The surface of the Earth is the ever-changing expression of the dynamic processes
occurring at depth and at or above its surface. However, our ability to “read” landscapes in …

Earth's mantle undergoes convection on million‐year timescales as heat is transferred from
depth to the surface. While this flow has long been linked to the large‐scale horizontal forces …

Earth's surface topography is a direct physical expression of our planet's dynamics. Most is
isostatic, controlled by thickness and density variations within the crust and lithosphere, but …

Earth's large-scale topography and lower-mantle structure are linked to past tectonic
motions and mantle flow, making it possible to gain insights in the properties of the solid …

In this paper, we report on a two-scale approach for efficient matrix-free finite element
simulations. It is an extended version of our previous conference publication [1]. The …

The slow creeping motion of Earth's mantle drives transient changes in surface topography
across a variety of spatial and temporal scales. Recent decades have seen substantial …

Mantle convection shapes Earth's surface by generating dynamic topography. Observational
constraints and regional convection models suggest that surface topography could be …

The origin of the high topography within the western United States has been attributed to
either crustal/lithospheric isostasy or dynamic topography, but their relative contributions …

We investigate the relationship between the global distribution of deep slab dips (at 250‐to
300‐km depth) and pressure and circulation in the upper mantle. Using an analytic method …

Due to the Mesozoic multi-plate convergence, prominent continental marginal tectonic belts
were formed in East Asia. The significant intra-continental magmatic events in the interior of …