Variety Spices Travel
In Flagstaff the giant cell towers that look like straight, tall Douglas fir trees, blend right in to the environment. They don't look a bit out of place. Andy said there was a move to put one in Newtown that was drawing a lot of protest. It wouldn't fit naturally there like it does here.Chunks of limestone mark the site of ancient homes in Walnut Canyon. |
Recent findings suggest increased rainfall with more water in the canyon, new water-conserving farming practices, trade and a general population increase in the Southwest may have prompted the development of community canyon living between 1125 and 1250 A.D.
The Ancestral Puebloans who lived here were Sinagua, Spanish for "without water." They called their new home talatupqa, meaning "long canyon." The 20-mile length and 400-foot depth contains mini plant life zones spanning the West from Mexico to Canada. At the top is the Upper Sonoran desert with yucca and prickly pear cactus; at the bottom is riparian riverbank community with boxelder and Arizona black walnut, for which the canyon was named.
Only the few larger rooms represent living quarters. Most areas have been identified as storage bins. |
The cliff dwellings of Walnut Canyon were occupied for little more than 100 years. By 1250, the occupants had moved southeast along Anderson Mesa and were eventually assimilated into Hopi culture. Their cliff dwellings, sealed shut when the people left on what the Hopi believe was a religious quest to have all clans come together, remained undisturbed until the late 1800's.
Lennox Crater Trail ends in a field of cinder pieces where very little can grow. |
In the canyon, the ancient homes usually faced south and east to take advantage of warmth and sunlight. Archaeologists suggest it was the women who built the homes, fashioned from shallow caves eroded out of the limestone cliffs by wind and water. The limestone rock walls were cemented with a gold-colored clay, found in another part of the canyon. Wooden beams reinforced doorways. Walls were plastered with clay inside and out. Men farmed small pockets on the semi-arid canyon rim. They hunted small game and gathered more than 20 species of plants. This life in the canyon probably evolved after departing the rimtop area closer to Sunset Crater.
Lennox Crater Trail at Sunset Crater took us straight up the side of a cinder cone along a path of loose, crumbled cinders for 300 feet in elevation to more than 7,000 feet. Andy said, "It sure feels like more than 300 feet up."
On the south face of Sunset Crater little can grow in the rough, nutrient-poor cinders. |
Sunset Crater is a 1000-foot volcanic cone with two lava flows. Erupting sometime between 1040 and 1100 for as long as a year, Sunset Crater is the most recent in a six-million-year history of volcanic activity near Flagstaff. Natural forces that created Sunset Crater also created more than 600 volcanic features in the area, including the San Francisco Peaks, which in turn have affected climate and habitat for all living things in this region.
Sunset Crater started when molten rock sprayed high in the air from a crack in the ground, solidified and fell back to earth as large bombs and smaller cinders. Periodic eruptions with debris around the vent created a 1000-foot cone. The lightest, smallest particles dusted 800-square miles of northern Arizona with ash. Closer to the base, two lava flows--the Kana-a and the Bonito--destroyed all living things in their paths. New gas vents produced spatter cones, and cooling lava pushed through cracks for squeeze-ups. A final burst of activity after six months or a year gave the cone its name. The colorful glow when red and yellow oxidized cinders shot from the vent reminded people of a sunset.
From Desert View Overlook, we can see the Colorado River far below. |
Flowers bloom everywhere in late September. |
We headed to the South Rim of the Grand Canyon at 1:15 p.m. with the intent of just driving from viewpoint to viewpoint.
Desert View near the East Entrance Station was crammed with foreign tourists. Maybe they were trying to catch the main attractions before the government shuts down on Monday or maybe they were oblivious.
From Lipan Point we could see layers of sedimentary rock that are millions of years old. |
At No Name Point #1 the views of the river are hidden by steep rock layers. |
Moran Point is bathed in color in the late afternoon. |
Low growing gamble oaks lined the edge at No Name Point #2. |
It took three complete circles around the multiple parking lots at Grandview Point just to find a place to park. We descended a short distance down and climbed back up for better camera angles. "When we were here before in the winter," said Andy, "this trail was solid ice. We only went down a couple switchbacks because it was so dangerous."
Ponderosa pine trees cling to the sides of the canyon at No Name Point #5. |
The river valley opens up at Grandview Point Overlook. |
Comfortably far from the edge, we blend in with the scenery. |
No Name #3 Viewpoint along Desert View Drive showed the Horseshoe Mountains in the far distance.
Bright sun warms No Name Point #4 in the afternoon as the river valley gathers shadows. |
Four o'clock shadows darkened the inner canyon after Yaki Point. Andy played with angles, and I adjusted camera settings to get good pictures. With images of the glorious vistas of the grandest Grand Canyon on earth, we headed back to Flagstaff. At 8,046 feet, as we drove through the divide on Route #180, it was 57 degrees and getting colder.
No comments:
Post a Comment