01The Landforms, Located

The Rio Grande rift has produced a remarkable variety of landforms across a span of perhaps 400 kilometres, each the direct product of crustal extension, volcanism, or the erosion that follows both. What follows is every landform treated in this guide, placed on the ground.

Layered mountain ridges fade into haze beyond a forested, grassy hillside

Albuquerque Basin

35.15°N, 106.65°W

The central structural depression of the rift in New Mexico — a graben bounded by fault-block ranges east and west, filled with kilometres of its own eroded debris.

Sandia Mountains

35.13°N, 106.45°W, summit Sandia Crest

A tilted fault block rising abruptly east of its escarpment, exposing Precambrian granite below Pennsylvanian limestone along a single dramatic face.

Manzano Mountains

34.63°N, 106.40°W, summit Manzano Peak

The same fault-block structure continuing south, structurally continuous with the Sandias and equally legible in cross-section.

Ladron Peak

34.40°N, 107.05°W

An isolated uplifted block standing well into the basin, exposing very old metamorphic and igneous rock far from any range front.

Jemez Mountains

35.87°N, 106.57°W

A large volcanic field on the rift's western margin, built over more than ten million years and punctuated by two caldera-forming eruptions in the Pleistocene.

Valles Caldera

35.87°N, 106.52°W

The 22-kilometre resurgent caldera produced by the Toledo and Valles eruptions, the structural heart of the Jemez volcanic field.

Cerros del Rio

35.83°N, 106.22°W

A basalt plateau north of the basin, dissected by the Rio Grande into a gorge that exposes individual flow sequences.

West Mesa and its escarpment

35.10°N, 106.75°W

A basalt-capped mesa whose eroded eastern edge provides the boulder field at Petroglyph National Monument.

Kasha-Katuwe Tent Rocks

35.67°N, 106.40°W

Hoodoos of pumice-rich tuff eroded from Bandelier Tuff deposits, each cone preserved by a harder caprock fragment.

Socorro magma body

34.06°N, 106.89°W

Not a surface landform but the active crustal structure beneath Socorro; geodetic measurements confirm ongoing inflation detectable at the surface.

The New Mexico Bureau of Geology and Mineral Resources publishes maps locating all of these features within the broader geological framework of the rift.

An adult geologist with a hand lens crouched at a rock outcrop, notebook on the ground
Plate 04Most of what is known about the fill under the valley was established at outcrops like this.