|
Location:
The Bandelier National Monument is located northwest of Santa Fe, New Mexico and south of Los Alamos, New Mexico. The park entrance to the monument can be accessed on SH 4 about 8 miles west of White Rock, New Mexico.
From Los Alamos, New Mexico, drive west on SH 501 (W Jemez road) about five miles to SH 4 then turn left. Drive east on SH 4 for almost 6 miles to the entrance to the national monument.
Entrance Coordinates:
35.796024, -106.275089
Entrance Elevation:
6662 feet
Geographical Region
When the
desert wayfarer culture, who most likely were part of the
second migration, transitioned from hunter-gatherers to a more settled lifestyle, one characterized by dependence on agriculture, social stratification, population clusters and major architecture, they began what is called in the writings of this web site the
post-wayfarer cultures (750 CE -1550 CE).
These Anasazi found this canyon perfect for there settlement. The tuff cliffs were easy to carve into and form rooms, there were areas where they could excavate rooms high above the canyon floor and thus provide a safe escape from any enemy that may have attacked them.
When the home was complete, when the crops were all in, when their bellies were full, and when they had enough animal skins to keep them warm, methinks, these people took the time to work on their latest rock art, or, what we call today, petroglyph. Here at Bandelier, the petroglyph are found carved into the tuff cliffs that line the valley, the same cliffs where the people excavated their homes. There are even some pictograph in the ruins.
The Ancestral Pueblo people in New Mexico, known on this website as the
Anasazi lived here from approximately 1150 CE to 1550 CE. They built homes carved from the volcanic tuff and planted crops in mesatop fields and washes.
Corn, beans, and squash were central to their diet, supplemented by native plants and meat from deer, rabbit, and squirrel. Dogs assisted in hunting and provided companionship. Domesticated turkeys were used for both their feathers and meat.
Colorado Plateau
On October 09, 2009, I begin what is the first day of nearly two weeks visiting the ruins of the ancient stone stackers and it is during these two weeks that so much knowledge about these people and their culture has come into my ken.
Too, this entire two weeks are spent living in the jammer and overnighting in the campgrounds and or nearby towns. So, by living, cooking and eating outdoors, I am able to experience the environment that they may have experienced.
Still, I have been wondering about the origins of the cliffs that all of these ancient people chose to build their homes in. Today, the temperature was quite warm here in the canyon but during my tour of the ruins, I noticed when I climbed into the caves carved out of the cliffs, it was amazingly cool in the back. What a perfect place to get out of the other than perfect weather outside.
How did all of these choice living opportunities come about?
What cause these Cliffs?
I am not yet sure about other areas, but here at Bandelier ruins, about a million years ago, the Jemez volcano just fifteen miles west of here had two massive volcanic eruptions and covered this area with flows of volcanic ash, many hundreds of feet deep, which later compacted into what is now known as tuff. In some places, the tuff was over a thousand feet deep.
Depending on how quickly it cooled, tuff varies from very hard to very crumbly. Over thousand of years, the frost, rain, streams and wind cut deep canyons into the tuff plateau creating the canyon and mesa terrain shown in the photo above.
Finally, the same elements began to carved holes into the side of the canyon walls of the tuff.
Valles Caldera National Preserve (35.851700, -106.455201)
Jemez Hot Springs (35.771628, -106.690476)
Jemez Ruins (35.777915, -106.687809)
|