Showing posts with label Colorado Plateau. Show all posts
Showing posts with label Colorado Plateau. Show all posts

Monday, September 7, 2009

Grand Circle - Torrey, Utah

Day 10-12

On our way to Torrey, Utah, we stopped at the Anasazi Indian Village where 87 rooms were uncovered. Anasazi is a Navajo word meaning “Ancient Ones” and is used to describe the basketmaker-Pueblo culture that existed in the Four Corners area from AD 1 to 1,300. The people who lived here disappeared suddenly around AD 1200. All that remains are their writings and dwellings.


The drive was just as before, spectacular!





























What a beautiful view from our campground in Torrey, Utah.
While in Torrey, we visited the Capitol Reef National Park. The park contains about a quarter of a million acres of towering cliffs and eroded landscape, known to the early Native Americans as “Land of the Sleeping Rainbow.” A giant, wrinkle in the Earth’s crust stretches for 100 miles across south-central Utah. This impressive buckling of rock, created 65 million years ago by the same tremendous forces that later uplifted the Colorado Plateau, is called the Waterpocket Fold. This waterpocket fold country is the free-flowing Fremont River and the big desert sky.




















We hiked through Capitol Gorge to see the “tanks,” which is basically a hole in the rock where water would pocket in heavy rains or snow runoff. It was so interesting to see the petroglyphs and the pioneer register (writings of pioneers on the rocks dated as far back as the 1800s).






















We stopped at the Gifford house, where we met a woman who was born & raised on the other side of the gorge that we hiked. It was so interesting to talk to her and her the stories of her childhood and the stories from her mother and grandmother. When the Giffords lived at the house, they had one girl and 2 or three boys. The parents and daughter slept in the 2 bedrooms in the house and the boys slept upstairs. To get upstairs, they had to go outside, around back, up a ladder and through the window.
Calvin Pendleton (who may be of the Pendleton wool family) arrived in Fruita in the 19th century and built a barn before World War I. He sold the land to Jorgenson in 1919 and the barn was changed over the years. The last owner, G. Dewey Gifford used the barn for over 40 years and rolled loose, cut hay from a wagon into the barn using an “A” rope with team or tractor.















We then visited the Fruita one room school house which was opened in 1896. Eight grades were taught in one room with 8 to 26 students. In the early years class was only held in the winter months so that the children could help with the farming during the spring, summer and fall. The building also served as Sunday School, a meeting place and Saturday night social center. The school closed in 1941 due to declining enrollment.













Then it was off to the orchard to pick apples, pears and peaches. The orchards were started by the mormons but is now run by the government. It’s pick your own on the honor system.
On our way home, we stopped at an overlook. Here on the Colorado Plateau has the best visibility in the lower 48 states. At the Capitol Reef National Park, the average summer visual range is 145 miles!!!



















The following day, it was on to Gobblin Valley, Utah. The drive was so different. The colors went from the rich red and white sandstone hoodoos to grey and black hills. We felt like we were in the middle of a mining operation.








































Along the way, we stopped at the Wolverton Mill which was built by Edwin Thatcher Wolverton, who came from Maine to look for gold. He built a mill to crush gold ore in 1921 didn’t discover very much gold. In 2003, a wildfire raged through the area of Straight Creek, where the Wolverton Mill originally stood, so it was relocated by the government to its present location in Richfield, Utah.
We finally reached the road we had to turn off to the state park where we were to camp for the night in Gobblin Valley State Park. All I could say was OMG! It was about 15 miles from the main road, on dirt, pavement, dirt and pavement.










We parked away from the group, due to lack of campsites, which was fine for use since we were all dry camping, we were able to run our generator 24 hours a day. We had a great view! As we were parking our rv, an antelope ran by us in the field.










Before 10 p.m. (generator turn off time at the campground) we were joined by 2 other rigs who wanted air conditioning since the evening was a little muggy.

We had a ranger led gobblin, urchin walk at 7:30 that evening. It was great! The ranger explained how the area was on the edge of a shallow inland sea. Tidal deposits of sand, silt and clay sediments were left. Over millions of years, these distinct layers hardened to become the sandstone, siltstone and shale layers of these formations. 145 to 170 million years ago, during the middle to latter part of the Jurassic Period these environments dominated the landscape.





























As we walked through, they looked like goblins and the full moon, which made it really cool.

Saturday, September 5, 2009

Grand Circle - Bryce Canyon

Day 7-9

On the way to Bryce, we drove through Red Rock.










Bryce Canyon was my favorite when we vacationed with our son, Robby in 2001. I think because of the rich colors and the odd shaped “hoodoos,” a natural column of rock.

The rock progresses from “fins” to developing “windows” that later collapse to form hoodoos., In ancient times, they thought that men turned to stone and had powers. It was fun to see the different shapes of hoodoos as we traveled through the park. We found Queen Elizabeth,
chicken,















lion and Trojan horse,

King Tutt















Bill discovered ET on our hike
Approximately 200 million years ago, the earth’s crust was crinkling throughout Nevada and into southern Canada. A strong, dense Pacific seafloor had smashed into North America’s weaker continental crust. Over 120 million years, compressional forces bent, folded, broke, and heaved our crust into the sky, giving birth to the Sevier Mountains. Rain and snow became geologic jackhammers, splitting mountains apart.

Just before dinosaurs went extinct (65 million years ago), the oceanic plate pushed up our continental crust uplifting land, forming the Rocky Mountains and warping Utah and Arizona. The rivers wore down the Sevier Mountains reaching the basin between the Sevier and Rockies, depositing layers of muds and silts., Lakes and ponds formed, but with no rivers flowing out of the basin, the sediment was trapped. Between 55-30 million years ago this mammouthb mud puddle, known as the Claron Basin, continued to fill with sediments rich in calcium carbonate – dissolved limestone (pink and white). Over time, these beds of sediment were compressed into rock and uplifted from 3,000 ft. to 9,000 feet in elevation 15 million years ago, forming the Colorado Plateau. About 8 million years ago, the Bryce Canyon area broke off this uplift as the Paunsaugunt Plateau and has been sinking ever since into the Great Basin. The freezing and thawing of water does most of the sculpting at Bryce Canyon, as opposed to a flowing river. In the photo below, the land as far as you can see use to be at the same level we were standing taking the picture. It is now 1,000 feet higher.















We went on an evening ranger walk on the rim of the canyon and learned that the canyon erodes between 1-4 feet per 100 years. They estimate that in 6 million years, Bryce Canyon will not exist. (he’ll be retired by then) Notice the difference in color as the sun went down.






























We took a 4 hour bus tour through the Canyon overlooks and had a wonderful bus driver/guide.


He told us if you sniffed the Ponderosa Pine Tree you are apt to smell vanilla, due to a fungus.















Of course everyone took a whiff. At the Agua Canyon Overlook, we were greeted by Vinny and Minnie Moocher who posed for pictures.

That evening, we took a group to see the sun set at Bryce Overlook. It is amazing how the rock formation colors become more enriched. I did not believe it could get more beautiful than when the sun is highlighting the canyon, but it does.



















On our free day, Marcia, Bill and I took a hike through the canyon, starting at Sunset Point and ending at Sunrise Point (yes we went backwards because it was easier to descent the steepest part of the hike. It was so beautiful that you can’t even imagine how different it looks from the bottom of the canyon as opposed to the rim. Around each turn everything looked different. It took us twice as long to do the hike because we had to keep stopping to take pictures and to just enjoy the scenery.

The start of our hike - Bill and Marcia on their way










Can you believe we found these trees in the middle of the rock!

We found quite a few arches that we could walk through and as we hiked, we found stones marking paths, like the indians used to do.






























This was the horse path!!!!!!

Done at last!!!!!
We finished our day with a dinner buffet at the Ruby Inn Lodge – dejavue – it was the same place Bill, Robby, and I stayed when we visited in 2001!