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title image - Pine Tree Wind Farm


Wednesday, September 12, 2018 7:13:36 AM

Pine Tree Wind Farm





Mankind has been harnessing the power of the wind for many millennia now. From windmills used to mill grain to sails for ships to windpumps and even chafing grain, wind was and is a free but unreliable power source. Modern industrial man almost completely forgot about the wind being used as a power source during his mad love affair with carbon based fuels. Now in the current era we find ourselves at the mercy of oil cartels, environmentalists, power hungry politicians, greedy automobile companies and a very spoiled population.

So now in the 2000's both solar power and wind power have become popular to the point that many people see both solar power and wind power as our salvation for our mobility freedom and independence from foreign oil/natural gas exporting nations. Public mass transportation in America is still a curse word and far too much of the population still considers public mass transportation as a device for getting the poor to government medical hospitals, Federal Aid centers and the local unemployment office! How totally lame and ignorant. See the Quick Facts PDF to refute this idea.

But fear not the wind is blowing up a storm and with it's sister solar power all will be saved! But at what cost? How many mountain ridges will be converted into wind farms? How many farmers will give under to the quick deal of cash so that their agricultural farms (used to feed the ever growing US population) can be plowed under to be re-made in wind/solar farms? How much of our western desert can be converted into solar power farms before the entire western desert looks like a massive aluminum stain across our landscape?

With those thoughts in mind let's go visit a wind farm in Southern California.

Many a traveler along the California State Route 58 going either Eastward or Westward through the Tehachapi Mountains between Mojave and Tehachapi will see a mass of wind turbines among the hills. This is the famous Tehachapi Pass Wind Farm. Back in the mid 1980's when I first traveled by motorcycle through the Tehachapi Mountains the wind farm was almost entirely concentrated on the mountains to the south of the freeway between the Sand Canyon road and the railroad overpass. Only a hundred or so wind turbines could be seen from the freeway. Now a third of a century has passed and the wind turbines have multiplied like weeds and have grown all over the Tehachapi Mountains almost down into the town of Mojave itself!

Photo of the Tehachapi Wind Farm from a aircraft
Tehachapi Wind Farm (via Wikipedia) showing how the wind turbines over the years have moved down the mountain side towards Mojave.

Presently the Tehachapi Wind Farm has about 4,730 plus wind turbines and altogether (maybe a dozen different companies) produce about 3,200 plus megawatts of electricity. Nice! But the Tehachapi Wind Farm has a significant amount of older kilowatt type wind turbines. What about a newer more current wind farm?

Going east from Tehachapi Wind Farm, along the southern Tehachapi Mountains paralleling the SR 14 is another wind farm that is set back further into the mountains. Originally known as the Pine Tree Wind Project but now that the LA Department of Water and Power owns the facility the official name is Pine Tree Wind and Solar Farm.

Access to the Pine Tree Wind and Solar Farm is normally via the Jawbone Canyon road which runs through, you guessed it, Jawbone Canyon!
image title - Jawbone Canyon
Where did the name "Jawbone Canyon" originate? And where is this Jawbone Canyon? European Americans (distinct from Native Americans) possibly named the canyon Jawbone due to the shape of the canyon acording to the Wiki.

"Europeans first settled in the canyon around 1860—naming it Jawbone because its shape resembled a mandible"

Really? But I have sincere doubts about this version for the naming of the canyon. So I am to believe that in 1860 the shape of the canyon was determined by what I imagine were a pack of European Americans gold rush miners, mule skinners, or prospectors climbing to the peaks of a dozen or so hills that surround Jawbone Canyon and then promptly after each hill climber was finished viewing his section of the canyon proceeded to huddle up with his peers and produce a composite map using pencil and paper that every miner carried in abundance!

I think the Myth Busters would blow up this myth quickly. Jawbone Canyon was probably named as such by one miner telling his fellow miners to just "follow my trail which will be littered with the jawbones of my dead mules cause I cannot find water anywhere"! Just my late night convoluted thinking.


So Jawbone Canyon is located in the south eastern Tehachapi Mountains just north of the SR14. The canyon was most likely made over many millennia by the Jawbone Wash, which is normally a dry wash. I am told that during winter and early spring a trickle of water may flow through the wash. A heavy summer downpour could lead to a flash flood through the canyon.

title image - Jawbone Station Visitors Center

aerial view of Jawbone Station Visitors Center
Jawbone Station Visitors Center, photo from the Friends of jawbone website.

First off lets get 1 item straight! Especially for the moron who penned a www.skyscanner.com review in 2017 stating:

"This blase ranger station is the worst facility of this type that I have ever been to."

"The primary reason to come here apparently is to get permits for ATVs n dirt bikes n maybe camping but that wasnt clearly disseminated from the volunteer staff member who i had to ring a bell for and it took about 5-10 minutes for her to show up".

This is NOT a federal or state run "ranger station" but is a privately run visitor center manned by volunteers from the  Friends of Jawbone! And on another note, when I visited the Jawbone Station Visitor Center in September of 2018 I found the site clean, manned by a nice fellow who let us know that in 10 minutes he would be closing the shop and asked us if we needed any assistance before he started to close up his booth.

Outside the front entrance of the Jawbone Station Visitor Center you might get a chance to meet "Bob" if you are there late in the evening. Bob is about 120 years old and is a Western Mojave Desert Tortoise who has been working as a mascot for the last 18 years!






1 / 8
Arrow and Arrowheads
2 / 8
Rocks and Atlatl
3 / 8
Bedrock Mortars
4 / 8
Desert Tortoise
5 / 8
Animal Diorama
6 / 8
Snakes and Lizard
7 / 8
Jawbone Flora
8 / 8
Bow and Arrowheads



Next we can start our journey up the Jawbone Wash on a Jawbone Road which goes from paved to dirt and back a few times ultimately ending up as a un-paved dirt road. Jawbone Canyon Road can thus be considered a roughly graded dirt road with patches of pavement in the lower elevations that ultimately connects the desert areas of Jawbone Canyon with the pine-covered Piute Mountain region which is about 38 trail miles away in the Sequoia National Forest.

Our journey only goes about 1/4 of this distance!

About 2 1/2 miles or so from the Jawbone Station you will see this whitish tube snaking across a ridge! This is part of the L.A. Aqueduct coming down from Owens Lake.

Jawbone Road with 2nd Los Angeles Aqueduct in the distance
Jawbone Road at LA Aqueduct. Plant life here is a mix sagebrush, creosote, pinion and maybe cheatgrass.

close up the LA Aqueduct at the Jawbone Road
Los Angeles Aqueduct at Jawbone Road

This is the 2nd of 2 aqueducts that the City of Los Angeles (DWP) built to remove most of the available water from the Owens Valley. The city of Los Angeles through it's DWP began a five-year construction plan in 1965 to build another 137 mile aqueduct to remove even more water from the Owens Valley. The cost of the second aqueduct in 1965 dollars was $89 million. Today that cost would be approximately $713 million!

Three items to notice in the above 2 photos:

1. The electrical power lines seen to the upper left in each photo are NOT from the Pine Tree Wind Farm but used at this point for the Beacon and Barren Ridge solar farms on the south side of the hills.

2. The aqueduct pipe itself has a water spigot and some form of catchment basin under the tube. Cannot find out what exactly this is. In the distance the aqueduct goes through the hills and then parallels the SR 14 highway until past Mojave.

3. Notice the hill to the upper right and to the left of the DWP dirt road going over the hill. OHV vehicle destruction can be easily seen. Are these trails that the OHV riders are supposed to follow or as one would expect that the Jawbone-Butterbredt ACEC and the Jawbone Canyon Off-Highway Vehicle Area are 2 polar opposites and the Jawbone-Butterbredt Area of Critical Environmental Concern is a horrible joke!


Above is a snapshot of the Second LA Aqueduct as it comes over the hills from the north. This is mid 1960 engineering tech. Later you will see early 1900's engineering tech of the original LA Aqueduct. You can see this feature from outer space!


This is the first Los Angeles Aqueduct built in the early 1900's. The project was approved by bond measure to the tune of $23 million (Wiki states $24.5 million). Today that would be $586 million or more!

The project started in 1907 and completed in 1913. Primarily engineered by William Mulholland and helped by former Los Angeles mayor Frederick Eaton.

The unbelievable irony here is that Los Angeles DWP now has to maintain this water thieving pipeline against the same people who use this area as a off-road vehicle playground who when finished with their "weekend warrior desert destruction" cycle head back down to Los Angeles to wash off their ATV's, water their lawns and then finally wash the desert dust off their trucks and vans using the same water that comes down through this pipe!


The above left photo shows 1 of the devices used to keep vandals and motocross riders off the aqueduct pipe itself. The above right photo we see a red sign post on the bottom left that states "Fence Line Ahead" which I imagine is required by law to inform ATV riders to NOT proceed up the hill or they might get de-capitated by the wiring of the fence. But if you look closely you will not see any wires or cables!



"TRAIL RIDING OUTSIDE THE OHV AREA: Outside of the OHV area and within the Jawbone-Butterbredt Area of Critical Environmental Concern (ACEC), motorized vehicle use is restricted to a specific designated road and trail network. All cross-country travel is prohibited in these areas, and the designated routes are marked with brown trail markers. You may only use the designated route network -- all other trails are closed -- even if you do not see a red closed sign."



RESEARCH ON OFF-HIGHWAY VEHICLE EFFECTS



Moving further up the Jawbone Canyon in the wash you will notice that the brush is thicker. Mostly likely due to the greater amount of water the plants receive here compared to plants on the hills beyond. This might be the Artemisia Tridentata type of sagebrush. But in reality it is Rabbitbrush!

Artemisia Tridentata — Big Sagebrush

Big sagebrush gets its name from its stature and its relation to members of the sagebrush group. Artemisia (ar-tay-MIS-ee-a) is from Artemisia, wife of Mausolus, ancient ruler of Ceria (southwest Asia Minor). She was named after Artemis, the Greek virgin goddess of the hunt and wild nature. Tridentata (tri-den-TAH-ta) means "three toothed," in reference to the three lobes on the tips of most leaves. Also called big sage, common wormwood or basin sagebrush.

Big sagebrush is the most abundant and widespread of all the species of sagebrush. Big Sagebrush has four distinctive subspecies, each with multiple geographic races that are sometimes named as varieties. Hybridization between subspecies is common, often making clear identification next to impossible.

The fourth subspecies (4) is Parish big sagebrush (subsp. parishii). It is similar to Basin big sagebrush in form and habitat, except that it extends southward from the Great Basin into the Mohave Desert shrublands, is more heat-tolerant than the other subspecies, and it has drooping inflorescence branches and hairy seeds.

Flowering period: Late summer to late fall.

For more information see the Sagebrush Pocket Guide from www.sagestep.org


The fencing seen here I suppose was used to keep out vehicles and prevent them from using the wash as a OHV area. Uhh this fence could not keep a 6 year old on a tricycle from entering!


Paved portion of the Jawbone road with Wind Turbines in the distance. The direction here is northwest. Notice that the hills are becoming mountains.

Rugged landscape olong the Jawbone Road Rugged landscape olong the Jawbone Road
Sagebrush dominated lowland and wash area with creosote bush on the hills.

Guard Shack at the end of the road

A typical guard shack or in this case a stunted trailer! Looks like the guards have a portable electrical generator and the always useful Port-a-Potty! 

Wait. What? A portable gasoline or diesel electrical generator will all that electricity being generated by those wind powered generators in the background!

Notice different types of sagebrush. The sagebrush in the wash is greener and fuller than the bushes along the side of the road and the small bushes clinging to the side of the hill are completely different altogether.

Nice fence fellows, the half fence to the left that is! Uhh what is it used for? Because it does not look as if it could stop that 6 year old kid on a tricycle we spoke about earlier when we were further down the wash.

At this point we will need to use a Arabian Flying Carpet to see the Pine Tree Wind and Solar Farm! So lets take a magic carpet to Part 2 of this overly large page.

 
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Getting to Jawbone Wash, Jawbone Road, Jawbone Canyon, Jawbone Canyon OHV Area and the Friends of Jawbone Station.

Below are directions provided by:
Bureau of Land Management
Ridgecrest Field Office


Latitude/Longitude 35.312571 / -118.050022

Directions Jawbone Open Area is located off State Highway 14, approximately 20 miles north of the intersection of State Highway14 and 58 in the town of Mojave. A left turn from State Highway 14 onto Jawbone Canyon Rd., when traveling from the south. Traveling from the north, it is a right turn onto Jawbone Canyon Rd.


Don't get confused about the 2 very similar sounding place names. The Friends of Jawbone Station is a volunteer manned station under contract with the BLM. Here you will find maps and a small wall of interesting books and a dozen or so dioramas of native wildlife and history.
Satellite image of the Friends of jawbone Station area Close Up Jawbone Canyon Store - Sat Image
Left is the clean Friends of Jawbone Station. Right is the messy looking Jawbone Canyon Store zone. Just saying .  .  .

The Jawbone Canyon store is a privately run operation where you can get rent a ATV, gasoline, oil, junk food snacks. Also looks like some RV parking in the back.


Desert Tortoise
Gopherus Agassizii


DesertUSA logo

Their are 2 main types of desert tortoise:

1. Sonoran desert tortoise
The Sonoran desert tortoise is flat and pear-shaped. The Sonoran desert tortoise is more active in summer.

2. Western Mojave tortoise
The Western Mojave tortoise which is more of a butterball shape; they are usually active in spring.

Photo of Bob the Desert Tortoise

These desert tortoises are herbivores that can grow to a length of 9 to 15 inches in (top) shell length. The desert tortoise will normally live in underground burrows to help it escape temperatures that can exceed 140 degrees F. The desert tortoise will spend at least 95% of its life in these burrows. There, the tortoise is also protected from freezing while in a dormant state from November through February or March.

The availability of suitable digging soil for burrows is a limiting factor to desert tortoise distribution. Some of their burrows extend only just beyond the shell of the tortoise inside. And this fact is another valid reason why the desert tortoise needs protection from vehicular traffic as the burrows can easily be crushed by off road vehicles. Other burrows may extend for several feet but the opening can still be caved in by vehicular traffic. A single tortoise may have a dozen or more burrows distributed over its home range. These burrows may be used by different tortoises at different times.

Read more about the desert tortoise in a full length article from DesertUSA by clicking the Logo below.

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logo for the Bureau of Land Management



STAGING AND CAMPING AREAS: The entire OHV area and surrounding public lands are open to primitive camping. Within Jawbone Canyon, there are a number of excellent primitive camping sites and OHV staging/off-loading areas. Most of the sites within the OHV area are accessible by 2-wheel drive vehicles with trailers.

BLM map of the Jawbone Canyon OHV Area

TRAIL RIDING OUTSIDE THE OHV AREA: Outside of the OHV area and within the Jawbone-Butterbredt Area of Critical Environmental Concern (ACEC), motorized vehicle use is restricted to a specific designated road and trail network.

All cross-country travel is prohibited in these areas, and the designated routes are marked with brown trail markers. You may only use the designated route network -- all other trails are closed -- even if you do not see a red closed sign.



Owens Lake should be properly referred to as Owens Dry Lake Bed!

Google Maps, Yahoo! Maps MapQuest and Bing Maps all used to show Owens Lake as a blue lake full of nice fresh water. Now Google maps is one of the last to move to some form of reality.

But in reality it looks like this. The satellite image give some stark reality to the current Owens Dry Lake Bed!

Don't let that puddle of water fool you. It is just dust mitigation forced upon LADWP by a court injunction!






Just a few miles to the north east of the Jawbone area we have the Red Rocks Canyon Park. A study in June of 2007 reveals the how and why OHV's are such a threat to the desert lands. Red Rocks Canyon is not any different from the Jawbone Canyon area with both zones having significant and permanent damage to the landscape. If you do not believe me then READ the entire report below from the California State Parks.

Effects of Off-Highway Vehicles on Archaeological Sites in Red Rock Canyon

Excerpt from the above article:

A large volume of published research exists concerning the effects of off-highway vehicle use upon public lands, including, numerous studies in the California deserts (e.g., Belnap 1995, 2002; Brattstrom and Bondello 1983; Bury and Luckenbach 1983; Eckert et al. 1976; Gilbertson 1983; Havlick 2002; Hinckley et al. 1983; Kassar 2005; Lathrop 1983; Lovich and Bainbridge 1999:315-322; Lyneis et al. 1980; Shore 2001; Sowl and Poetter 2004; Webb and Wilshire 1983; Wilshire 1977, 1983; and others). Scientific research on OHV effects initially grew out of a response by federal and state land-managing agencies to the exploding growth of vehicle recreation in the late 1960s and through the 1970s. According to this research, off-highway vehicles damage soils directly through (1) disruption of the surface soil and (2) compaction of the surface soil and subsoil (e.g., Belnap 1995, 2002; Dregne 1983:26; Webb et al. 1978:228-232). The most important long term effect of OHV use on public lands is the accelerated erosion and the attendant inability to support natural revegetation (Webb et al. 1978:219). Dr. Howard Wilshire (1977, 1983), then a geologist with the US Geological Survey, states that none of the natural soil stabilizers inherent to California deserts can hold up to the damaging effects of repeated vehicle passes. Even a single pass by an OHV or any vehicle upon desert soils can be sufficient to effectively destroy soil components (Wilshire 1977:ii). Tuttle Ridge, a landform found in Red Rock Canyon SP, is a prime example of extraordinary soil and plant loss from OHV use (see the observations in Wilshire 1977:6-8). Soil and sediment loss in the areas disturbed by vehicles was determined to be 11 million kg of material (Wilshire and Nakata 1977). Ongoing gully erosion and highly visible scarring on Tuttle Ridge over 25 years after its closure to vehicle use are manifestations of past unregulated OHV recreation (Figure 2, pictured below).

Figure 2. Tuttle Ridge is a prime example of soil and plant loss from OHV use.

Rabbitbrush
Rabbitbrush (Wikipedia)

rabbit bush - pleasantly aromatic shrub having erect slender flexible hairy branches and dense clusters of small yellow flowers covering vast areas of western alkali plains and affording a retreat for jackrabbits; source of a yellow dye used by the Navajo. Chrysothamnus nauseosus, rabbit brush.




Here is the route taken through Jawbone Canyon up to the guard shack.

In the above satellite image you will also notice a couple of geological anomalies. I have circled one in orange and the other is a polygon area outlined in turquoise.


The area in orange is interesting in that from a satellite view the white area almost looks like snow! And yes at time during a wetter and colder winter this area can be covered in snow. But his is NOT snow. But chalk or more likely gypsum.

Lets take a closer look.


You can see a well defined dirt road leading south from the Jawbone Canyon road to this area.

Now for a close up image of this area . It's a mining operation! Or better stated a surface mine of either chalk or gypsum as stated earlier.


In the below image we have 4 areas I found interesting:
  • A- mound of gypsum, ready for loading and shipment.
  • B-Backhoe used for loading the gypsum into center dump trailers or dump trucks.
  • C-Unknown peice of mining equipment.
  • D- Mine face or wall where the gypsum is actually being removed from the mountain.


Here you can see the mound of gypsum and the backhoe loader clearly.


Closer view of the unknown piece of mining equipment and the mine pit area.


Below is a 3D view of the mine operation but with the view turned 180°. I am very curious as to what type of machinery this is?


geological anomalies in the Jawbone Canyon area outlined in a satellite image


Another feature that can be seen when traveling up the Jawbone Canyon Road just as you turn the corner in the area marked in turquoise above.


Above is the area of interest marked in Red. It is another geological feature seen often in the Western Desert zones.


Above we can see something else clearly other than the large amount of Blue-green rock. ATV trails everywhere!

This Blue-green rock outcrop is considered sacred by the native Americans who once inhabited this area.

Below we can get a better look at this hill of Blue-green rock. And what is this blue-green rock anyway?

Chrysocolla is the scientific name. And this rock can be found in many locations throughout the desert southwest. It is usually found this Blue/Green form thay is known as Chrysocolla. It is NOT Turquoise!



Chrysocolla can be mined if large enough amount of copper can be found in the ore sample. It's the copper mineral that gives the rock it's blue-green coloring. It's the mineral oxidizing with air, just like old copper and brass fixtures.

If you look closely in the last photo above you can see that a open pit mine operation or a gravel pit was once tried here.