Brittle deformation and Mohr-Coulomb failure Deformation of Earth materials takes place predominantly within two rheological
Category: Interpreting ancient environments
Sandbox analogue models of strike-slip basins and pop-up structures How things have changed. It wasn’t
This post deals with the materials, their rheological behaviours, and scaling as they apply to
The correct scaling of geometric, dynamic, and kinematic system variables is a critical part of
The posts in this series focus on Earth science models, particularly the soft-rock kind. I
Analogue models are physical objects; we can touch them and observe represented systems directly. As
The primacy of beds, bedding, and bedding planes Beds are the fundamental units of stratigraphy
This is the fourth post in a series on vegetated coastal lithofacies – see also:
This post is part of the Lithofacies Series. Mangrove trees and forests occupy a very
This post is part of the Lithofacies Series. Manukau Harbour on the west edge