Fold/uplift.

Rocky Mountains.

Primary formation (the Laramide orogeny) occurred roughly 80–55 million years ago.

Michael Gäbler · CC BY 3.0 · Image source ↗

A landscape with a history.

Formed through a broad, unusually far-inland compressional event, likely caused by a shallow-angle subduction of an oceanic plate beneath western North America, transmitting stress much further inland than typical subduction-driven mountain-building. This makes the Rockies geologically distinct from more "textbook" subduction ranges like the Andes.

What makes it remarkable

Spans a huge portion of western North America, from New Mexico to British Columbia, with significant regional variation in rock type and age along its length.

Another skyline. Another story.