Part of the Alberta Front Ranges fold -thrust belt north of Highwood Pass. Sawtooth-like Lower Paleozoic carbonates are exposed as flatirons in the hanging wall of a thrust immediately east of Lewis Thrust. Late Jurassic – Early Cretaceous foredeep deposits in the valley floor (mostly covered) were involved in the deformation as the orogenic load migrated eastward. Orogenic transport to the right.
Glossary, Groundwater - geofluids, How to do things, Interpreting ancient environments

Geofluids: Lithosphere-scale fluid flow

Fluid flow at lithospheric scales There’s not much that goes on in sedimentary basins that doesn’t involve fluids, particularly the […]