Expect delays due to road work on HWY 64/87 west of Capulin, between Capulin and Raton, NM.
Picnic Area Restrooms Closed
Restrooms at the picnic area are temporarily closed. The restrooms in the Visior Center and in the Volcano Rim parking lot are open. Sorry for the inconvenience.
History & Culture
While the geologic history of Capulin Volcano began well over a million years ago, its involvement in human history has been much more recent. Capulin has traditionally been a crossroads of human activity as diverse people and cultures traversed to and from the Great Plains.
Archaeological evidence found at the Folsom Man site, eight miles from Capulin Volcano, confirms that Paleoindians roamed this area in search of Pleistocene Bison as early as ten thousand years ago. Likewise, groups of Native Americans, such as the Jicarilla Apache and the Ute, used this region as hunting grounds until the arrival of the Spanish in 1541. Early explorers Don Francisco Vasquez de Coronado and Juan de Padilla passed through Capulin area in search of riches and regions to conquer paving the way for a greater influx of Europeans and a transformation of the cultural landscape over the next 350 years.
Spain controlled New Mexico until August 1821 when Mexico declared independence. Spanish
Struggling to feed soldiers and captives a Fort Sumner, the War Department issued advertisements offering to pay high prices for cattle. Two Texas cattle dealers, despite the risks, forged a trail from Texas to New Mexico which became known as the Goodnight-Loving Trail. Charles Goodnight and Oliver Loving drove cattle north through sparsely populated, lawless regions with very little water to Fort Sumner. The cattle not sold to the military continued north, directly past Capulin Volcano, to Colorado for sale at the market. The cattle industry grossed a million dollars over the next five years and created a profitable economy for Great Plains which remains to this day.
Did You Know?
Tumuli or squeezeups usually develop when lava flows on level ground. A mound of lava is pushed up from the flow when the crust buckles, with additional pressure from the liquid lava of the flow.