Written by Justin Zzyzx – Author of “Rockhound Barstow”
This location and many others are featured in the field guide – Click here to buy a copy for yourself

I just love exploring the nooks and crannies of the hills and mountains around Barstow California. The area around here is known for the beautiful geological formations all around, such as Rainbow Ridge, as well as the silver mines of Calico, once a silver boom town, now a commercial tourist attraction. Barstow, a perfect place to set up base and explore the Cady Mountains, Afton Canyon, Opal Mountain, Mule Canyon, Alvord Mountain, Yermo’s rolling hills of alluvial agates and jaspers and so much more. There is a veritable treasure chest of mineral adventures to be had in these colorful hills, visiting is a thrill, and I, as a resident, love to take full advantages of these rock deposits.

As a frequent leader of field trips and author of the “Rockhound Barstow” field guide, I’m always looking for new places to take people to collect interesting minerals and lapidary materials. My personal favorite is finding places where there are both nice crystallized minerals, as well as colorful lapidary material, that way, out of the dozens of rockhounds who have joined me over the past year on each monthly field trip, everybody is happy with what they can find. Exploring mining information on MRDS.org, I noticed several mines located in the Northern parts of the Calico mountains. I could see, just 10 miles away from my pistachio grove I call home in Newberry Springs, there was a Wollastonite mine, a Nickel mine and an Arsenic mine, all bunched up to the West of Coyote Dry Lake.

On our first outing to this string of locations we tried to access it from the East, coming up Coyote Dry Lake road. The dry lake was not as dry as we expected, in fact, it was quite moist and with no desire to go “muddin”, we turned back and tried the other way into the area, all the way around the Fort Irwin road passage, 20 miles to the West. Fort Irwin road is a VERY busy two-three lane road that connects Fort Irwin to Barstow and highway 15. Fort Irwin, a large Marine base, requires a large amount of workers from the Barstow area to work the service industry jobs, as well as the tech jobs, along with all the contractors, you can imagine this is a very busy road. We drove through the pass on the West side, looking at all the remains from the silver mines that made the Calico district what it was and what it is today. The ore was mostly chloragyrite, a silver mineral that is toxic to process, proving to be costly and environmentally unsound, so, the silver mines stand dormant, forever.

Entering on Madrugador road, Eastbound from Fort Irwin road, you pass by a Wollastonite deposit to the North, which we inspected with little of interest to be found, then, continuing along on this fairly smooth, slightly rocky road we turned off to the Northeast on a power line road which then takes us directly to the Wolly Wollastonite #5 deposit, a long abandoned deposit of this interesting white mineral. Some field guides have published this location, however, they always refer to it as an Onyx deposit. Onyx, a name for Calcite, is found at lots of places around the Calico mountains, however, at this deposit, there is only the non-stop white bliss of massive Wollastonite.

Wollastonite is a mineral that can be found as part of a Skarn deposit. Common related minerals are Grossular Garnet, Calcite, Quartz, Hedenburgite, and Epidote. The grains of the skarn deposits can be quite dense, leading to amazingly hard stones that can be worked into lapidary objects like vases and pillars. The wollastonite here was most likely mined for use in the pottery industry. Wollastonite, CaSiO3, a Calcium Silica Oxygen mineral that often has impurities of iron, manganese and magnesium, all elements found in abundance across this mountain range. Crushed, this powdered rock would be used for adding to clay, reducing cracking when ceramics are fired in a kiln, as well as added to paint base, a filler to make paint thicker.

At the Wolly Wollastonite deposit we would find tons of massive white wollastonite with the choice mineral specimens being the small bits and thin plates of acicular “long fiber” wollastonite crystals, which form flat on the surface of the rocks and boulders. Along with these, a bit of orange Grossular garnet can be found forming in the sharp borders between the wollastonite and the county rock. Finding larger pieces of this material is uncommon, but possible, however bits of wollastonite with thin areas of garnet are fairly common along the waste rock piles. In the quarried areas, along the rock wall, you can see several veins of garnet, but, in my opinion, they are not terribly thrilling. One thing is for sure, the guides that have continuously pegged this as an Onyx deposit can now be corrected in the next printing! The deposit takes up the Northern side of this far outlying mountain, spilling out of the most Northern part of the Calico mountains. Various bits and smears of other minerals have been spotted, like epidote and hedenburgite, so with further exploration you might uncover something interesting.

A few months before I decided to visit this Wollastonite deposit, I was told by a gold miner in the Hesperia area that there was a Wollastonite deposit up in the North Calico mountains that had terminated grossular garnets. Wollastonite forms as a part of skarn deposits. One of the best mineral deposits in these formations are calcite pods with glossy grossular garnets underneath. Locations around the world produce specimens like this, the calcite acts as a blanket for the garnets, protecting them from any harm, until we, rockhounds, remove them from the ground and soak them in acid to dissolve the calcite and reveal the beautiful garnets underneath. While massive garnet is found at the Wolly Wollastonite deposit, the lack of calcite pods at this and every other Wollastonite deposit I’ve visited has turned up fruitless. Yet, chasing this lead has brought me to explore some infrequently visited areas of the rocky desert hillsides.

Going back in reverse from the Wollastonite deposit, you can head South in the first turn, which is a wash that leads up to the solid hillside and upwards on a road that leads to a former Nickel deposit, resting on this craggy spire, a semi steep climb leads to a non-connecting circular road around the peak. From here you have spectacular views of the valley below, the vast white/tan of Coyote Dry Lake, the Coptic monistary, and hey, I can even see my house from up here! Looking at this location from the comfort of my home, with my imported mine marker data from MRDS, I could see this Nickel mine and also find out more information about it. It referenced a mention in a a Southern Pacific Railroad booklet on Mineral of Industry, Volume 3, which mentions the deposit geology as “niccolite, arsenopyrite, annabergite, and uvarovite in a verticle silicic dike that strikes NE along a shear zone in hornfels and quartzite.”

Off we went, to go visit the un-named nickel deposit. The wind on our first visit makes the location very memorable. We can have wind gusts over 65 miles an hour on some days around these parts and that day the wind was so forceful we were quite worried we would be swept off the mountain. Maintaining a tight foothold, we explored the area, looking for bright green crystals of annabergite and chrome green uvarovite garnets. Instead, we found the meaning of “silicic dike”! All of the minerals we have found at this location have been frozen in blocks of silica. While this does not do anything for us mineral collectors, it makes for a unique lapidary material. The same stuff as the classic German “Nickel Quartz”, this green stone takes a nice polish and the contrast of white and green makes for an interesting stone. Floating around in this silica, tiny bits of chrome green uvarovite garnet are found, while nothing to write home about, they do add a little something to some of the slabs and tumbled stones we produced out of this ore. If there were crystals here, this could be one of my favorite locations, but even in massive lapidary form, this in a rare treat in terms of mineralogy, a geat view-point in this area of the North Calico mountains and yet, just one of many locations in a short distance in this mountain range.

Just off to the Southwest, the road takes you to the Puerto Negro mine, a series of rock dumps that stop at a mine entrance a few hundred yards south of the beginning of the dumps. This is an Arsenic mine that produced an arsenic rich ore with the occasional bit of calcite and realgar. While I have not found many specimens at this location, the few I have found have been quite uncommon, orangy red realgar in layered clear calcite crystals. Drive North to connect back with the power line road and drive over to the next canyon to the South, taking Madrugador Road, home to several prospects for copper and gold, before heading back out to Fort Irwin Road. These gold deposits do not have much in the way of collectables for mineral or lapidary enthusiasts, however, they do produce chunks of calcite and masses of red, iron stained, quartz.

From here, it is time to go across Ft. Irwin Road, just a few hundred yards to the South, a road stretches out towards the Northwest, reaching out to several locations were crystals and lapidary materials can be found. The road is a very nice, mostly smooth flat desert dirt road. There are a couple tiny washed out areas, but most any passenger car can navigate the area. Immediately to the North, a small set of ridges spread out, the ridge to the West of the hills contains two locations to explore. A massive Barite locality called the Ball mine and a funky Wollastonite deposit with some odd rocks to be found. You pull off this new dirt road and into a wash road that loops around, park here and hike into the mountain valley to find the Ball mine, which is easy to see and high up on the hillside.

The Ball mine was a series of tunnels and surface workings that produced massive white barite, which can be found in abundance as lumps of heavy white rock. While unassuming, when exposed to UV light, these lumps glow a pleasing green and pink. There are tons and tons of this material laying around the mine adits, so you will have plenty to choose from. Continuing North into the canyon you will come across a Wollastonite deposit that has bits of calcite and some black rock that is said to be chromium bearing.

Back on the main dirt road, you continue Northwest for a mile or so until you come across a faint road headed South which leads to a large pile of rocks in the middle of the flat desert. It is unusual to see a pile of rocks such as this, however, this outcropping of rock is a happy accident for all of us. Here you can find a great deposit of Onyx, a flowing series of banded tans and yellows, along with bright red caused by iron impurities, along with areas of quartz, in the center of the stones as well as on the surface. Druzy specimens of quartz and calcite can be found, the only drawback is the size of the matrix they are sometimes attached to! The large chunks of stone cut to reveal beautiful patterns, while being nice and crack free, solid cutting material. It is remarkably easy to find, within a half hour at the location, cutting material to keep you occupied for days and weeks.

Traveling only another thousand yards to the West along the main dirt road, you come across the Noble prospect, a mineralized zone consisting of a short canyon wash to the East, with short adits that pushed out garnets, quartz, epidote and calcite. While we were hoping for garnets trapped inside calcite pods, these garnets are frozen in a quartz matrix, an while crystals can get up to an inch across in size, there is no way to free them from the host rock. Still, terminated garnets can be found in this area and the masses of quartz, epidote and garnet make for interesting lapidary materials. Just a short distance from this wash, a road takes you a few hundred feet to a bench in the mountainside, filled with boulders containing calcite crystals and quartz druzy, the druzy areas measuring up to and over one foot in size on several of the boulders. The trick is to find specimens that are small enough to take home. Several pieces showed evidence of layers of quartz covering and replacing the calcite crystals, which make for very interesting mineral specimens.

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