The Prehistoric Trackways National Monument site includes a major deposit of Paleozoic Era fossilized footprints in fossil mega-trackways of land animals, sea creatures, and insects. These are known as trace fossils or ichnofossils. There are also fossilized plants and petrified wood present, as well as plenty of marine invertebrate fossils including brachiopods, gastropods, cephalopods, bivalves, and echinoderms. Much of the fossilized material originated during the Permian Period and is around 280 million years old. track Some of the animals who may have left tracks in the Robledo Mountains include Dimetrodon, Eryops, Edaphosaurus'', and multiple other pelycosaurs. There are at least 13 major trace fossils found at the monument, including Selenichnites or moon-shaped trace, Kouphichnium or light trace, Palmichnium or palm trace, Octopodichnus or eight-footed trace, Lithographus or rock writing, Tonanoxichnus or Tonganoxie trace, Augerinoichnus or Augerino trace, Undichna or wave-shaped trace, Serpentichnus or snake-like trace, Batrachichnus or frog trace, Dromopus or running foot, and Dimetropus or Dimetrodon foot. The trackways can be difficult for the general public to find, as the monument is largely undeveloped with few facilities yet existing to aid fossil hunters. Many of the slabs pulled out by Jerry MacDonald are housed at the New Mexico Museum of Natural History and Science, although they are not on display at this time. Guided hikes are periodically offered by BLM interpretive staff.
Geology
The monument lies along the western portion of the Rio Grande rift and is within part of the Robledo Mountains. It is made up of Cenozoic and Paleozoic sediments. The Hueco Group is Early Permian strata. Most of the monument is Permian and would have been underwater or along the coast of what was once the Hueco Seaway. The tracks can be found in the red rock which is called the abo red beds.
On average the coolest month in the monument is January with an average high of, the hottest month is June with an average high temperature of, and the wettest month is August with about of precipitation.
Discovery
In situ Paleozoic Era tracks were discovered on June 6, 1987 by Jerry Paul MacDonald. Scattered footprints had been found in the Robledos for almost fifty years prior to MacDonald starting his search. He used the recollections of local hikers, quarrymen, and fossil hunters to concentrate his search. This initial site was named the "Discovery Site". It is one of the best places in the monument for visitors to see fossilized tracks. Jerry MacDonald excavated three long trackways, carrying over 2500 slabs out from the site on his back. The majority of the slabs are housed in the New Mexico Museum of Natural History and Science in the Jerry MacDonald Paleozoic Trackways Collection. Two other continuous trackways are held in the Carnegie Museum of Natural History and Smithsonian.
The Bureau of Land Management is in the process of writing a resource management plan for the monument to be completed in 2012. In the meantime, there are no developed hiking or equestrian trails, and only one interpretive sign. Roads are not maintained and there are no facilities. There are OHV and mountain bike trails, which are rugged and require appropriate skills and equipment.