They are having the Riverside Co Fair & National Date Festival. We have been waiting for this for a couple of weeks, they are having Camel and Ostrich races at 3 and Cheap Trick playing at 7:30. Both on Friday and come to find out, it is ½ price day so charge is only $5. The camel and ostrich races were more silly than we anticipated, but entertaining none the less. Cheesy comedy show and very short track, but they did actually race. We had a hard time finding dates for sale, but did manage to have a date shake (tasted like vanilla with raisins) not bad. Of course, we visited the free buildings and toured the crafts, juniors and model trains buildings. We have to brag on May Ma Moore, the quilting at the Riverside Fair competition could not hold a candle to yours. You do amazing work and so original please keep it up.
This week Palm Springs is having “modernism” week, based around their modernism architecture. We found a free tour, but it was a bike ride. It was not as bad as imagined, but also did not take any pictures since I was riding a bike. Actually, cooler than normal temps mid 60’s sunny and beautiful surroundings made for a great 7 mile ride. The tour featured midcentury modernism neighborhoods designed by William Krisel, the homes are mostly 1 story with flat or “butterfly” roofs. Very modular and smaller than anticipated. New these homes sold for $20k, today they sell $800k to $1.3M. May ride back thru before we leave for pics?? Begin the ride…
Joshua Tree is now a naturalist’s mecca, but in days gone by it was used for ranching, cattle rustling and gold mining. There is some of the past civilization remaining to be explored. The most complete example is Keys Ranch which we did not visit because it is only accessible via a paid ranger guided tour and we are staying on the cheap.
Ryan Ranch although just ruins, was once a bustling ranch which housed approximately 60 people. While it was an active ranch the inhabitants also worked the nearby Lost Horse Mine. There was a well at the ranch which supplied water to the mine 3 miles away and 750 ft. higher than the well via a pipeline. There was evidence of the pipeline around the ranch, not sure how they pumped the water uphill, but expect they utilized the windmill. The original walls from the house were adobe. What is left had been covered by a concrete layer?? Don’t understand why, the concrete layer is falling off and is obviously not original since it covers the walls at their existing height not where they originally were. The adobe bricks are the original walls.
In addition to the well there was also a small “tank.” Tanks are basically small dams used to hold rain water. Call it global warming or simply climate change, but this part of the desert used to have a lot more rain fall than it currently does.
Near Keys Ranch is Barker Dam. This dam was constructed around 1900 by cattlemen and raised by rancher Keys in 1950. You can see the original portion on the backside where there is a stone face and the new level constructed with concrete. It appears that the Keys tried to rename the dam during their use see the inscription in the concrete “W F Keys – V Keys 1939.” The lake appears to be very low in comparison to the water level on the surrounding rocks. Note the water line is taller than me and I am on dry land. This may be due to recent Southern California droughts or again lessening rain fall in the area??
Further along the Barkers Dam hike are some Petroglyphs or rock drawings. These have not been dated, but were definitely used by native American Indians as land marks. The dam might have been a natural “tank” before the dam was constructed? The petroglyphs may be pointing this out? Petroglyphs are not naturally as bright as these are now. They were painted over for use in a Disney Movie in the early 1960s. Reports differ as to whether they had permission to do this or not??
Another nearby hike is thru Hidden Valley. A diverse valley surrounded by high rocky walls which is currently a mecca for rock climbers, we stayed and watched for a while. Kind of crazy, they work so hard to climb up these rock walls and don’t even stay to savor the moment, they just repel back down to do it again?? The valley is thought to have been a favorite for cattle rustlers since it was well hidden and has diverse vegetation for grazing. Beautiful area and a nice hike.
This trip to Joshua Tree was about a week since our last and towards the end we found that the Joshua’s have begun to bloom. Not sure if the recent rain helped the process or not, but we think so. The info we find says they bloom from Feb to April so maybe they are just on time. It is raining again today so hopefully this will be good news for the wildflowers and cacti as well.
Palm Springs has an aerial tram which climbs Mt. San Jacinto the snow capped mountain to our left. It climbs almost 5,400 ft. and the floor rotates while you go up for a 360 degree view. We thought very hard about going up and seeing the snow covered mountain and the view, but it is a little pricy for us. After parking fees and tram fees it would be over $60.00. So we decided to drive up Mt San Gorgonio in San Bernardino National Forest the highest peak in Southern California at 11,500 feet. We see Mt San Gorgonio to our right. The valley between Jacinto and Gorgonio is filled with windmills and is directly in front of us.
There was not a road to the summit or if there was it was closed. The highest we got was at Onyx Summit at 8,443 feet. Which has a nice view of Mt. San Gorgonio and the surrounding area.
We took Ca Hwy 38 winding around the mountains. There was very little development, some camps and recreational areas, but no real towns. The area was gorgeous and the snow really added to the beauty. You may remember me saying that I could care less whether I ever saw snow again or not, so you may find it weird that we went up. The weather was great even with the snow it was 50 degrees and sunny. Really made for a nice contrast.
Further down and around the northern side is Big Bear and Big Bear Lake. We had our picnic there and enjoyed the lake and Nellie getting a run in the snow. There were numerous ski resorts in the area.
In Big Bear we hit Ca Hwy 18 and traveled back west along a scenic drive called the “rim of the world highway.” It runs the length of the San Bernardino Mountains right across the top. When we started out we were surrounded by these beautiful snowy mountains.
And then we turned a corner and the snow disappeared. The mountains were very lush and green, you can see the city of San Bernardino in the distance.
The drive was amazing and quite a nice change from the desert of Joshua Tree. It was really nice to see trees again!!!
We have spent most of our time enjoying our natural surroundings, but have ventured into town on a couple of occasions. The area has several towns that run together into one. Only signs tell you when you go from one to the other. There is Palm Springs, Desert Hot Springs, Cathedral City, Palm Desert, Rancho Mirage, Thousand Palms and Coachella just to name a few. Below is our home for this month address is Desert Hot Springs, signs say Sky Valley??.
Palm Springs has stars on the sidewalk similar to Hollywood (I hear have not yet seen theirs). Most are people we have never heard of but there are some familiar names.
They also have a nice art museum which is free on the second Sunday of each month. We enjoyed the free visit. Their feature exhibit was of cowboy and Indian art; but the permanent exhibits included baskets, modern art, glass, sculpture garden and much more.
Cathedral City has a really nice fountain that made us think of Teresa Sandeford. It is mosaicked aquatic animals. The first day we went by it was a nice sunny day but the fountain was not running?? When we saw the fountain running it was a cloudy overcast day so the colors did not come out as well. We are going to start a petition for the Town of Carolina Beach to commission a similar fountain utilizing Teresa’s mosaics, she has already done most of the businesses so why not. Check out her work. http://www.mosaicsbyteresa.com/
There are some interesting rules also. Guess they saw the need??
Peace and love from Southern California desert, while lying on the sidewalk!!!
We have been busy this last week. Great weather with high temps in the upper 70 and lower 80s and crystal clear skies. Yesterday that all changed with a southern California winter storm. The main part of the storm is on the western side of the mountains, the desert doesn’t get much rain but the wind has picked back up and the mountains are hidden by clouds. There was rain overnight and flash flood warnings, but just wet and cloudy today so far. Hopefully the rains will bring wildflowers in the next couple of weeks before we leave?? Yesterday and today enjoying staying in, restocking, washing and making some stew since the temps this weekend are to be below average with highs in the 60s. Also catching up on our blog!!
Of course, we went back to Joshua Tree. We took the self-guided geology tour, an 18 mile off road tour of various geological formations. When you realize that many of the rocks and formations have been created over 1.7 BILLION years, it really makes our life span seem very insignificant. Being from the coast, we understand erosion as it relates to the beach, but to realize that the mounds of rock all around Joshua Tree were once mountains that have since eroded is fascinating.
Some of the mountains are still intact. This is because the rocks in these mountains are harder than others and erode much slower. All mountains are still eroding, it is just a matter of how fast the erosion occurs. The intact mountains are formed from 1.7 billion year old Pinto Gneiss which is a metamorphic rock. That means that this rock was formed from pressure, heat and chemical activity and is much harder and erosion resistant.
The mounds of uncovered rocks are 85 million year old White Tank Monzogranite. This rock was formed when molten magma intruded the gneiss. It cooled much slower being 15 to 20 miles below the surface and is therefore less dense than the gneiss and erodes much faster. You can really see that the rock is softer it looks and feels much like concrete, rough and grainy. While the gneiss is smooth. The erosion of monzogranite and sediments around it that have created the “piles” of rocks and interesting formations. So, each “pile” used to be a mountain and after erosion of that mountain these piles are what is left. Just imagine what it looked like millions of years ago!!
The white tank monzogranite cracked while cooling from molten magma and created joints. Over time some of these joints refilled with more molten magma and created dikes which are still another type of rock either aplite (light colored) or pegmatite (darker). This is what created the veins in some of the large boulders. It erodes slower than the monzogranite and sometimes protrudes out of the large boulders. Where these joints did not refill they eroded and formed the boulder formations. Some look like children’s blocks stacked on each other while others have rounded off and look like marbles. This is due to various stages of erosion.
You can also see strange pits and hollows on the rock surface where irregularities in the rock trapped water. This moisture promotes chemical breakdown of the rock to clay which holds more moisture. As they erode they produce shade which in turn promotes more moisture and before you know it (millions of years) you have a large hollow in the rock. Some as large as a cave, they are much cooler and a nice respite from the sun and heat of a hot day. These hollows create some of the distinctive images in the park.
Beyond these two kinds of mountains and rocks on the geology trail, there is a third much younger mountain. This mountain is believed to be as young as 2 or 3 million years old and is made of black basalt. This is believed to be formed from molten magma intruding into the monzogranite but not quite reaching the surface. The Basalt is more resistant to weathering than the monzogranite. The former layer of monzogranite that covered the basalt has since eroded and become part of the valley surrounding these young mountains.
This is an elementary geology report which could be better explained by some of my former co-workers (geologist) at Clark Environmental. But is what I understood from our brief class via the self-guided tour. Well worth the time. Although I did not mention it earlier, of course earths movement especially here on the San Andros fault line contributed (a lot) to the mountains formation and cracking of rocks over time.
Below you can see the difference kinds of rock side by side.
and the difference in erosion rates on the edge of this mountain.