Time, written on the skyline

14 ranges.
14 histories.

Explore how moving plates, faulting, volcanism, and erosion shaped these real landscapes.

Himalayas landscape
Fold mountains

Himalayas

Began forming approximately 50 million years ago; still actively rising today.

Andes landscape
Fold/volcanic, subduction-driven

Andes

Formation began roughly 200 million years ago, with the modern range's major uplift occurring within the last 25 million years.

Rocky Mountains landscape
Fold/uplift

Rocky Mountains

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

Appalachian Mountains landscape
Fold mountains (ancient)

Appalachian Mountains

Began forming approximately 480 million years ago.

Alps landscape
Fold mountains

Alps

Began forming approximately 65 million years ago; still tectonically active.

Sierra Nevada landscape
Fault-block mountains

Sierra Nevada

Uplift primarily over the last 5–10 million years (though the underlying rock, largely granite, is much older).

Cascades landscape
Volcanic mountains, subduction-driven

Cascades

The current volcanic arc has been active for roughly the last 5–7 million years, though volcanism in the region extends further back.

Black Hills landscape
Dome mountains

Black Hills

Uplift occurred roughly 65–70 million years ago.

Ural Mountains landscape
Fold mountains (ancient)

Ural Mountains

Began forming approximately 300–250 million years ago.

Karakoram landscape
Fold mountains (part of the same India–Asia collision system as the Himalayas)

Karakoram

Began forming alongside the Himalayas, roughly 50 million years ago.

Caucasus Mountains landscape
Fold mountains

Caucasus Mountains

Began forming roughly 28–23 million years ago.

Zagros Mountains landscape
Fold mountains

Zagros Mountains

Began forming roughly 25–20 million years ago, with major uplift continuing into the last 5 million years.

Scandinavian Mountains landscape
Fold mountains (ancient)

Scandinavian Mountains

Began forming roughly 500–400 million years ago.

Southern Alps landscape
A mix of fault-block and fold processes, driven by an unusual, largely transform-but-oblique plate boundary

Southern Alps

Uplift primarily within the last 5–10 million years, and ongoing.