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Hiking | 0.43 Miles |
41 AEG |
| Hiking | 0.43 Miles | 16 Mns | | 1.72 mph |
41 ft AEG | 1 Min Break | | | |
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| partners | | After Wall Street we headed up to Keys View. It does indeed have quite the views but it was really windy and it's very crowded. We walked up to the top and had a beer but ended up walking back down to the main area to get out of the wind. It was a great area for people watching and also two lizards at play.
The Keys family created one of the most successful homesteads in the Joshua Tree National Park area, and this viewpoint is named for the family and the ranch that sits near the Hidden Valley Nature Trail and campground. From this 5,185-foot overlook in the San Bernardino Mountains you'll gain an excellent view of the Coachella Valley and the Indio Hills that mark the San Andreas Fault's course through the valley. Keys View is a great spot to contemplate the forces at work here, as you can see the earth rise from near sea level on the valley floor all the way to the 10,834-foot summit of Mount San Jacinto. The collision of plates (Pacific and North American) at the fault creates this massive uplift immediately west, the steepest of its kind in the country. (Fits right into the series I am currently watching: Voyage of the Continents)
Palm Springs sits beneath Mount San Jacinto, and Indio is the town to the south along I-10, its location marking sea level. In fact, this entire Salton Basin would be part of the Gulf of California were it not for the massive deposits made by the Colorado River over millions of years. Because of these deposits, the basin remains below sea level and still dry, at least for the time being. The basin has hosted lakes in the past, as is evidenced by the dry beds and the Salton Sea itself, which is 230 feet below sea level and visible to the south on a clear day.
Next we headed for Cap Rock. It was a very quick loop hike but there was a lot to see and observe.
About seven to nine million years ago, the Mojave Desert was semi-arid, covered in soft rolling hills and vegetation, a vastly different scene than the dry, cactus-filled ground today. The granite bedrock was covered by soil which formed from water moving down through the rock, assisted by joints in the granite. Slowly, the jointed granite became more rounded, resulting in tall, elongated boulders encased by soil. As the landscape became drier, less water was available to chemically weather the rock and remove debris away, and soil stopped forming so rapidly. Rounded boulders and small rocks were left behind, no longer having enough water to carry away eroded material. Inselbergs can be found at Hidden Valley, Caprock, Jumbo Rocks, and Ryan Campground. They look like islands of rock. We passed a group at a ranger presentation. In the front of us was Ryan Mountain, where we had been this morning. We passed through another boulder hallway which is always so cool; literally, ha! Around the bend we came back to where we started passing by some nice Joshua Trees and then the big view of Cap Rock Tor. A tor is piles of massive boulders of granite – rock formations known as tors – towering the surrounding sparsely vegetated hilly landscape . These formations vary in size from isolated groups of boulders to entire mountains. (Reminds me a bit of glacial tarns except those are made of water.)
We checked out the kiosk which had a list of all the hikes with miles and elevation but no brochure of the same. I realized later I had that list saved in my gmail. We drove the hour home still enjoying our trip through the Pinto Basin and luckily again, not much traffic at this time of day. After dinner we had another starry nite to enjoy and shoot some photos.
Here is the video that I had to reload because youtube somehow got the Venus label in the wrong slide as their load timing must have been off. Anyway, it includes Keys View, Cap Rock and a few evening/nite shots: [ youtube video ] |
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Wildflowers Observation Isolated
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For me, sometimes it's just as much about the journey as the destination.
Oh, and once in awhile, don't forget to look back at the trail you've traveled. |
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