Chemical weathering is a fundamental Earth surface process that transforms primary rock minerals into secondary minerals and dissolved ions, thereby controlling the long‐term regulation of atmospheric ...

Magnesium isotope geochemistry has emerged as a pivotal tool in deciphering Earth’s surface and subsurface processes, particularly in the context of chemical weathering. By studying the subtle ...

Geophysical surveys reveal subsurface weathering indirectly. The arrival of seismic energy, generated by a sledge hammer and recorded by geophones, is used to calculate seismic velocities. Slower ...