Caldera is one of the largest volcanic systems on Earth, hosting three major caldera-forming eruptions in the past two million years, interspersed with periods of less explosive, smaller-volume eruptions1. Caldera-forming eruptions at Yellowstone are sourced by rhyolitic melts stored within the mid- to upper crust. Seismic tomography studies have suggested that a broad region...
Authors
Ninfa Lucia Bennington, Adam Schultz, Paul A. Bedrosian, Esteban Bowles-Martinez, Kendra J. Lynn, Mark E. Stelten, Xiaolei Tu, Clifford Thurber
Considerations and perspectives on pregnancy and fieldwork Considerations and perspectives on pregnancy and fieldwork
Fieldwork is integral to geoscience but can come with risks that increase for fieldworkers who are pregnant. Consultation with medical staff and completion of risk assessments are essential steps, but pregnant individuals also benefit from supportive colleagues, reasonable accommodations, and the freedom to adapt plans as pregnancy progresses.
Authors
Jennifer L. Jenkins, Beth A. Johnson, Kendall Valentine, Kendra J. Lynn
Awakening of Maunaloa linked to melt shared from Kilauea’s mantle source Awakening of Maunaloa linked to melt shared from Kilauea’s mantle source
Maunaloa—the largest active volcano on Earth—erupted in 2022 after its longest known repose period (~38 years) and two decades of volcanic unrest. This eruptive hiatus at Maunaloa encompasses most of the ~35-year-long Puʻuʻōʻō eruption of neighboring Kīlauea, which ended in 2018 with a collapse of the summit caldera and an unusually voluminous (~1 km3) rift eruption. A long-term pattern...
Authors
Aaron J. Pietruszka, Daniel E. Heaton, Jared P. Marske, Marc D. Norman, Mahinaokalani G. Robbins, Reed B. Mershon, Kendra J. Lynn, Drew T. Downs, Arron R. Steiner, J. Michael Rhodes, Michael O. Garcia
Triggering the 2022 eruption of Mauna Loa Triggering the 2022 eruption of Mauna Loa
Distinguishing periods of intermittent unrest from the run-up to eruption is a major challenge at volcanoes around the globe. Comparing multidisciplinary monitoring data with mineral chemistry that records the physical and spatio-temporal evolution of magmas fundamentally advances our ability to forecast eruptions. The recent eruption of Mauna Loa, Earth’s largest active volcano...
Authors
Kendra J. Lynn, Drew T. Downs, Frank A. Trusdell, Penny E. Wieser, Berenise Rangel, Baylee Rose McDade, Alicia J. Hotovec-Ellis, Ninfa Lucia Bennington, Kyle R. Anderson, Dawn Catherine Sweeney Ruth, Charlotte DeVitre, Andria P. Ellis, Patricia A. Nadeau, Laura E. Clor, Peter J. Kelly, Peter Dotray, Jefferson Chang
Depths in a day - A new era of rapid-response Raman-based barometry using fluid inclusions Depths in a day - A new era of rapid-response Raman-based barometry using fluid inclusions
Rapid-response petrological monitoring is a major advance for volcano observatories, allowing them to build and validate models of plumbing systems that supply eruptions in near-real-time. The depth of magma storage has recently been identified as high-priority information for volcanic observatories, yet this information is not currently obtainable via petrological monitoring methods on...
Authors
Charlotte DeVitre, Penny E. Wieser, Alexander T. Bearden, Araela Richie, Berenise Rangel, Matthew Gleeson, John Grimsich, Kendra J. Lynn, Drew T. Downs, Natalia I. Deligne, Katherine M. Mulliken
Reexamining the Honolulu Volcanics: Hawai‘i's classic case of rejuvenation volcanism Reexamining the Honolulu Volcanics: Hawai‘i's classic case of rejuvenation volcanism
Rejuvenated volcanism is a worldwide phenomenon occurring on many oceanic islands in all of the major ocean basins. This plume-related volcanism follows the main edifice-building stage after a hiatus of variable duration (e.g. 0.6–2 Myrs in Hawai'i). The Honolulu Volcanics (HV), the classic case of rejuvenated volcanism, involved monogenetic eruptions from at least 48 vent areas...
Authors
Michael O. Garcia, Marc D. Norman, Brian Jicha, Kendra J. Lynn, Peng Jiang
Olivine diffusion constrains months-scale magma transport within Kīlauea volcano’s summit reservoir system prior to the 2020 eruption Olivine diffusion constrains months-scale magma transport within Kīlauea volcano’s summit reservoir system prior to the 2020 eruption
The unprecedented 2018 summit collapse at Kīlauea and subsequent 2020–2021 eruption within the newly deepened Halema‘uma‘u Crater provide an unparalleled opportunity to understand how collapse events impact a volcano’s shallow reservoir system and magmatic processes. Glass and olivine from tephra ejected by lava fountains and several explosions on 20–21 December, within a few hours of...
Authors
Kendra J. Lynn, Patricia A. Nadeau, Dawn Catherine Sweeney Ruth, Jefferson Chang, Peter Dotray, Ingrid A. Johanson
Dynamics of magma mixing and magma mobilization beneath Mauna Loa – Insights from the 1950 AD Southwest Rift Zone eruption. Dynamics of magma mixing and magma mobilization beneath Mauna Loa – Insights from the 1950 AD Southwest Rift Zone eruption.
Eruptions from Mauna Loa’s Southwest Rift Zone (SWRZ) pose a significant threat to nearby communities due to high eruption rates and steep slopes resulting in little time for evacuation. Despite the large body of research done on Mauna Loa, knowledge of the timing and duration of magma residence and transfer through its internal plumbing system is still poorly constrained. This study...
Authors
Maren Kahl, Daniel J. Morgan, Carl Thornber, Richard Walshaw, Kendra J. Lynn, Frank A. Trusdell
Creating oriented and precisely sectioned mineral mounts for in situ chemical analyses—An example using olivine for diffusion chronometry studies Creating oriented and precisely sectioned mineral mounts for in situ chemical analyses—An example using olivine for diffusion chronometry studies
Diffusion chronometry is now a widely applied methodology for determining the rates and timescales of geologic processes from the chemical zoning observed in minerals. Despite the popularity of the method, several challenges still remain during its application, including: (1) the random sectioning of minerals either in thin sections or grain mounts in which both off-center and oblique...
Authors
Kendra J. Lynn, Liliana G. Desmither
Baydiff: Bayesian diffusion chronometry for volcanic systems Baydiff: Bayesian diffusion chronometry for volcanic systems
Diffusion chronometry is a powerful tool for estimating the time scales of magmatic processes. This MATLAB software can be used to estimate diffusion time scales using the forsterite content of olivine crystals. Estimates are obtained probabilistically, using a Bayesian framework, and account for uncertainties in data as well as any independent (prior) information.
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government