Datil-Mogollon Section

The Datil-Mogollon Section is a volcanic landscape in southwestern New Mexico formed by massive eruptions that created steep cliffs and layered rock formations. The region displays extensive fields of hardened lava and ash deposits that shape the terrain across numerous mesas and ridges.

This volcanic region formed during an ancient period of intense magmatic activity that created massive calderas and eruption zones. The geological structures preserve evidence of major volcanic developments that shaped the southwestern landscape.

The geological formations of the Datil-Mogollon Section play a central role in New Mexico's scientific research and geological education programs.

Spring and autumn offer the best conditions for exploring, with moderate temperatures and clear visibility across the volcanic landscape. Sturdy footwear and plenty of water are essential since trails cross over rough volcanic rock and exposed terrain.

Mount Taylor, a prominent volcanic peak in the southeastern section, serves as a natural vantage point overlooking the surrounding lava-covered mesas. Its location makes it the tallest and most visible volcanic feature in this landscape.