Events
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BEG Seminar: Tamie Jovanelly - Berry College
Start:October 1, 2021 at 9:00 am
End:
October 1, 2021 at 10:00 am
Location:
Zoom
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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Exploring the quality of major river systems: lessons learned in conservation
As a hydrologist, Dr. Jovanelly has traveled the globe for more than a decade testing water quality on major river and surface water systems while asking the question, “What is the best way to promote clean water for all?” Through her qualitative and quantitative data collection it has become apparent that solving any water crisis must start with the understanding of human perceptions towards the environments in which they live and their value systems. Her global water quality data show that human connect to water differs by religious following, and intrinsic or instrumental ethos.
Dr. Tamie Jovanelly research website: https://globalwaterquality.com
Join Zoom Meeting
https://utexas.zoom.us/j/98681392151?pwd=b1hJMHFTbFk0WTJORUdqdHI5U2U5Zz09
Meeting ID: 986 8139 2151
Passcode: 102238
UTIG Seminar Series: Mark Panning, NASA Jet Propulsion Laboratory
Start:October 1, 2021 at 10:30 am
End:
October 1, 2021 at 11:30 am
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Download Presentation Slides (PDF)
Speaker: Mark Panning, NASA Jet Propulsion Laboratory
Host: Cyril Grima
Title: Planetary Seismology: Nearly 3 years on Mars, and a return to the Moon
Abstract: InSight has been recording seismic data on Mars nearly continuously since landing in November, 2018. This mission has not been without challenges, including work to get the heat flow probe to depth, and a fight to keep energy going in the absence of dust cleaning through dust devils. In this time on the surface, we’ve observed hundreds of seismic events, which have let us determine key characteristics of the martian crust, mantle, and core. Meanwhile, NASA has recently selected a set of geophysical instruments, including the Farside Seismic Suite with instruments derived from InSight, to fly on a commercial lander to Schrödinger Crater on the far side of the Moon. This will be the first seismic data recorded anywhere on the Moon since the Apollo instruments were turned off in 1977, on the most sensitive seismometer ever to record on the Moon, and the first ever on the far side of the Moon.
EPS Faculty Meeting
Start:October 5, 2021 at 12:30 pm
End:
October 5, 2021 at 1:45 pm
UTIG Discussion Hour: Zach Sickmann, UTIG
Start:October 5, 2021 at 2:00 pm
End:
October 5, 2021 at 3:00 pm
Location:
Zoom Meeting
Contact:
Naoma McCall, nmccall@utexas.edu
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Speaker: Zach Sickmann, Postdoctoral Fellow, UTIG
Title: Progress on “fingerprinting” the illicit sand crisis
GeoTalks Webinar | Dean Claudia Mora and Andrew West
Start:October 6, 2021 at 9:30 am
End:
October 6, 2021 at 10:00 am
Location:
Virtual: https://utexas.zoom.us/j/91904554193
Contact:
Courtney Vletas, cvletas@jsg.utexas.edu
EPS Undergraduate Research Fair
Start:October 6, 2021 at 5:00 pm
End:
October 6, 2021 at 7:00 pm
Location:
JGB 3.222 or Zoom
Undergraduate research in EPS is of critical importance for both the education and research missions. Because momentum has been stymied by the COVID pandemic, faculty and researchers want to kick-start undergraduate involvement in research for the next academic year.
The event starts at 5 pm and will be hybrid – meaning presentations by faculty and researchers will be in person in JGB room 3.222 or via Zoom at this link: https://utexas.zoom.us/j/92686072555
The Research Fair will be followed by an in-person an socially-distanced pizza social on the JBG patio starting at 6 pm to offer a more informal way for undergraduates to ask questions or connect with faculty and researchers that are present. Please RSVP here if you will be attending the pizza social.
UT Paleontology Seminar
Start:October 7, 2021 at 11:00 am
End:
October 7, 2021 at 12:00 pm
Location:
JGB 4.102
Contact:
David Trevino Ledesma, ledesma-david@utexas.edu
Inferring Reptilian Ecology in
Mitchell Riegler
University of Florida
Zoom Link: https://utexas.zoom.us/j/
Graduate Studies Committee (GSC) Meeting
Start:October 7, 2021 at 12:30 pm
End:
October 7, 2021 at 2:00 pm
This is an internal Jackson School of Geosciences meeting for faculty and research scientists who are part of the Graduate Studies Committee.
DeFord Lecture | Marisa Palucis
Start:October 7, 2021 at 4:00 pm
End:
October 7, 2021 at 5:00 pm
Location:
https://utexas.zoom.us/j/96370762511
Contact:
John Lassiter
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Geomorphic response to climate change in the Arctic: Implications for early Mars
Dr. Marisa Palucis, Dartmouth University
Abstract:
Alluvial fans may represent one of the last widespread signs of significant fluvial activity on Mars’ surface. Understanding the climatic conditions during the formation of these features may provide key insights on habitability and climate change on Mars.
Numerous studies have used data and theory from terrestrial fans from warm, arid, rainfall-dominated climates to estimate flow discharges, runoff rates, and total water volumes that likely built Martian fans. However, it has been suggested that Martian fans sourced water only from snowmelt, and perhaps under periglacial conditions. Thus, there is a knowledge gap about the dominant processes building fans under periglacial conditions, and importantly for Mars, a lack of understanding about the characteristic flow magnitudes during depositional events.
In this talk I will present results from a field-based terrestrial analog study involving characterization of the sedimentology and geomorphology of a periglacial alluvial fan in the Richardson Mountains, Northwest Territories, Canada. I will (1) qualitatively describe the range of sedimentary processes occurring on a periglacial alluvial fan and compare them to prior observations, (2) report measured flow discharges and runoff rates that occurred during a summer storm event, and (3) show that melt rates suggested for Mars are capable of entraining and transporting appreciable amounts of sediment by fluvial processes.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
BEG Seminar: Michael Young - Bureau of Economic Geology
Start:October 8, 2021 at 9:00 am
End:
October 8, 2021 at 10:00 am
Location:
Zoom or PRC, BEG Bldg. 130, Main Conference Room 1.202
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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Regional Land Impacts in Texas from Energy Development
Understanding landscape impacts from the development of fossil and renewable energy sources is essential to land use decisions and management. This presentation focuses on current and potential future landscape alteration stemming from oil and gas, wind and solar installations, including recent observations and estimates of land needed in west Texas over the next ~30 years to accommodate estimates of new facilities. The field site focuses on the Permian Basin of West Texas, an area of significant interest for energy production. The research findings will be placed into the context of the broader discussions of the energy transition, in Texas and elsewhere, and how new and ongoing research at the Bureau will help to understand and quantify the broader life-cycle impacts of a broader mix of energy systems.
Send anonymous feedback on Bureau presentations to: speakerfeedback@beg.utexas.edu
UT participants may login at utexas.zoom.us with UT-EID/password
Join Zoom Meeting
https://utexas.zoom.us/j/92792561070?pwd=ZitUMmVYT0FnWHFBTk1GUGFVb09iQT09
Meeting ID: 927 9256 1070
Passcode: 745476
UTIG Seminar Series: Heather Ford, Queen Mary University of London, UK
Start:October 8, 2021 at 10:30 am
End:
October 8, 2021 at 11:30 am
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Heather Ford, Queen’s University in London, UK
Host: Chris Lowery
Title: The mid-Pleistocene Enigma: detangling regional and global signals in seawater ð18O records
Abstract: High-resolution seawater ð18O records, derived from coupled Mg/Ca and benthic foraminifera ð18O analyses, can be used to evaluate how global ice volume changed during the mid-Pleistocene transition (MPT, ca. 1250–600 ka). However, such seawater ð18O records are also influenced by regional hydrographic signals (i.e., salinity) and changes in deep-ocean circulation across the MPT, making it difficult to isolate the timing and magnitude of the global ice volume change. To explore regional and global patterns in seawater ð18O records, we reconstruct seawater ð18O from coupled Mg/Ca and ð18O analyses of Uvigerina spp. at Ocean Drilling Program Site 1208 in the North Pacific Ocean. Comparison of individual seawater ð18O records suggests that deep-ocean circulation reorganized and the formation properties (i.e., salinity) of deep-ocean water masses changed at ca. 900 ka, likely related to the transition to marine-based ice sheets in Antarctica. We also find that an increase in ice volume likely accompanied the shift in glacial-interglacial periodicity observed in benthic carbonate ð18O across the MPT, with increases in ice volume observed during Marine Isotope Stages 22 and 16.
Friends and Alumni Networking Event at GSA Connects 2021
Start:October 11, 2021 at 5:00 pm
End:
October 11, 2021 at 7:00 pm
Location:
Hyatt Regency Portland at the Oregon Convention Center 375 NE Holladay
Contact:
Courtney Vletas, cvletas@jsg.utexas.edu, 512-621-6120
UTIG Seminar Series: Ian Hamling, GNS Science, New Zealand
Start:October 14, 2021 at 2:30 pm
End:
October 14, 2021 at 3:30 pm
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Ian Hamling, GNS Science, New Zealand
Host: Xiaohua Xu
Title: Our shifting planet: Utilising satellite observations for measuring the deformation of the Earth’s surface
Abstract: The surface of our planet is constantly deforming and changing shape in response to the build-up and release of tectonic strain before and after an earthquake or the movement of magma in the crust. In the past, measuring this deformation was time consuming, expensive and in the case of volcanoes, often required the observer to venture into difficult or dangerous regions to make measurements. However, the development of a technique known as Interferometric Synthetic Aperture Radar (InSAR) has revolutionized the way we measure the deformation of the Earth’s surface.
From the triggering of volcanic eruptions and zombie volcanoes to nationwide estimates of the interseimic deformation and Vertical Land Movements (VLM), this talk will cover a range of InSAR observations from across the SW-Pacific and explore how we can utilise these vast datasets to improve our understanding of volcanic and tectonic processes.
DeFord Lecture | Claire Masteller
Start:October 14, 2021 at 4:00 pm
End:
October 14, 2021 at 5:00 pm
Contact:
John Lassiter
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How rivers remember: the effects of flow history on sediment mobility in gravel-bed rivers
Dr. Claire Masteller, Washington University
Abstract: Rivers transmit environmental signals across landscapes. In the wake of a changing climate, predicting river channel response to variations in flow magnitude and flood frequency is of significant importance for floodplain communities and ecosystems. As these environmental perturbations propagate across a drainage basin, it’s important to consider the role of prior flow history in a channel when predicting its future evolution. However, widely used models for fluvial sediment transport currently do not integrate these history effects. This omission represents a fundamental, outstanding knowledge gap in earth surface processes.
In this talk I will focus on the process of bedload sediment transport in gravel-bed rivers, where memory effects are observed over a variety of time-scales. I will first discuss the origins of memory in gravel bed rivers, using results from a series of laboratory flume experiments. I will then apply these new insights to a unique, continuous record of coarse sediment transport to quantify the thresholds for memory formation and destruction in a steep mountain stream. I will discuss the development and implementation of a history-dependent function to better describe sediment mobility by accounting for these memory effects.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
BEG Seminar: Jerry Jensen - Bureau of Economic Geology
Start:October 15, 2021 at 9:00 am
End:
October 15, 2021 at 10:00 am
Location:
Zoom or PRC, BEG Bldg. 130, Main Conference Room 1.202
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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Estimating vertical permeability in the Ormskirk Sandstone, East Irish Sea Basin
Engineers love permeability. After all, permeability is simple in concept, a major control on production and economics, and it is easy to measure. What’s not to love about permeability?
Alas, in truth, permeability is a difficult and mercurial rock property: 1) it is extremely variable, typically varying by four to six orders of magnitude in a reservoir; 2) permeability is scale-dependent, changing with sample size; and 3) permeability is direction dependent, changing by a factor of 10 or 100 when the flow direction changes. What a monster! Fortunately, there are a few ways to tame the beast, including 1) taking many samples, 2) measuring permeability in multiple ways; and 3) relating the permeability to the reservoir geological features.
This talk will demonstrate all these taming ways in a case study. We show that 1) integrating probe permeameter, core plug, and wireline tester measurements with the geology leads to a coherent picture of vertical permeability for the Ormskirk Sandstone; 2) without the geological information, we needed twice as many samples to obtain the same level of uncertainty of the estimated vertical permeability; and 3) permeability assessment within a geological framework reduces the upscaled vertical permeability variation from more than three orders of magnitude to less than one order of magnitude.
Send anonymous feedback on Bureau presentations to: speakerfeedback@beg.utexas.edu
Join Zoom Meeting
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Passcode: 485295
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In-Person at PRC, BEG Bldg. 130, Main Conference Room 1.202
Water, Climate and Environment Seminar | Caleb E. Adams - LANL
Start:October 15, 2021 at 12:00 pm
End:
October 15, 2021 at 1:00 pm
Location:
Online
Contact:
Cansu Demir, cdemir@utexas.edu
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A Plant Physiology-based Live Fuel Moisture Model for Use in Fire Behavior Models
Habitability Seminar: Charity Phillips-Lander, SWRI
Start:October 18, 2021 at 1:00 pm
End:
October 18, 2021 at 2:00 pm
Location:
Zoom Meeting
Contact:
David Goldstein, david@oden.utexas.edu
A seminar from the Center for Planetary Systems Habitability
Title: The Value of Building a Texas Astrobiology Community
Speaker: Charity Phillips-Lander, Senior Research Scientist, Astrobiology, Space Science and Engineering Division, Southwest Research Institute
UTIG Discussion Hour: Antoniette Grima, UTIG
Start:October 19, 2021 at 2:00 pm
End:
October 19, 2021 at 3:00 pm
Location:
Zoom Meeting
Contact:
Naoma McCall, nmccall@utexas.edu
Speaker: Antoniette Grima, Postdoctoral Fellow, UTIG
Title: Deep slab dynamics and surface evolution
Lithosphere and Dynamic Earth seminar: Elizabeth Catlos
Start:October 20, 2021 at 12:00 pm
End:
October 20, 2021 at 1:00 pm
DeFord Lecture | Nandita Basu
Start:October 21, 2021 at 4:00 pm
End:
October 21, 2021 at 5:00 pm
Location:
https://utexas.zoom.us/j/96370762511
Contact:
John Lassiter
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Water Quality Challenges and Opportunities from the Local to the Global Scale
Dr. Nandita Basu, University of Waterloo
Abstract: Declining water quality is a growing global issue. As the human population increases, a multitude of factors, from intensive agricultural practices and widespread over-application of commercial fertilizers, to climate change and wildfires threatening our drinking water supplies, to emerging contaminants from rapid urbanization and concentrated livestock operations, threaten our water resources.
Multiple new policies have been developed to improve water quality in our lakes and streams; however, water quality remains a persistent problem. In this talk, Nandita Basu will address the nature of water quality challenges, especially focusing on long term legacies of nutrients, and discuss opportunities for addressing some of these challenges through a combination of top-down analysis — using large geospatial datasets to identify watershed functional traits — and mechanistic modeling, from the reach to the watershed scale. Through this discussion, she will highlight novel approaches for regional- and global-scale solutions to water quality challenges.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
BEG Seminar: Peter D. Warwick - USGS
Start:October 22, 2021 at 9:00 am
End:
October 22, 2021 at 10:00 am
Location:
Zoom
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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Coal Geology and Resources of the U.S. Gulf of Mexico Coastal Plain
The primary coal-bearing strata of the U.S. Gulf of Mexico Coastal Plain occur in Upper Cretaceous, Paleocene, and Eocene coastal, deltaic, and fluvial sediments deposited along the north-northwestern margin of the Gulf of Mexico Basin. Coal ranks in this area range from lignite to bituminous. Most of the coal currently mined in Texas is lignite from the upper part of the Wilcox Group (Paleocene to Eocene), whereas in Louisiana and Mississippi, lignite is mined from the lower part of the Wilcox Group. Other Gulf of Mexico Coastal Plain coal-mining areas in south Texas and northern Mexico have produced bituminous coal from the Upper Cretaceous Olmos Formation and Eocene Claiborne Group, and lignite from the Eocene Jackson Group. Coal beds within the Gulf of Mexico Coastal Plain generally are less than 15 ft thick and most coal mines produce from several beds. All coal-bearing strata dip regionally into the Gulf of Mexico Basin unless disturbed by local faulting or folding.
The U.S. Geological Survey (USGS) has assessed recoverable coal and coalbed gas resources of the Gulf of Mexico Coastal Plain. Detailed assessments of coal quality and coal resources were focused on parts of the Wilcox Group in (1) northeast Texas, (2) central Texas, and the Sabine uplift in (3) Louisiana and (4) Texas. Estimates of coal in these areas total 97 billion short tons with less than 500 ft of overburden, or 175 billion short tons with less than 2000 ft of overburden (Warwick and others 2011, American Association of Petroleum Geologists Studies in Geology No. 62). The USGS assessment of coalbed gas resources of the Gulf of Mexico Coastal Plain estimated a mean of 4.06 trillion cubic feet of undiscovered, technically recoverable, continuous gas resources primarily from the Wilcox Group coals (Warwick and others 2007, https://pubs.usgs.gov/fs/2007/3039/).
Join Zoom Meeting
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Meeting ID: 958 5597 6870
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UTIG Seminar Series: Michael Pyrcz, UT Cockrell School of Engineering
Start:October 22, 2021 at 11:30 am
End:
October 22, 2021 at 12:30 pm
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Host: Gail Christeson
Water, Climate and Environment Seminar | Matthew Bartos - UT CAEE
Start:October 22, 2021 at 12:00 pm
End:
October 22, 2021 at 1:00 pm
Location:
Online
Contact:
Cansu Demir, cdemir@utexas.edu
View Event
TBD
UTIG Discussion Hour: John Christian, UTIG
Start:October 26, 2021 at 2:00 pm
End:
October 26, 2021 at 3:00 pm
Location:
Zoom Meeting
Contact:
Naoma McCall, nmccall@utexas.edu
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Speaker: John Christian, Postdoctoral Fellow, UTIG
Title: Disentangling the roles of natural variability and anthropogenic forcing in driving rapid outlet glacier
Lithosphere and Dynamic Earth seminar: Student Talks
Start:October 27, 2021 at 12:00 pm
End:
October 27, 2021 at 1:00 pm
Aaron Satkoski, Sarah Brooker, Hoss Hostettler
DeFord Lecture | Xiaowei Chen
Start:October 28, 2021 at 4:00 pm
End:
October 28, 2021 at 5:00 pm
Location:
https://utexas.zoom.us/j/96370762511
Contact:
John Lassiter
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Multi-scale analyses reveals diverse triggering processes during induced earthquake sequences
Dr. Xiaowei Chen, University of Oklahoma
Abstract: In the past decade, Oklahoma experienced a large-scale earthquake experiment with significant variations of seismicity rates that are strongly correlated with injection rates from wastewater disposal. In response to the increased seismicity rate, the seismic network has been significantly expanded, providing a rich dataset to better understand the earthquake triggering processes during fluid injection. The original view of induced seismicity was simple and straightforward – increase pore pressure reduces effective normal stress, promoting fault failure. However, observations in Oklahoma suggests that triggering processes of induced earthquake sequences can be very complex, and are strongly influenced by fault structure and stress state.
In this presentation, I start with large-scale observation of seismicity migration and stress/fault distributions. Multi-scale analysis of seismicity migration allows us to derive hydraulic properties for the Arbuckle group and the crystalline basement. These parameters contributed to large-scale modeling that suggested the importance of poroelastic stress from fluid injection. With detailed analysis of the stress state of seismogenic faults, we find that fault stress state could strongly influence temporal evolution of earthquake sequences. Then, I discuss diverse triggering processes observed during several individual sequences. The Woodward sequence in western Oklahoma suggests that earthquake-to-earthquake triggering drives the fault activation. The Guthrie sequence in central Oklahoma occurred within a complex fault mesh network, and showed evidence of aseismic slip along a normal fault. These detailed observations provide a reference framework for future earthquake rupture simulations within different fault systems, and insights into the triggering processes during fluid-driven natural earthquake sequences.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
UTIG Seminar Series: Rick Colwell, Oregon State University
Start:October 29, 2021 at 10:30 am
End:
October 29, 2021 at 11:30 am
Location:
Seminar Conference Room - Pickle Research Campus, Bldg 196-ROC 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Rick Colwell, Oregon State University
Host: Kehua You
Title: Deep Life: What’s Up Down There?
Water, Climate and Environment Seminar | Daniel O. Breecker - JSG
Start:October 29, 2021 at 12:00 pm
End:
October 29, 2021 at 1:00 pm
Location:
Online
Contact:
Cansu Demir, cdemir@utexas.edu
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Automated monitoring of soil CO2 and O2 concentrations
SSL Seminar Series | Tian DongJanuary, 20 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Natural and Human Impacts on Coastal Land Building by Dr. Tian Dong Abstract: Sediment and water delivered by rivers build and sustain coastal landforms such as deltas and wetlands, which are densely populated and ecologically vital areas threatened by rising sea levels. In this talk, I highlight theory-driven and field-based research to understand how coastal land building operates across broad deltaic plains and how human activity affects these processes. On the theoretical front, inspired by Hack’s law (the scaling between watershed drainage area and channel length in tributary networks), we analyzed a global dataset of distributary delta networks and discovered a nearly identical scaling relationship between distributary channel length and nourishment area, the land-building counterpart to drainage area. Despite this apparent global scaling, we identified two distinct local land-building patterns: Uniform Delta Networks consistently follow Hack’s law, while Composite Delta Networks exhibit a scale break, transitioning from space-filling growth around the delta apex to quasi-linear growth near the coast. These surprising growth patterns suggest that global simplicity and local variability coexist in how river deltas grow and organize. To assess regional variability and human impacts, we combined remote sensing with field observations from the Lower Rio Grande, finding that the river currently carries about one-third of its median 1900s discharge, and only about 0.3% of its natural flow reaches the Gulf due to human consumption. This reduction leads to channel contraction, higher water levels for the same discharge, and significant shoreline retreat (up to 6 m/yr). I conclude by highlighting three ongoing/future research directions on deltaic land building: (i) sedimentation influenced by human engineering, (ii) wind-driven sediment redistribution, and (iii) the effects of sediment influx from retreating glaciers. |
DeFord Lecture | Venkat LakshmiJanuary, 22 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 Progresses and Challenges in Hydrology by Dr. Venkat Lakshmi, professor at the University of Virginia Abstract: In order to study land surface hydrology, we need to use a multitude of tools, namely, modeling, observations and their synergism. After multiple decades of hydrological modeling, we still have major challenges. However, we have novel observations and mathematical methods that are now available and can be harnessed to achieve progress. These include earth observations that are available at global scales and at high spatial resolutions and frequent temporal repeat. Artificial Intelligence and Machine Learning (AI/ML) can be used (specifically Transfer Learning) to determine streamflow in un-gaged or poorly-gaged watersheds. In this talk, I will focus on four major questions and provide examples for each of the questions. These examples will highlight both advances and limitations for each issue. (i) Do earth observations compare well with in-situ counterparts? (ii) How important is rainfall in hydrological modeling? (iii) Can we get higher spatial resolution of earth observations? (iv) How do we study un-gaged/poorly gaged watersheds? |
Bureau of Economic Geology Seminar SeriesJanuary, 23 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented by Dr. Bridget Scanlon, BEG in person. Topic: Remote sensing, hydrology |
SSL Seminar Series | Kristin BergmannJanuary, 27 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Temperature and the earliest animals: Quantitative climate reconstruction across the Neoproterozoic–Phanerozoic transition by Dr. Kristin Bergmann Abstract: The Neoproterozoic–Phanerozoic transition records the emergence of complex animals, the origin of biomineralization, and the establishment of modern marine ecosystems—yet the climate context for these evolutionary milestones remains poorly quantified. Reconstructing ancient temperatures requires integrating sedimentology, carbonate petrography, and isotope geochemistry. Our field-based stratigraphic analysis establishes depositional context and identifies the most promising sampling targets; detailed petrographic screening and microstructural analyses constrain diagenetic paragenesis. Clumped-isotope thermometry (Δ47–Δ48) reconstructs temperature signals within this sedimentological framework, resolving the ambiguity between temperature and seawater composition that limits traditional δ¹⁸O approaches. This rocks-first workflow reveals large, directional climate shifts with ecological consequences. In the Tonian and Cryogenian, data from Oman and elsewhere indicate near-modern tropical temperatures before and after Snowball Earth glaciations, suggesting dynamic hydrologic and climatic transitions. During the Ediacaran, post-glacial warming followed by ≥20 °C cooling likely expanded oxygenated habitats and set the stage for early animal diversification. In the Ordovician, ~15 °C of long-term tropical cooling over ~40 Myr culminated in brief but extensive glaciation, providing the climate context for the Great Ordovician Biodiversification Event. By grounding geochemical data in sedimentological and petrographic observations, we build a quantitative framework linking climate and habitability and provide evidence that temperature change guided life\'s evolutionary trajectory in deep time. |
SSL Seminar Series | Ted PresentJanuary, 29 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Biogeochemical Signals of Seafloor Oxygenation by Dr. Ted Present Abstract: Earth’s oxygenation transformed the atmosphere, oceans, and ultimately the seafloor, establishing the carbon and sulfur cycles that govern our planet today. When and how did oxygen penetrate into marine sediments, shifting where organic matter was recycled and setting up the biogeochemical architecture we recognize in modern oceans? I approach this question by studying how microbial and chemical processes at the sediment-water interface leave lasting signatures in sedimentary rocks. Using sulfur isotopes and detailed sedimentology, I will show how Paleozoic carbonates and evaporites track the reorganization of ocean redox structure through critical evolutionary transitions like the Late Ordovician glaciation and mass extinction. The Permian Reef Complex of West Texas demonstrates how cementation and dolomitization patterns archive ancient sulfur cycling, with insights grounded in observations from modern tidal systems where diagenetic processes govern carbon storage along our changing coasts. I will close with how I envision training UT Austin students in integrated field and laboratory approaches to pursue future research leveraging evaporite basins, novel phosphatic archives, and terrestrial carbonates. By extracting environmental signals from the diagenetic processes that create the rock record, this work builds a framework for understanding how Earth’s oxygenation reshaped life and its environment. |
Bureau of Economic Geology Seminar SeriesJanuary, 30 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented in person by Dr. Todd Halihan, Oklahoma State University, and Chief Technical Officer for Aestus, LLC in person Topic: Subsurface hydrogeology |
SSL Seminar Series | Mackenzie DayFebruary, 03 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) From sand to stratigraphy: How dunes record the changing landscape of Earth and other planets by Dr. Mackenzie Day Abstract: Desert dune fields preserve rich sedimentary records of environmental change, providing insight into both past climate and modern landscape evolution. This presentation explores three desert systems on Earth and Mars, using dune fields as a lens to examine how landscapes, both ancient and modern, respond to shifting environmental conditions. These investigations address the longevity of Earth’s dune fields, the interplay between wind and water, and the applicability of aeolian sedimentology to planetary bodies beyond Earth. Together, they highlight how dune fields serve as dynamic archives of change, and how Earth, Mars, and other bodies can be studied in tandem as natural laboratories for generalizing aeolian sediment transport to arbitrary fluid-gravity conditions. |
SSL Seminar Series | Marjorie CantineFebruary, 05 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Human, climate, sediment and geobiological history of a rapidly-growing carbonate island by Dr. Marjorie Cantine Abstract: You may have heard the line that real estate is valuable because \"they aren\'t making more land\"; in this talk, I\'ll show you that that\'s not true. I\'ll use the sedimentary and radiocarbon records of a carbonate island in the Caribbean, Little Ambergris Cay, to describe its formation over the last millenium, how its growth relates to past climate, and what it means for mechanisms potentially capable of protecting shorelines in the near future. I\'ll leverage geobiological field experiments to help explain the mechanisms of island growth. Finally, I\'ll share how ongoing work in my group is leveraging geoarchaeological archives to better understand the human and climate histories of the Common Era and inform hazard predictions in the region through testing climate models. I will also briefly describe other work ongoing in my group, which tackles questions at the nexus of time, sedimentary processes, and geochemistry from the Precambrian to the Common Era. |
15th Annual Jackson School of Geosciences Student Research SymposiumFebruary, 06 2026Time: 12:00 AM - 12:00 AM |
Bureau of Economic Geology Seminar SeriesFebruary, 06 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented by Stacy Timmons and Mike Timmons, New Mexico Bureau of Geology & Mineral Resources, in person. Topic: New Mexico Geological Survey |
SSL Seminar Series | Vamsi GantiFebruary, 10 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) From Dunes to Channel Belts: How Rivers Organize and Move Across Scales by Dr. Vamsi Ganti Abstract: Rivers are Earth’s arteries: they transport water and sediment from uplands to oceans, sustain ecosystems and agriculture, and build the stratigraphic record of past environmental change. Yet rivers are far from static—they are dynamic systems that evolve across scales, from ripples and dunes on the riverbed to entire channel belts. In this seminar, I will present three discoveries that reveal the mechanisms shaping alluvial river form and motion across these scales. (1) Laboratory experiments and theory identify a previously unrecognized transition in river-dune organization at the onset of significant suspended sediment transport. This transition influences flow roughness, flood-driven dune reconfiguration, and the nature of preserved fluvial strata. (2) Using a new image-processing tool, we analyzed 36 years of satellite imagery from 84 rivers to uncover the origins of single- versus multithread channels. Single-thread rivers achieve a balance between lateral erosion and accretion, maintaining equilibrium width, while multithread rivers arise when erosion outpaces accretion, causing individual threads to widen and split. This mechanistic insight informs both planetary geomorphology and cost-effective river restoration. (3) Finally, I’ll show how human activity and climate change are already altering the way rivers flow and evolve. Dams dampen river motion and reduce the number of active threads, whereas increased sediment supply from land-use change and glacial melt are making rivers in the Global South and High Mountain Asia more dynamic. Together, these discoveries provide a mechanistic view of river evolution across scales and highlight why understanding river behavior is essential—not only for managing water, life, and landscapes they sustain today, but also for decoding the history of environmental change recorded in sedimentary strata. |
DeFord Lecture | Jake JordanFebruary, 12 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 |
DeFord Lecture | Daniel MinisiniFebruary, 19 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 |
Bureau of Economic Geology Seminar SeriesFebruary, 20 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented by Dallas Dunlap, BEG, in person. Topic: Channel Architecture Influenced by Precursor Channelized Submarine Landslide Topography in the Taranaki Basin |
Hot Science - Cool Talks: The Biology of LoveFebruary, 20 2026Time: 5:30 PM - 8:30 PMLocation: Welch Hall 2.224 and Grand Hallway What does science say about love and long-term relationships? In this Hot Science – Cool Talks event, biologist Dr. Steven Phelps explores the biology of love through the surprising world of prairie voles, one of the few monogamous mammals. By studying how vole brains form lasting bonds, Dr. Phelps reveals what biology, brain chemistry, and evolution can teach us about human connection and commitment. This engaging talk offers a fresh, science-based look at why we pair up right after Valentines Day! |
