A recent paper in the Journal of Open Source Software describes the implementation details of Underworld3 and a brief motivation for the rewritten codebase (Moresi et al, 2025). Underworld3 combines the power of the symbolic algebra package, sympy (Meurer et al, 2017), with the equation templating system in the parallel finite-element framework of PETSc, through petsc4py (Knepley et al, 2013, Dalcin et al, 2011). Underworld3 has the same

Coupling in Underworld 2 Underworld 2's UWGeodynamic module enables the coupling of tectonics and surface processes models, most notably, with Underworld 2 handling the tectonics and Badlands (Salles, Ding, & Brocard, 2018) handling the surface processes.

Parallel computation puts many CPUs to work on solving a problem much more quickly than one CPU alone. But this only works if the tasks are carefully scheduled and the additional CPUs are not waiting around for something to do. How do we choose the right number of processors for a given problem ?

You are invited to a full-day workshop on Underworld — a computational Geodynamics / Tectonics modelling framework. This is an excellent opportunity for researchers, students, and professionals interested in computational geodynamics and Earth science modelling to learn about Underworld.

TL; DR: Underworld is now Singularity-enabled, making it easier and somewhat quicker to use compared to traditional HPC installs. We demonstrate results using over 10,000 CPUs and more than one billion unknowns for solving the Stokes equation with Underworld 2.16

Introducing Underworld3: Mathematically Self-Describing Modelling in Python for Desktop, HPC and Cloud.

CITCOM is a geodynamics modelling code based on the finite element method that is designed for planetary evolution modelling where large spatial variations and strong non-linearities occur in the material properties.

Introduction and benchmarking The convection of the Earth’s mantle is usually modelled as an incompressible process, referred to as the Boussinesq approximation. However, in the Earth’s mantle, the pressure increase associated with depth also increases the density due to self-compression (King et al. 2010). In some applications, this compressibility may be non-negligible and modelling it may be desirable.

Abstract Numerical models have become an indispensable tool for understanding and predicting the flow of ice sheets and glaciers. Here we present the full-Stokes software package Underworld to the glaciological community. The code is already well established in simulating complex geodynamic systems. Advantages for glaciology are that it provides a full-Stokes solution for elastic–viscous–plastic materials and includes mechanical anisotropy.

Yeah, one repo, one vision! In an effort to simplify maintenance and compatibility between Underworld and UWGeodynamics, we have decided to merge the codes into a single repository. Starting with version 2.13, UWGeodynamics will now live under Underworld. All UWGeodynamics functionalities and workflows will remain available to the users.

The Underworld Community has been supporting usage of Docker containers for developing and running Underworld powered scientific models.