Sunday, July 13, 2008
On the way home, the Roths, Denver
Was fortunate to be able to spend some time in Denver, on the way home, with my nephew, John Roth, his wonderful wife, Susan and their lovely daughters, Sierra and Alexus. Enjoyed every minute.
Good looking set of mugs; (left to right) Susan, Sierra, Alexus and John. Having dinner on the deck (beautiful evening).
Saturday got to see both girls in softball action. Here, through the fence (best I could do), Sierra shows her batting stance; getting ready to hit a home run.
Sierra, sprinting home after her home run, amidst the cheers of her teammates (the Mets) and their parents.
Wednesday, July 9, 2008
The Best of the Rest
Other parks/sites we saw in beautiful Utah. Why don't they just name the entire southern half of Utah as a national park?
Red Canyon. Just prior to getting into Bryce Canyon. Near our campsite, beautiful red sandstone formations.
One of two passageways through the red rocks.

Me, in a slot canyon along Burr road in Escalante.
Interesting shot of cottonwood tree w/varnished (looks like it was painted) red sandstone in the background.
Red Canyon. Just prior to getting into Bryce Canyon. Near our campsite, beautiful red sandstone formations.
Escalante National Monument (Grand Staircase). 1.9 million acres to the east of Bryce. Designed to be enjoyed by hikers and atvs/jeeps. Most of the roads to the interior are unpaved. Recently designated (1996). I called an outfitter to see if there were atv/jeep tours. "No, we primarily teach people to repell down the rocks". There was one 30 mile road (Burr Road) mostly paved to the interior. Definitely worth it.
Capital Reef National Park.
Located northeast of Bryce, just east of Highway 12 (124 miles of scenic highway that rivals Hwy 1 in Ca (Big Sur etc), a must see if you get out here), Capital Reef shows excellent examples of the different geologic periods. Once again, the rangers are excellent; can we get some of these people to teach in our schools or work in the government; they have great passion and are very knowledgeable.
Next layer (some purple) is the Chinle formation, which includes volcanic ash; depth varies in different areas. Next layer is Wingate Sandstone formation; accumulated when the area was desert like; some depths up to 3000 feet (compared to the Sahara, depths of only several hundred feet). Top layer is harder/more cemented, called Navajo Sandstone, looks more like limestone, cemented much harder than the Moenkopi. What then happens is called differential erosion, with the Moenkopi (softer) eroding more quickly than the layers above. The results are frequent and interesting landslides.
Tuesday, July 8, 2008
Beautiful Bryce Canyon Jul 2-6
Bryce Canyon National Park
Another masterpiece. All of these places are affected by the same elements. But the composition of the earth makes all the difference. Bryce Canyon is at the northern most and highest elevation of the Colorado plateau. Again, sedimentary remains and the uplift of the plateau set the table for the earthquake instability from Ruby's Inn Overthrust Fault. The fractures produced a checkerboard pattern. The 200 days/year of freezing temperatures produce expansion/contraction that cracks the rock. Bryce is famous for its "hoo doos", spires that have a hardened rock top (eroding more slowly) than the sandstone below it. The result is a fairly spectacular mix of spires that are magical to the eyes. Once again the rangers are wonderful (recommend you attend one of their lectures if you ever get out this way). These parks offer wonderul hikes from easy to strenuous, and the stars at night are amazing.
A great shot of Bryce, reminds me of a giant natural pipe organ.

Another shot of what they call "differential erosion"
A shot at sunrise point at, you guessed it, sunrise. Lot's of people there, taking pictures.
Took a 5 mile hike down to the base of the hoodoos; quite a bit of up and down; a full 1785 feet down from the top; this is a picture from below, looking up at the hoodoos. Did this early in the morning w/plenty of water. Felt good doing it.
After the hike had to climb back up to the top via a trail called "Navajo Loop", about 1200 feet, almost straight up. In order to get back up you have to go through this slot canyon (notice the steps on the right). As evidence of the instability of the rock, this boulder was part of a landslide in summer, 2006 that closed off the slot for awhile (no one hurt). As I was down among the hoodoos I wondered where I would hide if one of these things collapsed. Probably only saw 10 people along the entire 5 mile hike.
Going up the slot
Another masterpiece. All of these places are affected by the same elements. But the composition of the earth makes all the difference. Bryce Canyon is at the northern most and highest elevation of the Colorado plateau. Again, sedimentary remains and the uplift of the plateau set the table for the earthquake instability from Ruby's Inn Overthrust Fault. The fractures produced a checkerboard pattern. The 200 days/year of freezing temperatures produce expansion/contraction that cracks the rock. Bryce is famous for its "hoo doos", spires that have a hardened rock top (eroding more slowly) than the sandstone below it. The result is a fairly spectacular mix of spires that are magical to the eyes. Once again the rangers are wonderful (recommend you attend one of their lectures if you ever get out this way). These parks offer wonderul hikes from easy to strenuous, and the stars at night are amazing.
Another shot of what they call "differential erosion"
Tuesday, July 1, 2008
Cedar Breaks/Cedar City, UT June 25-July 1
Visited the spectacular Cedar Breaks National Monument, 10,000 ft above sea level, again part of the west end of the Colorado plateau, approx 70 miles north of St. George; erosion of a lake bed forms a very unstable amphitheater of eroded sandstone, colors of red, orange, yellow and even some purple. Only open 5 months of the year, while 110 in Vegas, it was 75 at Cedar Breaks with snow still visible on the ground. Perimeter continues to erode at 12mm/year; they have to constantly move the viewing areas back, and eventually will have to move the ranger headquarters. So many different landscapes.
One view of the amphitheater; you can see the edge of the viewing area at the bottom of the picture.
Another shot at a different angle. Depth is about 2500 feet down.
Nice spires, huh? Drive up to the entrance was pretty great also.
Lost in America.
Well, we hooked up and were going to Bryce Canyon over a mountain when we got an overheat light. Promptly stopped, cooled off, unhooked went back down the mountain to a town called Cedar City on I-15 about 60 miles North of St. George. Discovered a bad engine cooling fan, and replaced water temperature sensors (they read 15-20 degrees higher than actual). Hopefully will leave tomorrow. In the meantime, spent a few days in Cedar City, another pretty Mormon town (smaller than St. George); they call themselves the city of festivals, and home to Southern Utah University. Shakespeare Festival currently going on, Neil Simon Festival to begin in few weeks, and this past Saturday was "Groovefest", a one day long series of individual and group musical performances at an outdoor park in the center of town. Think a mini-Woodstock with a Mormon flavor (that should scramble your brain). Example: One country group kept saying they would be kicked off the stage if they didn't stop talking about "reefers", much to the crowd's delight. A lot of fun. Some adventure. Got a great haircut for $13.
St. George, UT June 21-25
St. George is a very pretty Mormon town, about 2 hours from Vegas (the trip on I-15 through the passes is breathtaking). It is continually rated as a top retirement location (I can see why), is in a valley that runs due north up to Salt Lake, bordered by red rocks (Snow Canyon) on the West and Zion Natl Park (Colorado plateau) on the East. Climate a little cooler than Vegas, gets cold in the winter, but very little snow. Happens to be the home of Vic Braden tennis academy (highly acclaimed) and the ajoining well known Green Valley Spa. The tennis academy recently had the Bryan brothers there, producing extensive video of their world class doubles strokes. I couldn't resist and took two lessons from the head pro (overheads and volleys). We'll see.
Area has been overbuilt a bit, but nothing like Vegas; some beautiful homes there at reasonable prices (compared to HH).
Also took another trip into Zion Natl Park; wonderful; can't believe how many folks are speaking other than English; I'll bet 33%, at least. Result of the cheap dollar?
Road trip through Snow Canyon; can you get used to the scenery?
Area has been overbuilt a bit, but nothing like Vegas; some beautiful homes there at reasonable prices (compared to HH).
Also took another trip into Zion Natl Park; wonderful; can't believe how many folks are speaking other than English; I'll bet 33%, at least. Result of the cheap dollar?
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