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Understanding how climate change will affect the flooding of rivers may become easier with a new framework for assessing flood risk that's been developed by an interdisciplinary team from Penn State.
A recently dedicated lab at Penn State bears the name of a longtime geosciences faculty member who used isotope geochemistry to better understand processes deep within the Earth.
The Peter Deines Isotope Mass Spectrometry Laboratory was dedicated on Oct. 28 in a ribbon-cutting ceremony officiated by Penn State President Eric Barron, Geosciences Department Head Andrew Nyblade, Evan Pugh University Professor Katherine Freeman, John Leone Dean in the College of Earth and Mineral Sciences (EMS) Lee Kump, Melissa Deines, wife of the late Peter Deines, Senior Vice President for Research Lora Weis and Emeritus Professor and Former Associate Dean of the college’s Office of Graduate Education and Research John Hellmann.
Susan Brantley, professor of geosciences and director of the Earth and Environmental Systems Institute, was selected to receive the inaugural Dr. Hubert Barnes and Dr. Mary Barnes Professorship in Geosciences.
The mechanism behind one of the first stages of coal creation may not be what has long been thought, according to a team of researchers who found that microbes were responsible for coal formation and production of methane. The finding has implications for methane fuel recovery from some coal fields.
Schedule of Events
Zoom Link: https://psu.zoom.us/s/94992382444
2:00pm Ribbon cutting and remarks by:
• Andrew Nyblade, Head of the Department of G eosciences;
• Eric Barron, President of Penn State;
• Katherine Freeman, Evan Pugh University Professor;
• Lee Kump, John Leone Dean in the College of Earth and Mineral Sciences; and
• Melissa M. Deines, Ph.D.
2:20pm Open house and tours; poster session
3:20pm Reception in Foundry Parklet (under the tent)
4:30pm CoIIoquium virtuaI talk by Barbara Sherwood Lollar: "Imaging Habitable Worlds - Lessons from the Deep Biosphere Hydrogeosphere" Zoom link: https://psu.zoom.us/j/95787957863?pwd=M2pvWWt5bH
pPbGFUWXRmQktoNHlhdz09 Also join group to watch Zoom in 220 Hammond Building.
A new endowed professorship in the Department of Geosciences in the College of Earth and Mineral Sciences honors the legacy of husband-and-wife Penn State researchers, one a distinguished professor emeritus in the department.
The flooding caused by Hurricane Ida across the Southeast and Mid-Atlantic regions provides a glimpse at the disasters threatening coastal communities as the climate warms. These disasters often disproportionately affect communities of color and other historically underserved neighborhoods. A $19.9 million grant from the National Science Foundation’s Coastlines and People Program (CoPe) will help to bring researchers and stakeholders together to equitably support coastal communities to better manage coastal climate risks.
Bradford Foley and Kimberly Lau, both assistant geosciences professors in Penn State’s College of Earth and Mineral Sciences, are part of the eight multidisciplinary teams of researchers selected to receive funding in the inaugural year of "Scialog: Signatures of Life in the Universe," a new research initiative designed to bring the world closer to answering basic questions about the possibility of extraterrestrial life.
Investigation of subsurface environments and subsurface processes is becoming more and more important in our understanding of planetary evolution, habitability and the search for life. Barbara Sherwood Lollar, University Professor in Earth Sciences and Dr. Norman Keevil Chair in Ore Deposits Geology at the University of Toronto, will discuss her research on this topic in the talk, "Imaging Habitable Worlds – Lessons from the Deep Biosphere and Hydrogeosphere."
By Davitia James, Temblor Earthquake News Extern (@davitiaa)
Citation: James, D., 2021, Fluids and tiny minerals play a big role in subduction zones, Temblor, http://doi.org/10.32858/temblor.213
The Earth’s surface is constantly moving as tectonic plates slide past, rip away from, and bump into each other. All this commotion commonly creates earthquakes at plate boundaries, but these seismic events are not evenly spaced, geographically speaking. Why do earthquakes happen more often along some parts of a plate boundary? And why do some places seem to escape large seismic events?