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Access to Frijoles Canyon Will Be Limited
Starting June 1, 2012 all access to the most visited part of the park, Frijoles Canyon, will be via a shuttle bus from the nearby community of White Rock. This is to alleviate a parking shortage created by the Las Conchas Fire. More details to follow.
Bandelier Geology
Volcanic map of New Mexico "Our ancestors knew how to shape these volcanic rocks into arrowheads, axe heads, corn grinding tools, and homes." – Affiliated Pueblo Committee The geology of the Pajarito Plateau shaped the lives of the people who inhabited this landscape. The dramatic cliffs of Frijoles Canyon were created from the ash of massive volcanic eruptions.
photo by sally king Just a portion of the Valles Caldera can be seen from State Highway 4. Massive Eruptions
photo by sally king Consolidated volcanic ash forms a rock known as tuff. During the eruptions that formed the Valles Caldera, ash flows up to 1,000 feet thick covered the landscape from the caldera rim to the Rio Grande. As the hot ash cooled, it welded into a rock called tuff. Bandelier is located on this broad, sloping layer of tuff called the Pajarito Plateau.
photo by sally king Homes were made from the volcanic tuff. Tuff is very light and soft. Over time, wind and water gradually eroded away softer areas of tuff, creating holes in the exposed canyon faces. The Ancestral Pueblo people used these to their advantage. With hand tools, they enlarged and shaped cliff openings into useful shelters called cavates (CAVE-eights). They used tuff blocks to build apartment-like homes along the cliff faces in front of the cavates. |
Did You Know?
Pinon nuts are rich in vitamins, flavor, and calories (3,000 per pound). Although produced in abundance only every 7 to 10 years, these nuts were a valuable native food source for the Ancestral Pueblo people. More...