Attention GPS Users
To find the visitor center please use the coordinates provided in the 'Directions' link. Otherwise you will get lost driving in various neighborhoods that surround the monument. Do not go to Headquarters (6001 Unser Blvd.) it is not designed for visitors. More »
Trail Closures due to trail restoration project
Per Superintendent's Order: T36 CFR 1.5(f), Rinconada Canyon and other side trails are closed until further notice due to an extensive trail restoration project. Inquire at visitor center for open petroglyph viewing trails. Thank you.
Volcanos and Basalt
The rock that makes up the West Mesa escarpment is vesicular basalt. The basalt flow originated from fissures marked by five volcanic spatter cones that can be seen along the western horizon of Albuquerque. Located within the monument boundary, these cones are considered part of a sacred landscape by many Puebloan people today. The last volcanic eruption occurred approximately 150,000 years ago. Although the area is still geologically active, geologists consider these spatter cones to be extinct.
The basalt that makes up the boulders on which the petroglyphs are carved was originally a light gray color. Over time the surface of the rock was coated by a thin black or dark brown layer of oxidation scientists call "desert varnish." When the surface of the boulder is pecked or abraded, the lighter rock underneath is exposed, displaying a stunning light gray-on-black contrast.