Events
2026 - 2 Events
Resolving the Earth's Mantle Composition
EVENTS
Workshop on Resolving the Earth's Mantle Composition
December 3 – 4, 2026, New York, USA
Leading Deep-Earth Researchers to Convene at Columbia to Resolve the Composition of Earth's Mantle
NEW YORK — The MINERALS Project at Columbia University will host Resolving the Earth’s Mantle Composition, a two-day international workshop bringing together mineral physicists, seismologists, geodynamicists and geochemists to confront one of the most consequential open questions in the Earth sciences: what the planet’s mantle is actually made of.
The workshop takes place December 3–4, 2026 at Columbia University in New York, and is convened by Prof. Renata M. Wentzcovitch, Principal Investigator of the MINERALS Project and a professor at Columbia’s Department of Applied Physics and Applied Mathematics and Lamont-Doherty Earth Observatory.
The mantle accounts for the overwhelming majority of Earth’s volume, yet no sample of it has ever been recovered from depth. Everything known about its composition is inferred — from seismic waves that pass through it, from laboratory experiments that recreate its crushing pressures and temperatures, and, increasingly, from quantum-mechanical simulations that predict how minerals behave under conditions no experiment can yet reach. Each of these approaches produces a partial answer, and the answers do not always agree.
Resolving those disagreements has consequences well beyond the deep interior. Mantle composition governs how heat escapes from Earth’s core, how continents move, how volcanoes erupt, and how the planet has evolved chemically over 4.5 billion years. It also anchors our understanding of what makes a planet habitable — a question now being asked of worlds far beyond our own.
The workshop is designed to be small and deliberately interdisciplinary. Nineteen invited participants from institutions across North America, Europe, Asia and South America will present current work and spend structured time on the points where their fields diverge.
Invited participants
- Jamison Assunção — Universidade de São Paulo
- C. Alberto M. C. — Universidade de São Paulo
- Laura Cobden — Utrecht University
- Arwen Deuss — Utrecht University
- Edward Garnero — Arizona State University
- Damanveer Grewal — Yale University
- Kei Hirose — University of Tokyo
- Christine Houser — Earth-Life Science Institute, Institute of Science Tokyo
- Shun-ichiro Karato — Yale University
- Tomoo Katsura — University of Bayreuth
- Jun Korenaga — Yale University
- Jung-Fu (Afu) Lin — University of Texas at Austin
- Maureen Long — Yale University
- William F. McDonough — University of Maryland and Tohoku University
- Robert Myhill — University of Bristol
- Kaveh Pahlevan — Carl Sagan Center, SETI Institute
- Keith Putirka — California State University, Fresno
- Jessica Santos Rego — Universidade de São Paulo
- Paul Tackley — ETH Zürich
They will be joined by members of the MINERALS research team at Columbia and partner institutions.
The meeting is organized under the MINERALS Project — Modeling Earth from Atomic to Global Scale — a multi-institutional research effort led from Columbia and supported by the Gordon and Betty Moore Foundation. MINERALS works across an unusually wide range of scales, from the behavior of individual electrons in iron atoms to the convection of the whole mantle, and the workshop reflects that span.
Recent work by the MINERALS team illustrates the approach. The iron spin crossover — a quantum-scale rearrangement of electrons within iron atoms under extreme pressure — changes how seismic waves travel through the lower mantle, meaning a phenomenon measured in angstroms leaves a signature detectable from the surface of the planet. Connecting effects at those two scales is precisely the kind of problem the workshop exists to address.
The workshop is by invitation. Further details, the program, and participant abstracts will be posted here.
About the MINERALS Project
MINERALS — Modeling Earth from Atomic to Global Scale — is a collaborative research project led by Prof. Renata M. Wentzcovitch at Columbia University, spanning Columbia’s Department of Applied Physics and Applied Mathematics, Lamont-Doherty Earth Observatory, and partner institutions. The project develops and applies first-principles computational methods to determine the properties of Earth-forming minerals and to link them to global-scale geophysical observations. MINERALS is supported by the Gordon and Betty Moore Foundation.
Media Contact
Vishal Manve (Vishy) former Project Coordinator, The MINERALS Project Lamont-Doherty Earth Observatory, Columbia University vbm2109@columbia.edu
High-Pressure Mineral Physics and Geophysics Applications
EVENTS
Workshop on High-Pressure Mineral Physics and Geophysics Applications
February 2 – 7, 2026, São Paulo, Brazil
Multidisciplinary discussion between mineral physics, seismology, and geodynamics
Materials simulations bring powerful methods for predicting the physical properties of complex mineral phases, assemblages, and melts under the extreme conditions expected in Earth’s interior (~6,500 K and 3.6 Mbar). They play a central role in probing the deep Earth and have brought us to the threshold of developing a general predictive theory of planetary interiors grounded in their material properties.
This workshop advances this vision by bringing together a multidisciplinary team of scientists to discuss the integration between three core fields of computational geophysics: mineral physics, seismology, and geodynamics.
There is no registration fee. Register here.
Organizers:
- Renata MM Wentzcovitch (Columbia University, New York, USA)
- Carlos Alberto Moreno Chaves (IAG, USP, São Paulo, BR)
- Caetano Miranda (IF-USP, São Paulo, BR)
- John Hernlund (Earth-Life Science Institute, Tokyo-Tech, Tokyo, JP)
- Alexandre Reily Rocha (IFT/UNESP, ICTP/SAIFR, São Paulo, BR)

2025 - 2 Events
AGU Fall Meeting 2025 - New Orleans
EVENTS
AGU Fall Meeting 2025
December 13–19, 2025, New Orleans
Abstracts presented by the Wentzcovitch Group:
- DI31A-01 – Fe–Ni Phase Diagram: Mineral Physics Implications for a Layered Inner Core
- MR13A-04 – Thermoelasticity of Geologically Relevant Silica Phases (SiO₂) Using Machine Learning Potentials
- MR13A-08 – Ferroelastic Hysteresis, Shear Modulus Softening, and the Tetragonal↔Cubic Transition in Davemaoite
- MR31B-0044 – Phase Transitions, Stability, and Thermodynamic Properties of Mg₀.₅Fe₀.₅O Under Super-Earth Conditions
- MR31B-0048 – Machine Learning Potential for Serpentines
- MR31B-0049 – The Fe–Si–O System at Terapascal Pressures
G51C-0184 – Quantifying Uncertainty in Glacial Isostatic Adjustment through Community Model Intercomparison Project: GIAMIP
APS March Meeting 2025 - Global Physics Summit
EVENTS
APS March Meeting 2025 - Global Physics Summit
March 16–21, 2025, Anaheim
Abstracts presented by the Wentzcovitch Group:
- MAR-L49.4 – Effects of the pressure-induced H-bond disorder/symmetrization in δ-AlOOH on its phonon properties
- MAR-L49.1 – Deep learning-based simulations in geophysics
- MAR-W46.8 – Understanding the stability of superionic phases in Earth’s inner core
- MAR-W46.9 – Ferrous iron partitioning in the lower mantle: consequences for seismic velocities and heterogeneities
- MAR-W46.11 – Elastic softening in the tetragonal-cubic transition in davemaoite
- MAR-W46.12 – Machine learning potential for serpentines
2024 - 1 Event
AGU Fall Meeting 2024
EVENTS
AGU Fall Meeting 2024
December 9th - 13th, 2024 - Washington D.C.
Abstracts presented by the Wentzcovitch Group:
- MR22A-02 – Understanding the stability of superionic phases in Earth’s inner core (Invited)
- MR23B-03 – An ab initio study on the hydrous minerals: stability and elasticity of brucite
- MR21C-3217 – Deep-learning-based prediction of the tetragonal to cubic transition in davemaoite
- MR21C-3221 – H-bond disorder-symmetrization in δ-AlOOH under pressure: a view from phonon quasiparticles
- MR21C-3218 – Fe2+ partitioning in Al-free pyrolite: consequences for seismic velocities and heterogeneities
- DI11A-03 – Observational Evidence for Iron Spin Crossover and Chemical Heterogeneity in the Deep Mantle from both Body Waves and Whole Earth Oscillations (Invited)
Sessions co-organized by Renata Wentzcovitch
MR21C – Exploring Planetary Materials Through Computational Simulations and Data Analytics I Poster
MR23B – Exploring Planetary Materials Through Computational Simulations and Data Analytics II Oral
Primary Convener
- Jie Deng, Princeton University
Conveners
- Renata Wentzcovitch, Columbia University in the City of New York
- Jun Tsuchiya, Ehime University
- Bijaya B Karki, Louisiana State University
