Sunday, September 20, 2015

St. George KOA Campground - Hurricane, UT – Sept 14-19, 2015

Monday, September 14—my, where does time go? Early last week a wildfire started directly across the road from our campground. These are photos of the fire over 2 days.

We decided to spend a couple of days exploring Bryce Canyon and surrounding areas. We packed an overnight bag and lunch for 2 days, and headed out.

On the way we stopped at the Kolob Canyons section of Zion National Park, which is located in the NW section of the park, accessible from Interstate Highway I-15. This is definitely one to put on your bucket list. The views of this 5-mile drive are stunning, with vistas of crimson red canyons that take your breath away. The narrow parallel box canyons cut into the Colorado Plateau, forming 2,000’ cliffs and soaring peaks of Navajo sandstone with cascading falls and streams. (For the avid hiker there is over 20 miles of hiking trails for you!)

The Kolob Canyon area was first settled by Mormon farmers in 1851 that used the area for timber and grazing cattle, sheep and horses. They also prospected for mineral deposits. The Mormons named this place Kolob, from Mormon scripture, which means “the heavenly place, nearest the residence of God.”

It was difficult to select photos, so enjoy these ‘til you have an opportunity to visit Kolob Canyon for yourselves!



Our next stop was the Cedar Breaks National Monument off State Route 14. This area is a form of badlands, with canyons, spires (known as hoo-doos), walls and cliffs so steep that its only value is aesthetic. Early settlers called this area badlands or “breaks” and their misnaming the junipers in this area as cedars ultimately gave it its name: Cedar Breaks.

Cedar Breaks is a natural amphitheater, stretching 3 miles across, with a depth of over 2,000 feet. The rim of the amphitheater is over 10,000 feet above sea level! Although similar to Bryce Canyon, the rock here is more eroded than at Bryce. And, because of its elevation, the road through the park is often inaccessible from October through May. Cedar Breaks was established in 1933, with a small lodge that was deemed uneconomical to operate by the park service; protests regarding its demolition caused the park service to reexamine its policies and thus contributing to its preservation and eventual expansion to what it is today.

Erosion is taking its toll on the canyon: about 2” every 5 years. The brilliant colors that draw us are created by the iron (reds, oranges and yellows) and manganese (shades of purple) in various combinations.

Wildlife thrives at this altitude, and includes mule deer, porcupines, marmots, red squirrels, golden-mantled ground squirrels, pocket gophers and chipmunks, as well as mountain lions and elk (these are seldom seen). And, the ravens are HUGE! We saw only squirrels. We would love to see this area in the spring when wildflowers are in full bloom. The growing season is quite short, but apparently Colorado Columbine, Scarlet Paintbrush, Subalpine Larkspur, Shooting Stars, Orange Sneezeweed, Silvery Lupine, Yellow Evening Primrose, Plantainleaf Buttercups and other varieties cover the canyon in vivid color.





That evening we spent the night in Parowan, which is Southern Utah’s first settlement, founded in 1851. The main economic resource is tourism, as it serves as a year-round gateway to Brian Head Resort for skiing, and Cedar Breaks National Monument.

Artifacts, including petroglyphs, arrowheads, pottery and pit houses dating from A.D.750 to 1250, have been found in this area, and are evidence that Parowan was on a major thoroughfare of early Native Americans, most probably Fremont and Anasazi Indians. In addition, the Old Spanish Trail also passed through this area.

Parowan has been called the “Mother Town of the Southwest” because of the many Mormon pioneers who left from there to start other communities in southern Utah, Nevada, Arizona, Colorado, Oregon and Wyoming.

We stayed at the Victorian Rose Inn Monday night, a quaint inn built in 1904 as a single family home. It subsequently became a boarding house or hotel, and then apartments. More recently it was purchased and converted into a Victorian Inn, with 5 apartment-like rooms complete with kitchens. Our “apartment” had 15’ ceilings, a sitting room, full bath, small kitchen and bedroom. Very comfortable. And…their WiFi was screaming!

Dinner that evening was at La Nueva Villa Mexican restaurant across the street. Being a “dry” town, no alcohol was available so no Margaritas, but the food was excellent! We chowed down enchiladas, tacos and tostados—and tons of chips and salsa!

Breakfast Tuesday morning was at Parowan Café—food was good but the wait time for it was extremely looooooong. We ordered almost immediately, but weren’t served for almost 45 minutes. Good thing we like coffee! Ha!




After breakfast we headed to Bryce Canyon. But to get to Bryce we had to drive through Red Canyon.

Red Canyon, it is said, is the inspiration for the term “red rock.” Its formations of colorful limestone formations made for a photographer’s dream, as you’ll see in the photos below. Sparse vegetation dots the steep slopes and cliffs of this beautiful area; the rich green ponderosa pines add a beautiful contrast to the deep red of the canyon. Seven plant species grow here that are found together nowhere else in the world. Pretty cool. These plants have adapted to the severe environmental conditions here that tend to exclude other common species, and are called edaphic, meaning that they are influenced more by the soil than the climate.




Although Bryce Canyon is called a canyon, it’s actually a collection of giant natural amphitheaters. As we saw at Cedar Breaks, Bryce is distinctive due to the “hoodoos” found throughout the park. Bryce sits at a much higher altitude than Zion, with the rim varying from 8,000 to 9,000 feet, and all the vistas are visible from these altitudes. We noticed the pressure a bit, and found breathing to be a bit labored, especially at Bryce Overlook where we trekked up and down a few paved paths (all for the purpose of capturing—or trying to capture its beauty on camera).

Bryce Canyon was settled by Mormon pioneers in the 1850s, and was named after Ebenezer Bryce, who homesteaded in the area in 1874. The LDS church sent Bryce and his wife Mary to settle land in this area because they thought his carpentry skills would be useful to other pioneers settling in the area. They chose to live right below Bryce Canyon Amphitheater, grazing their cattle inside what are now park borders. He is reputedly to have said that the amphitheaters were a “helluva place to lose a cow.” He also built a road to the plateau to retrieve firewood and timber, and a canal to irrigate his crops and water his animals. Other settlers soon started to call this unusual place “Bryce’s Canyon,” which was later formalized into Bryce Canyon. 

Covering an area of almost 36,000 acres (or 55.992 square miles), the area around Bryce Canyon became a National Monument in 1923 by President Warren G. Harding, and designated as a National Park in 1928. The current Bryce Canyon Lodge was built in 1924-25 of local materials.

Archaeological surveys of the canyon show that people have been in the area for at least 10,000 years; basket-maker Anasazi artifacts several thousand years old have been found south of the park and artifacts from the Pueblo-period Anasazi and Freemont cultures have also been found.

The Paiute Indians, who moved into this area after the other cultures left, developed a mythology surrounding the hoodoos in Bryce Canyon. They believed the hoodoos were the Legend People whom the “trickster Coyote” turned to stone. At least one older Paiute said his culture called the hoodoos “anka-ku-was-a-wits,” which is Paiute for “red painted faces.”

The Rim Road, which is still in use today and is the scenic drive atop the plateau we drove, was completed in 1934 by the Civilian Conservation Corps. The National Park Service implemented a voluntary summer-only, in-park shuttle service in June 2000, transporting visitors to each of the scenic overlooks in the park.

For you who are interested, the brown, pink and red colors in the park are from iron oxide; the yellows from limonite; and the purples from manganese dioxide. The hoodoos are composed of soft sedimentary rock, topped by a piece of harder, less easily eroded stone. Bryce Canyon has one of the highest concentrations of hoodoos of any place on earth.

Due to the elevation, there are 3 distinct life zones in the park: dwarf forests dominate the lower areas, ponderosa pine forests cover the mid-elevations, and Douglas fir and white fir make up the forests on the plateau. It was interesting to learn that the harshest areas of the park have limber pine and ancient Great basin bristlecone pine thriving, some more than 1,600 years old.

The most common large animals found in the park are the mule deer—we didn’t see any. Elk and pronghorn deer are also sometimes seen. However, the forests and meadows of Bryce Canyon support diverse animal life, from birds and small mammals to foxes and occasional bobcats, cougars and black bears. In addition, 3 wildlife species currently as endangered species take up residence in the park: the Utah prairie dog, the California condor, and the southwestern willow flycatcher. There are about 170 species of birds in the park, as well as 11 species of reptiles, and 4 species of amphibians.

Unfortunately, while we were in the park, we were hit with strong gusty winds, rain and cold temperatures (48°); we didn’t plan our wardrobe very well, as we had donned shorts and t-shirts that morning. Thankfully, we did have sweatshirts and fleece with us, which helped—a little. Even still, Dick was able to capture some amazing photos of Bryce. Enjoy.



We decided to drive the Rim Road all the way to the end, to Rainbow Point and work our way back to the park entrance. The following photos are in order from that point, with the exception of Ponderosa Canyon--it was too foggy to see anything!











As we left the Canyons, we turned south to take state route 14 across to Highway I-15. As we drove, we came upon acres of lava beds, which apparently represent the last of the extensive volcanism in the area. Geologists believe that some of this lava rock is not more than 2,000 years old, and that it didn’t come from a central volcano, but rather it welled up from cracks and fissures in the earth’s surface. We passed Navajo Lake which was formed when lava flowed across the eastern end of the valley where it’s located. Lava tubes run under the lake and drain water into both the Great Basin and Colorado River drainages as the headwaters of the Virgin River (which subsequently flows through Zion National Park).
We returned to our camper about 5:00 p.m. It sure was a lot warmer there than at Bryce! We stopped at the office to collect mail/packages/etc., and to my surprise my husband did not forget it was my birthday! He handed me an Amazon box containing a dozen long-stemmed red roses with a dozen Asian lilies! And, now that they’ve all opened, the fragrance is fabulous and permeates the entire camper! Thanks, Honey! I love you!
Well that was Tuesday.
Wednesday we stayed close to home. Temps hit 86°, which felt really good after days of near 3-digit temps, and then a day of half that!
Thursday, after I did laundry (a woman’s work is never done!), we drove a few short miles to the nearby Silver Reef Museum.
The mining town of Silver Reef really flourished between 1876 and 1890. Sadly, now it’s a ghost town with nothing left but crumbling rock walls and foundations set against a spectacular background of red sandstone cliffs. Of the original structures, only the 1878 Wells, Fargo & Co.’s Express building remains intact and houses the museum. An item of interest: Silver Reef is the only place in North America where silver has been found in mineable quantities in sandstone. In the 14 years that the town was at its zenith, over 7 million ounces of silver were taken out of the areas 33 mines.
The museum was interesting too, in that many of that era’s artifacts, documents and photographs are on display. These include:
·        The original Wells Fargo vault where the silver bullion was held and protected until it could be loaded on a stage coach or wagon and hauled 75 miles to the rail head in Milford, UT;
·        Bottles, buttons, guns, shoe lasts, Chinese gambling games, carpentry tools, hat pins, and myriad other items;
·        At its peak, the town had almost 2,000 residents  from 18 countries and 29 U.S. states (interesting that there were no Mormons); photographs and documents depict the daily life in this early frontier mining town;
·        Geologic samples and information from the mines and the surrounding area;
Adjacent to the museum is the restored Cassidy Powder House, which was originally used to store dynamite for the nearby mines. It now houses a diorama of the main part of the old town. We took the interpretive walking trail to get a better idea of what the town was like. The town included the Cosmopolitan Restaurant which was reputed to serve the best hash in the territory. The Harrison House was considered to be Silver Reef’s Waldorf Astoria with 45 rooms and a 5-star restaurant. There was a printing office, and a variety of main-street shops. The Elkhorn Saloon which was the site of many gun fights, one of which involved the owner; the saloon also served as a courtroom. The Cassidy Powder House, Catholic church, the Rice Bank, mines, schoolhouse (which has been moved to nearby Leeds and still serves as the Town Hall), and the Nichols/Lubbock home (the most beautifully built, surrounded by trees and gardens) were all the landmarks still visible.
Silver Reef Museum is located in the Wells Fargo and Company Express Building, built in 1877.

The Cosmopolitan Restaurant burned but was totally rebuilt and now is the venue for special events. The Elk Horn
Saloon is no more, but the sign says it all! Many businesses lined the streets; the bottom 2 photos are ruins of
those businesses and the Harrison House Hotel.

The ruins of the printing house are still visible; the Cassidy Powder House was rebui.lt and now houses
a complete diorama of the town and an audio of the town's history

The mine shaft and various other buildings are still visible. A sign for the old school is adjacent
to the stone walls that surrounded it. A memorial to St. John's catholic Church stands adjacent to the
Rice Bank building.
Friday was travel day to Cornville, Arizona for a 1-week stay at Page Springs RV Resort. It was an easy but long day, 320 miles. It did involve driving up and down mountains (the highest elevation was 8,700’), through high deserts and canyons, which were beautiful. Along the drive we saw wild horses, wild turkeys, chipmunks, an Airstream caravan (14 of them!), beautiful Navajo jewelry at Vermillion Cliffs rest area, and giant boulders at Cliff Dwellers, AZ. (Oh, and before we left Utah, we saw a giant squished tarantula at our site!)
Gaining an hour, we arrived to our next park at 5:00 p.m. Still daylight, still warm. Our site is adjacent to a stream running through the park. The only down side was Dick backed into a neighbor’s pickup, just barely making a mark, as he was attempting to back our camper into our site. Oh, the hazards of backing up into a narrow spot, from a not-so-good angle. The park has 46 sites, and is part of the Sunrise Resorts family. Most of the campers are here for the weekend only, as there’s a big motorcycle rally in nearby Cottonwood.

Dinner was nachos here at home. We were so tired…
Saturday dawned with 66° and sunshine. We drove back into Cottonwood to run some errands and visit the visitor center. Dick hit the Home Depot and I walked to the visitor center. Wouldn’t you know, it was closed on weekends of all things. Dang!  I did meet Jade and Thomas from New York City, who were also at the visitor center and disappointed they were closed. We struck up a conversation; they were very interested in our full-time RVing and everything that went into preparing for this life. We talked for almost 20 minutes. Very cool. Hope they stay in touch, as they sounded like they were ready to hit the road!
Back at the ranch, we spent the afternoon watching football (The Ohio State University 20: Northern Illinois University 13. (Woot-woot!)
That’s it for this week. Stay tuned for more exciting adventures in next week’s blog as we share our day trip to Red Rock State Park, Sedona and other places in the area. Until then,
Hugs ‘n’ love,
RJ and Gail




No comments:

Post a Comment