Hannah R. Dietterich, Ph.D.
Hannah works on eruption dynamics, remote sensing, and quantitative volcanic hazard assessment at the USGS Alaska Volcano Observatory in Anchorage, AK.
Hannah Dietterich is a Research Geophysicist at the U.S. Geological Survey Alaska Volcano Observatory. Her work focuses on the physics of volcanic processes, remote sensing of volcanic activity, numerical modeling of volcanic hazards, and probabilistic volcanic hazard assessment. She integrates geologic mapping, physical volcanology, remote sensing, and numerical modeling with observations of ongoing eruptions to advance our understanding of volcanic hazards.
Professional Experience
2018–present, Research Geophysicist, USGS Alaska Volcano Observatory, Anchorage, AK
2015–2018, Research Geologist (postdoc), USGS Volcano Science Center, Menlo Park, CA
2014–2014, Postdoctoral Research Associate, University of Oregon, Eugene, OR and University of Bristol, Bristol, UK
2013–2014, Graduate Teaching Fellow, University of Oregon, Eugene, OR
2010–2013, NSF Graduate Research Fellow, University of Oregon, Eugene, OR
2009–2010, Graduate Teaching Fellow, University of Oregon, Eugene, OR
Education and Certifications
University of Oregon: Ph.D. (2014), Geological Sciences
Pomona College: B.A. (2009), Geology
Science and Products
Filter Total Items: 40
Cyclic lava effusion during the 2018 eruption of Kīlauea Volcano
Lava flows present a recurring threat to communities on active volcanoes, and volumetric eruption rate is one of the primary factors controlling flow behavior and hazard. The timescales and driving forces of eruption rate variability, however, remain poorly understood. In 2018, a highly destructive eruption occurred on the lower flank of Kīlauea Volcano, Hawaiʻi, where the primary vent...
Authors
Matthew R. Patrick, Hannah R. Dietterich, John J. Lyons, Angie Diefenbach, Carolyn Parcheta, Kyle R. Anderson, Atsuko Namiki, Ikuro Sumita, Brian Shiro, James P. Kauahikaua
Topographic changes during the 2018 Kīlauea eruption from Single-pass Airborne InSAR
The 2018 eruption of Kīlauea volcano, Hawai‘i, was its most effusive in over 200 years. We apply the airborne Glacier and Ice Surface Topography Interferometer (GLISTIN‐A) interferometric synthetic aperture radar (InSAR) instrument to measure topographic change associated with the eruption. The GLISTIN‐A radar flew in response to the eruption, acquiring observations of Kīlauea on seven...
Authors
Paul Lundgren, Marco Bagnardi, Hannah R. Dietterich
Lava flow morphology at an erupting andesitic stratovolcano: A satellite perspective on El Reventador, Ecuador
Lava flows pose a significant hazard to infrastructure and property located close to volcanoes, and understanding how flows advance is necessary to manage volcanic hazard during eruptions. Compared to low-silica basaltic flows, flows of andesitic composition are infrequently erupted and so relatively few studies of their characteristics and behaviour exist. We use El Reventador, Ecuador...
Authors
David W. D. Arnold, Juliet Biggs, Hannah R. Dietterich, Silvia Vallejo Vargas, Geoffrey Wadge, Patricia A. Mothes
The 2018 rift eruption and summit collapse of Kilauea Volcano
In 2018, Kīlauea Volcano experienced its largest lower East Rift Zone (LERZ) eruption and caldera collapse in at least 200 years. After collapse of the Pu'u 'Ō'ō vent on 30 April, magma propagated downrift. Eruptive fissures opened in the LERZ on 3 May, eventually extending ~6.8 km. A 4 May earthquake (M6.9) produced ~5 m of fault slip. Lava erupted at rates exceeding 100 m3/s...
Authors
Christina A. Neal, Steven Brantley, Loren Antolik, Janet Babb, Matthew Alexander Burgess, Michael Cappos, Jefferson Chang, Sarah Conway, Liliana G. Desmither, Peter Dotray, Tamar Elias, Pauline Fukunaga, Steven Fuke, Ingrid A. Johanson, Kevan Kamibayashi, James P. Kauahikaua, R. Lopaka Lee, S. Pekalib, Asta Miklius, Brian Shiro, Don Swanson, Patricia A. Nadeau, Michael H. Zoeller, Paul G. Okubo, Carolyn Parcheta, Matthew R. Patrick, William Tollett, Frank Trusdell, Edward F. Younger, Emily K. Montgomery-Brown, Kyle R. Anderson, Michael P. Poland, Jessica L. Ball, Joseph A. Bard, Michelle L. Coombs, Hannah R. Dietterich, Christoph Kern, Weston A. Thelen, Peter F. Cervelli, Tim R. Orr, Bruce F. Houghton, Cheryl Gansecki, Richard W. Hazlett, Paul Lundgren, Angie Diefenbach, Allan Lerner, Greg Waite, Peter J. Kelly, Laura Clor, Cynthia A. Werner, Katherine M. Mulliken, Gary B. Fisher, David Damby
Reconstructing lava flow emplacement histories with rheological and morphological analyses: the Harrat Rahat volcanic field, Kingdom of Saudi Arabia
Mafic volcanic fields are widespread, but few have erupted in historic times, providing limited observations of the magnitudes, dynamics, and timescales of lava flow emplacement in these settings. To expand our knowledge of effusive mafic eruptions, we must evaluate solidified flows to discern syn-eruptive conditions. The Harrat Rahat volcanic field in western Saudi Arabia offers a good...
Authors
Hannah R. Dietterich, Drew T. Downs, Mark E. Stelten, Hani M. Zahran
Timescales of magmatic differentiation from alkali basalt to trachyte within the Harrat Rahat volcanic field, Kingdom of Saudi Arabia
A fundamental goal of igneous petrology is to quantify the duration of time required to produce evolved magmas following influx of basalt into the crust. However, in many cases, complex field relations and/or the presence of a long-lived magmatic system make it difficult to assess how basaltic inputs relate to more evolved magmas, therefore, precluding calculation of meaningful...
Authors
Mark E. Stelten, Drew T. Downs, Hannah R. Dietterich, Gail A. Mahood, Andrew T. Calvert, Thomas W. Sisson, Hani M. Zahran, Jamal Shawali
Non-USGS Publications**
Dietterich, H. R., Soule, S. A., Cashman, K. V. and Mackey, B. H. (2015) Lava Flows in 3D, in Hawaiian Volcanoes: From Source to Surface (eds R. Carey, V. Cayol, M. Poland and D. Weis), John Wiley & Sons, Inc, Hoboken, NJ. doi: 10.1002/9781118872079.ch22
Dietterich, H. R., and K. V. Cashman (2014), Channel networks within lava flows: Formation, evolution, and implications for flow behavior, J. Geophys. Res. Earth Surf., 119, 1704–1724, doi:10.1002/2014JF003103.
Cashman, K. V., S. A. Soule, B. H. Mackey, N. I. Deligne, N. Deardorff, and H. R. Dietterich, (2013), How lava flows: New insights from applications of lidar technologies to lava flow studies, Geosphere, 9, 1664-1680, doi:10.1130/GES00706.1.
Dietterich, H.R., and S. L. de Silva (2010), Sulfur yield of the 1600 eruption of Huaynaputina determined by apatite compositions, Journal of Volcanology and Geothermal Research, 197, 303-312, doi:10.1016/j.jvolgeores.2010.01.003.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 40
Cyclic lava effusion during the 2018 eruption of Kīlauea Volcano
Lava flows present a recurring threat to communities on active volcanoes, and volumetric eruption rate is one of the primary factors controlling flow behavior and hazard. The timescales and driving forces of eruption rate variability, however, remain poorly understood. In 2018, a highly destructive eruption occurred on the lower flank of Kīlauea Volcano, Hawaiʻi, where the primary vent...
Authors
Matthew R. Patrick, Hannah R. Dietterich, John J. Lyons, Angie Diefenbach, Carolyn Parcheta, Kyle R. Anderson, Atsuko Namiki, Ikuro Sumita, Brian Shiro, James P. Kauahikaua
Topographic changes during the 2018 Kīlauea eruption from Single-pass Airborne InSAR
The 2018 eruption of Kīlauea volcano, Hawai‘i, was its most effusive in over 200 years. We apply the airborne Glacier and Ice Surface Topography Interferometer (GLISTIN‐A) interferometric synthetic aperture radar (InSAR) instrument to measure topographic change associated with the eruption. The GLISTIN‐A radar flew in response to the eruption, acquiring observations of Kīlauea on seven...
Authors
Paul Lundgren, Marco Bagnardi, Hannah R. Dietterich
Lava flow morphology at an erupting andesitic stratovolcano: A satellite perspective on El Reventador, Ecuador
Lava flows pose a significant hazard to infrastructure and property located close to volcanoes, and understanding how flows advance is necessary to manage volcanic hazard during eruptions. Compared to low-silica basaltic flows, flows of andesitic composition are infrequently erupted and so relatively few studies of their characteristics and behaviour exist. We use El Reventador, Ecuador...
Authors
David W. D. Arnold, Juliet Biggs, Hannah R. Dietterich, Silvia Vallejo Vargas, Geoffrey Wadge, Patricia A. Mothes
The 2018 rift eruption and summit collapse of Kilauea Volcano
In 2018, Kīlauea Volcano experienced its largest lower East Rift Zone (LERZ) eruption and caldera collapse in at least 200 years. After collapse of the Pu'u 'Ō'ō vent on 30 April, magma propagated downrift. Eruptive fissures opened in the LERZ on 3 May, eventually extending ~6.8 km. A 4 May earthquake (M6.9) produced ~5 m of fault slip. Lava erupted at rates exceeding 100 m3/s...
Authors
Christina A. Neal, Steven Brantley, Loren Antolik, Janet Babb, Matthew Alexander Burgess, Michael Cappos, Jefferson Chang, Sarah Conway, Liliana G. Desmither, Peter Dotray, Tamar Elias, Pauline Fukunaga, Steven Fuke, Ingrid A. Johanson, Kevan Kamibayashi, James P. Kauahikaua, R. Lopaka Lee, S. Pekalib, Asta Miklius, Brian Shiro, Don Swanson, Patricia A. Nadeau, Michael H. Zoeller, Paul G. Okubo, Carolyn Parcheta, Matthew R. Patrick, William Tollett, Frank Trusdell, Edward F. Younger, Emily K. Montgomery-Brown, Kyle R. Anderson, Michael P. Poland, Jessica L. Ball, Joseph A. Bard, Michelle L. Coombs, Hannah R. Dietterich, Christoph Kern, Weston A. Thelen, Peter F. Cervelli, Tim R. Orr, Bruce F. Houghton, Cheryl Gansecki, Richard W. Hazlett, Paul Lundgren, Angie Diefenbach, Allan Lerner, Greg Waite, Peter J. Kelly, Laura Clor, Cynthia A. Werner, Katherine M. Mulliken, Gary B. Fisher, David Damby
Reconstructing lava flow emplacement histories with rheological and morphological analyses: the Harrat Rahat volcanic field, Kingdom of Saudi Arabia
Mafic volcanic fields are widespread, but few have erupted in historic times, providing limited observations of the magnitudes, dynamics, and timescales of lava flow emplacement in these settings. To expand our knowledge of effusive mafic eruptions, we must evaluate solidified flows to discern syn-eruptive conditions. The Harrat Rahat volcanic field in western Saudi Arabia offers a good...
Authors
Hannah R. Dietterich, Drew T. Downs, Mark E. Stelten, Hani M. Zahran
Timescales of magmatic differentiation from alkali basalt to trachyte within the Harrat Rahat volcanic field, Kingdom of Saudi Arabia
A fundamental goal of igneous petrology is to quantify the duration of time required to produce evolved magmas following influx of basalt into the crust. However, in many cases, complex field relations and/or the presence of a long-lived magmatic system make it difficult to assess how basaltic inputs relate to more evolved magmas, therefore, precluding calculation of meaningful...
Authors
Mark E. Stelten, Drew T. Downs, Hannah R. Dietterich, Gail A. Mahood, Andrew T. Calvert, Thomas W. Sisson, Hani M. Zahran, Jamal Shawali
Non-USGS Publications**
Dietterich, H. R., Soule, S. A., Cashman, K. V. and Mackey, B. H. (2015) Lava Flows in 3D, in Hawaiian Volcanoes: From Source to Surface (eds R. Carey, V. Cayol, M. Poland and D. Weis), John Wiley & Sons, Inc, Hoboken, NJ. doi: 10.1002/9781118872079.ch22
Dietterich, H. R., and K. V. Cashman (2014), Channel networks within lava flows: Formation, evolution, and implications for flow behavior, J. Geophys. Res. Earth Surf., 119, 1704–1724, doi:10.1002/2014JF003103.
Cashman, K. V., S. A. Soule, B. H. Mackey, N. I. Deligne, N. Deardorff, and H. R. Dietterich, (2013), How lava flows: New insights from applications of lidar technologies to lava flow studies, Geosphere, 9, 1664-1680, doi:10.1130/GES00706.1.
Dietterich, H.R., and S. L. de Silva (2010), Sulfur yield of the 1600 eruption of Huaynaputina determined by apatite compositions, Journal of Volcanology and Geothermal Research, 197, 303-312, doi:10.1016/j.jvolgeores.2010.01.003.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.