Ebooks for Rockhounds – Information at Your Fingertips

Our portable electronic devices have memory that allows them to store thousands of pages of information in the palm of your hand. To a mineral collector a century ago, it would sound like total magic. By storing a library of field collecting sites in the palm of your hand on the Kindle or other device, you’ll never run out of places to go. Perhaps to your surprise, many great guides are available in digital format so you don’t have to bring stacks of field guides or a cumbersome library of dated, out of print texts with you when you get muddy. The rockhound ebook revolution is happening now. Let’s take a look.

Check out all the ebook field guides listed for sale on Amazon!

As you can see, there are some great choices for guides on Amazon. Just by searching “rockhounding” in the Kindle ebooks section of Amazon, I got 55 results, most of them being informative guides to collecting sites and prospecting methods. Imagine how much information you can have at your fingertips! Mineral collecting books tend to be really affordable, I had a hard time finding one that cost $20 or more. Although the feel of a paper text is nice, you can’t beat the price and field-usefulness of these ebooks.

Searching “mineral collecting” brings up less field guides, but still a lot of them. Notice a trend? Seems like digital versions of field guides are getting popular! Take advantage of this.

Searching “mineral collecting” brings up one of the best recent field guide for collecting minerals in Southern California — Rockhound Barstow: Mineral Collecting in the Mojave Desert by Justin and Brandy Zzyzx. This great guide to collecting a wide variety of material gives you tons of sites that are currently open to the general public where you can find mineral specimens and lapidary material! If you had read some field guides, they will provide directions and info on sites, but note that they are closed to collecting. This great guide gives you places in SoCal you can actually visit and dig.

Another thing to mention, are PDF files of old texts and surveys available for free online. Museums, universities, personal websites of collectors, and state and national government geological surveys are some places where you may find many old texts that have been digitized for your convenience. Looking at these types of resources is a good way to find old localities. These types of texts often include sites that the newer guides do not, and while they require a bit more fishing around in terms of actually finding them and acquiring permission, the rediscovery of an old site might produce some amazing results.

Here is an example: https://www.des.nh.gov/organization/commissioner/gsu/documents/nh-mines1960.pdf

Screenshot of the PDF of this classic guide.

This classic guide by Philip Morrill, published in 1960 is notoriously difficult to find in print but known among NH collectors for the unique, often forgotten localities described within it. This book is something you probably wouldn’t want to bring into the field with you because it would be hard to get another copy. Now you can have the info in your digital library and bring it with you without trashing your copy

Ebooks and PDFs are a powerful tool for the collector looking to get themselves into new areas or sites. The advantages modern collectors have over previous generations due to the amount of technology and convenience available have allowed for a lot of new discoveries and rediscoveries of old localities. If you haven’t been using these resources and are itching to find a new place to hunt, then it’s time to step on board the digital library revolution!

Beryl and Pegmatite Minerals at the Simpson Quarry, South Glastonbury, CT

Overview: One of many abandoned feldspar prospects in Central CT, this particular location has been a popular beryl collecting site for several decades. This location is one of the most visited pegmatites in Connecticut if not all of New England and is somewhat of a local classic for beryl.

Large, sharp blue aquamarine beryls have been found both in the dumps and in solid pegmatite at this location. A variety of other minerals can be found at this site as well, including some rare species.

Conneticut Beryl Aquamarine Crystal

37mm tall beryl dug in 2009 by CT field collector Adam Berluti

Radioactive Mineral Torbernite found in Conneticut

2cm tall specimen covered with minute green Torbernite crystals. Roger Sedgwick collection. (Source: https://www.mindat.org/photo-494986.html)

This is one of the first sites many collectors in CT visit, and it is not hard to find something worth bringing home. The collecting status of this location is unclear (and with all sites featured on this website, you are responsible for obtaining permission and checking current property ownership), and as of early 2021 it remains unposted and is still frequented by diggers in the area.

Quarry dumps at the Simpson. Dig through these dumps to find nice aquamarine beryl crystals as well as many other pegmatite minerals like almandine garnet, schorl, torbernite, and columbite. (Source: https://www.mindat.org/photo-123808.html. Image copyright 2004 Peter Cristofono)

Quarry dumps with foliage down. Taken April 2nd 2011 by Matthew Kimball. (Source: https://www.mindat.org/photo-390478.html)

Getting there: This mine is easy to get to. Park at the end of Michele Drive in Portland, CT. You will see a small path through the woods to your left. Follow the path until you see the very obvious big quarry dumps approximately where the pin in the photo is. You will have to cross some swampy areas. The location is approximately a quarter of a mile northeast from where you park. A word of caution, the collecting status of the location is not officially known. Many people dig here though it may be private property. The locality has been frequented by collectors on a near daily basis for decades.

Location of the Simpson Quarry, and location of beryl crystals.

Collecting: There are two main approaches to digging this spot- dump digging and hard rock mining. At minimum you will want to bring a shovel, crack hammer and chisels to the location but other tools that may be useful are hand rakes, a sledgehammer, sifters, small bags, and a UV light. Many rare minerals are found at this site, some of which, autunite and hyalite, are highly fluorescent. The mosquitoes get terrible at this spot in the summer, be prepared with lots of bug spray. Pegmatite is an extremely hard rock and will take persistence to break. The mica and quartz can be extremely sharp so wearing gloves is a good idea. Do not get discouraged if you have a difficult time working the hard rock. Digging pegmatite takes immense skill and practice. It is something that experienced New England diggers take years to hone.

A large 6mm microlite dug at Simpson by Andrew Kruegel. A unique feature about this pegmatite is the abundance of this rare tantalum mineral. This example shows the typical form and color. A loupe can help you spot these more easily. (Source: https://www.mindat.org/photo-525514.html)

Geology and Mineralogy: This locality is very similar to the other Paleozoic pegmatite in CT. It is linear in shape and not very pocket rich. This pegmatite also contains a great deal of heavier rare elements. Collectors often visit this site only interested in beryl, but perhaps more notable to the mineralogist is the abundant microlite found in sugary albite. Microlite contains the rare element Tantalum. These microlite occur in brown modified octahedral crystals. If you are interested in them, familiarize yourself with them on mindat.org. Microlite is often somewhat radioactive and will produce a radiation halo, which is a good way to spot them.

Sources:

https://www.mindat.org/loc-29587.html

Sea Cliff Zeolites at Oceanside, Tillamook County, Oregon – A Zeolite Tutorial

Volcanic Basalt Lava is found all over the world. Often the host for beautiful minerals and crystals of quartz, calcite, agate and a host of zeolite minerals. The Amethyst deposits of Southern Brazil/Uruguay are considered the best quartz in basalt find, as are the fine Zeolite deposits of Southern India. Before India, many places were considered to be the world’s best zeolite deposits, like Scotland or Iceland.

It just goes to show, deposits of minerals in basalt rock deposits are well worth searching out in your local area. Consider the volcanic basalts of Oregon/Washington. Beautiful examples of rare and exotic minerals were once only known from these basalts, including, shockingly to some collectors, Cavansite!

Small Cavansite crystals on matrix from the type locality in Oregon

Specimen of Cavansite from the first place it was found, in Oregon. Zeolite deposits found in volcanic deposits are well worth inspecting for rockhounding possibilities!

Found in volcanic lava that has interacted with water, zeolites are beautiful minerals which are found in a huge diversity of different appearances. They are known to form where enormous volcanic events have occurred in the ancient past when lava flows into a body of water.

The lava instantly chills, creating a unique bubbly, rounded texture called pillow basalt where within spaces between the rounded “pillows” grow delicate crystals of zeolites as steam chemically leaches the basalts and forms new minerals.

Steam may rise through the molten lava as well, where the rock may solidify before it escapes. This type of rock is called a vesicular basalt. Many minerals tend to form in the “bubbles” or vesicles in this type of rock.

Pillow Basalt that zeolites are found in

A recently formed pillow basalt at the Galapagos Rift versus an ancient pillow basalt in the Bonin Islands, Japan. Zeolite minerals are found between the “lobes” of the lava.
A vesicular basalt boulder. The holes are known as vesicles and represent where rising gasses got trapped in the rock. Minerals often form in these vesicles.)

The Cape Lookout area is the remains of a volcanic island that emerged in the Miocene period, about 16 million years ago. Cracks in the earth formed, releasing lava into the sea which cooled on contact with the water, forming pillow basalts and bubbly vesicular basalts which further altered to form zeolite minerals in the pores.

Many rare zeolites are found here, not the ones you would typically see in the large, flashy specimens from India many collectors love, but equally as beautiful if you can appreciate tiny things. Minerals you may encounter are erionite, mordenite, clinoptilolite, and dachiardite. Often these are found with calcite and clay minerals, the latter can give specimens some nice color and visual depth.

Specimens from this area are typically small, but absolutely stunning especially under magnification. A good, readily available microscope to view your microminerals with is the Dino-Lite, which you can attach to your computer via USB.

A Dino-Lite digital microscope.

On this page, our focus is on two collecting sites you can visit, though exploring the beach may yield many more discoveries. Keep an eye out for sprays and nodules of zeolite minerals in the rock, much of which occurs in vesicular basalt, which looks like Swiss cheese.

The first area is Short Beach. There should be a stairway near a creek where you can access the rocky beach below. Here you will find boulders of vesicular basalt that you can break up to yield minerals in the vesicles.
Bring a pocket lens or loupe with you so you can more easily see minerals in the vesicles. They will be somewhat obvious, appearing as white puffballs and sprays, but some may be more hidden.

There is said to be better collecting even still at Tunnel Beach, down the road to the south.

North of the tunnel, you will see pillow basalt cliffs. Formed as lava was ejected into the sea, these cliffs and the surrounding boulders are rich in zeolites and offer some of the best collecting in the area. Use the tunnel to access the beach.

Minerals: These localities are heaven especially to the micro-mount collector. Some beautiful photos of material from the surrounding area are on Mindat (these are copyrighted and we don’t care to hotlink, just click the links for some great photos).

Embed:
https://www.mindat.org/photo-750805.html
Caption: Found by Rudy Tschernich, famous PNW zeolite collector. 14 mm FOV Golden erionite hemispheres on a white backdrop, looking like a fried egg with a broken yolk
https://www.mindat.org/photo-750632.html
Tiny, bushlike mordenite in a tiny vesicle from Tunnel Beach. Found by Rudy Tschernich
https://www.mindat.org/photo-257230.html
About a 1 inch wide plate of green gray clinoptilolite on mordenite from Short Beach, collected by Bill Tompkins
https://www.mindat.org/photo-751603.html
Tiny, about 2.5mm vesicle of delicate golden erionite sprays. Found by Rudy Tschernich

Collecting Zeolites: To do the best job you can collecting these delicate specimens, you will need to be prepared to break the hard basalt rock. Use a heavy crack hammer and a chisel to smash the boulders open, revealing fresh material. Zeolites are extremely delicate and the freshest, nicest ones will be found unexposed inside the rocks.

As said above, loupe or hand lens will help you see what’s going on inside the tiny vesicles a lot better. Some of the most beautiful specimens from this location are extremely tiny so you may miss them without a lens.

Remember to wrap your specimens very carefully. Many of these specimens are extremely delicate to the point that even blowing on them may damage them. Do not wash anything very velvety, hairy, or puffy or even moisture can mat and destroy the crystals.

You will have to time your collecting with the tides at these locations. Be aware of the tides and weather conditions before you go to the beach and collect.

More Info:
https://www.mindat.org/loc-210854.html
https://www.mindat.org/loc-205422.html
https://www.netartsbaytoday.org/html/zeolites_of_oceanside.html

And, if the Cavansite deposit sends your imagination wild, check out this article:
https://www.mindat.org/article.php/964/Field+Trip+to+Cavansite+Type+Locaility

Holiday Gift Guide: What to Get for the Rockhound in Your Life

Rocks! (Or maybe more properly in this case: "Minerals")

The holiday season is rolling in quickly and that means it’s time for gifts!  But what do you get for that special rockhound in your life?  We’ve compiled a holiday gift guide for you!

Disclaimer: Every rockhound is going to be a little bit different, but here are some ideas for you to consider.  Once you’ve spotted the perfect item, we suggest a Google shopping search to find the exact model that will work for you.  We can make some recommendations of items that have worked well for us, but take a look around and shop smart!

1. Rocks.

Rocks! (Or maybe more properly in this case: "Minerals")

Rocks! (Or maybe more properly in this case: Minerals!)

Obviously.  Because what rockhound doesn’t want more rocks?  But let’s be honest, some of you might not have any idea WHICH rocks your rockhound will love.  We have good news!  Many mineral dealers, lapidary companies, and others in the mineral trade DO offer holiday gift cards and holiday promotions!  Take the trouble out of choosing a rock and let your loved one choose their own!

Yeah, yeah, we know that gift cards kind of get a bad reputation.  But from a true rockhound, the idea that I can go into a dealer’s inventory and pick out something I LOVE is definitely exciting in a way that a gift card to the local fashion boutique will never be.

So how do you find the right company to go through?

First, decide what kind of material you think your rockhound will love – some love mineral specimens, others love gemstones, and others love just rough lapidary material!  Find a company that deals in the material you’re looking for.

Next, find a company that has a great reputation.  Checking out Facebook and other reviews is a great way to establish whether a company has a good reputation amongst its customers.  If you know that your Rockhound has had good relationships with a company in the past, go with that one!  (And if there’s a small-time company in your area, think about sharing the love by shopping local!)

Finally, if the company you’ve found doesn’t have a posted notice about gift cards or holiday promotions – ASK THEM!  Shoot them an e-mail or a message to their Facebook page – chances are, whoever receives your message will be happy to work with you!

 

2. Tools.

Every rockhound needs tools.  Similar to a rockhound’s choice in rocks, a rockhounds choice in tools might be a little difficult to pin down.  We’ve got a few ideas for you though, so take a look at some of these items to see if any of these seem like they fit your rockhound!

The Rock Scoop

A rock scoop in use by the Apollo astronauts to collect lunar samples!

A rock scoop in use by the Apollo astronauts to collect lunar samples!  Because the suits worn by astronauts made bending over nearly impossible, the rock scoop allowed them to collect rock and soil samples for return to Earth.

Though your rockhound might not be likely to be collecting on the moon, this is a proven tool.  A favorite amongst those who do a lot of beach combing, the rock scoop is a handy gadget that lets you scoooooop up your treasures without bending over.  This saves your rockhound on back and knee strain!   Of course, this tool works well in places other than beaches too (you know, like the moon!)!  We wouldn’t recommend this for the rockhound that likes to hammer on rocks, but for the collector who likes to walk along and pick up treasures, this is perfect!  (It can also double as a walking stick!)

There are a lot of different models of this tool out there.  Some feature a scoop with holes to let smaller debris fall through.  Some are collapsible for easy transport.

The Rock Hammer

The Rock Hammer - the most essential tool of the Rockhound!

The Rock Hammer – the most essential tool of the Rockhound!

Now, for those of you who have a rockhound who likes to do some damage on your hands, there is no tool more critical than the rock hammer.  And even if your rockhound already has a rock hammer, check it!  These tools wear out over time, so a new hammer is never a bad thing!

There are a lot of choices in this department, but make one important distinction: NEVER think that a regular hardware store hammer is the right tool.  It’s not.  Be sure that whatever product you choose is labeled as a rock hammer or a geologists’ hammer.  (This author has had great experiences with the tools made by Estwing, but there are certainly other choices out there.)

Note: if you need a stocking stuffer to go along with your gifts, some eye protection is always a great idea when using these tools.  Throw in some safety glasses!

The Geo/Paleo Pick

The Geo/Paleo Pick - perfect for a competition over who's pick is the biggest...

The Geo/Paleo Pick – perfect for a competition over who’s pick is the biggest…

Now, some of you might have a rockhound who’s mastered the rock hammer and needs something bigger.  That’s where the Geo/Paleo Pick comes in.  This tool features a longer handle for maximum power in the swing.  It also has two tips: one pick-end for, you know, picking.  The other end is broader and flatter and makes a great tool for scraping away debris.

There aren’t many choices available for this tool, so Estwing is a solid choice.

The Gad Bar:

The Gad Bar - for poking and prying.

The Gad Bar – for poking and prying.

The gad bar is a tool with a little more subtlety than the hammers and picks, but it is incredibly useful.  This is the rockhounds version of the pry bar.  There’s a pointy end for sticking into crevices, and  a chisel shaped end for wedging into cracks.  This tool is great for working in areas where you don’t have the space to make big swings with a tool, or in situations where all you need is a little leverage.  (Note: this is the author’s favorite field collecting tool.)

 

3. Information

One of the most important things you can gift a rockhound is the gift of information!  Here are a few different resources you can tap to help your rockhound get more educated!

Field Guides

Fred Pough's classic Field Guide to Rocks and Minerals

Fred Pough’s classic Field Guide to Rocks and Minerals

Field guides come in all shapes and sizes.  Some will cover topics related to field identification of rocks and minerals.  There are lots of options in this department!  Pough’s Field Guide to Rocks and Minerals has long been a favorite of rockhounds.  The author also recommends Sorrell’s Golden Guide to Field Identification of Rocks and Minerals.

Others tackle the subject on a more regional level and will give your rockhound ideas about new places to go and what can be found there.  Check out our section on Field Guides for more regional guides.

Magazine Subscriptions

Rocks & Minerals Magazine

Rocks & Minerals Magazine

Books are a great gift, but several rockhound magazines are also available.  Of course, the major perk to a magazine subscription is that you get new information delivered monthly or bimonthly!  Several well established magazines are out there, including Rocks & Minerals magazine (offers a wide variety of topics at different levels, though primarily directed towards mineral specimens), Rock & Gem magazine (suited more for those interested in lapidary hobbies), the Mineralogical Record (specializes in mineral specimens) and the Lapidary Journal Jewelry Artist (specializes in lapidary and jewelry).  Magazines are a great way to keep your rockhound regularly inspired by new information.

 

4. Technology

As we move into increasingly advanced times, technology is one of the greatest tools we have accessible.  Just because your rockhound is concerned with ancient, dirty rocks doesn’t mean they can’t be aided by technology!

The Dino-Lite Digital Microscope

The Dino-Lite Digital Microscope - for looking at small things.

The Dino-Lite Digital Microscope – for looking at small things.

The Dino-Lite Digital Microscope offers a series of microscope options, from handheld USB models to eye-pieces designed to convert traditional microscopes.  These tools allow your rockhound to examine the small things!  Microcrystals to wood grains in petrified wood, this is a tool that has a wide variety of applications that will allow your rockhound to nerd out at the highest of magnifications.

The Ultrasonic Cleaner

The Ultrasonic Cleaner - reduce the wear and tear on your household supply of toothbrushes!

The Ultrasonic Cleaner – reduce the wear and tear on your household supply of toothbrushes!

Ultrasonic cleaners are a device used to submerge an object in liquid, which is then vibrated with high-frequency sound waves.  These waves act to scrub the object of grimes, and hit all the surfaces of an object including pores and cavities.  Ultrasonic cleaners are often used for cleaning machining parts or jewelry, but they also work wonders on rocks!  Take away the burden of hours of tedious scrubbing by investing in one of these machines!  (Disclaimer: do not put your water soluble minerals in here unless you want them so clean that they’ve disappeared entirely.)

 

Handheld GPS Units

GPS Devices - help your rockhound know where they are and where they're going!

Handheld GPS Units – help your rockhound know where they are and where they’re going!

For those of you who have a rockhound who loves being out in the field, one of the greatest resources you can give them is GPS!  Handheld GPS devices can be used to navigate to a new digging spot, or mark an existing one for easy navigation later!  Many GPS units feature topographic maps and land status maps, which give your rockhound even more information about where they are and what they can and cannot do while they’re there.

 

Rock Trimmers

Rock Trimmers - for precision splitting of rocks!

Rock Trimmers – for precision splitting of rocks!

Rock trimmers are perfect for the rockhound who carries home boulders for a small vug of crystals on one side.  These tools can be tricky to find, but a variety of models are available – from small and simple, hand-crank units, to large, hydraulic-powered units.  All rock trimmers work off the same concept: a rock is placed between two chisel-tipped points and pressure is used to pinch the rock and split it.  This method of splitting is not without risk to specimens (sometimes it is going to split where you don’t want it to), but it offers far more control over beating on your rock with a hammer and results in a more natural finish to a specimen than a saw cut.  These units can also be adapted to be used in the field, which saves your rockhound the trouble of lugging that boulder home in the first place.

 

Bonus Section: Stocking Stuffers!

They say it’s the little things that count – so here are some smaller, but very useful items you can throw into your rockhound’s stocking!

Headlamps

Headlamps - for hands free lighting!

Headlamps – for hands free lighting!

Headlamps are an invaluable tool – whether your rockhound is out in the field or trying to organize a dimly lit garage, lighting is always helpful!  Headlamps allow your rockhound to have their hands free while still providing plenty of light.  These are available in many different brightnesses and light modes.

Chisels

Chisels - necessary, but always disappearing...

Chisels – necessary, but always disappearing…

Chisels are another indispensable tool for your rockhound.  Chances are they have some – chances are that they’ve also lost some!  These are easy to misplace, but the good news is they’re easy to replace too!  Be sure that you are looking at “cold chisels” when shopping for your rockhound – wood chisels, etc., are not the right tool.  Chisels come in a variety of sizes and lengths, and every one of them is necessary for a different situation!

 

There are an abundance of great gifts for your rockhound – please drop us a note if you’ve got an idea that we missed!

Smoky Quartz Crystal Digging- Moat Mountain, White Mountain Nat’l Forest, New Hampshire

Scepter Smoky Quartz from New Hampshire

Welcome to Moat Mountain! Here is beautiful example of the typical smoky quartz and microcline combo found at this locality.

For more info and directions, Nat’l Forest Service page: https://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5382896.pdf

Background:
The iconic New Hampshire locality, Moat Mountain has been popular for its gorgeous smoky quartz and microcline specimens for decades. New Hampshire is known as “The Granite State” so it is fitting that specimens at its signature locality occur in a granite. In many ways, these specimens bear resemblance to other granitic quartz and feldspars from throughout the US, such as those from Colorado and Montana. The association of smoky quartz and feldspar is very typical in a miarolitic granite. More about how exactly these crystals form later.
One of the few if only free, open to the public dig sites in New England where pocket smoky quartz crystals can be found, this location is maintained by the National Parks Service and is accessible from mid spring to early autumn. The severe winter weather in the area makes collecting during that time impossible. Nearly the entire mountain has various mineral locations for smoky quartz, amethyst, microcline, and fluorite, but please respect where the parks service allows and doesn’t allow digging.

Geology and Minerals:
This locality occurs in miarolitic granite and these crystals are over 200 million years old. The minerals at this location formed at the contact between the Conway granite and the Moat Mountain volcanics. These volcanic rocks were part of a very active ancient volcano. As they rose and depressurized, gasses escaping from them were trapped by the surrounding Conway granite, forming the smoky quartz, microcline, and other minerals. The chemistry of the gasses was pretty simple, but enriched in fluorine which gave rise to some of the rarer, highly collectible minerals at the site.

Minerals:
Smoky Quartz: Commonly found in miarolitic pockets. Gemmy, very lustrous smoky quartzes are abundant. Usually they are an inch or less, but crystals to over a foot have been found. Some of the Moat Mountain pockets have been massive. It is still possible to find large pockets here, but it requires a lot of both work and luck.

Scepter Smoky Quartz from New Hampshire

Some fantastic examples on Mindat of smokies collected at Moat. Note the red mud on the freshly pulled piece. These gorgeous specimens are proof good finds at Moat can still be made.


Fine Smoky Quartz Crystal from the Granite of New Hampshire

Microcline: Blocky crystals of microcline provide the matrix for many smoky specimens. They represent the walls of the miarolitic cavities. Often overlooked, these microclines make fine specimens on their own. Beautiful blue green amazonite and Baveno twinned crystals have been found on occasion.

Old school specimen of smoky and amazonite from Moat Mountain

Topaz and Fluorite: The ultimate Moat Mountain specimen is a fine topaz, however this mineral is extremely rare here. When found, it is known to produce gorgeous gem quality champagne, pale blue, or colorless crystals that are sometimes slightly etched. Specimens can exceed five centimeters.
Fluorite crystals to several centimeters in diameter have been found on Moat Mountain. Also a rarity, they are quite sought after. Fluorite is a fragile, sensitive mineral so it often weathers away if it is at all present in a pocket. It occurs primarily in green, blue, and purple at this locality and can form cubic or octahedral crystals.

Directions (From Forest Service):
From West Side Road in Conway turn onto Passaconaway Road. Travel 1.2 miles and turn right onto High Street (dirt road). This road leads into the White Mountain National Forest, passing a gate at 1.4 miles. At 1.7 miles, bear left and continue 0.7 miles to the parking area at the end of the road. The Moat Mountain Mineral Collecting Site is a 0.9 mile hike from the parking area. On the Mineral Site Trail, keep right at both branches.
GPS Coordinates: • Moat Mineral Collecting Site Trailhead: 44.021700, -71.169500

Collecting Tips: There are many ways to collect this material. A popular way is to dig through loose, weathered rock paying attention for crystals and pocket sections. A hand rake and shovel are good for this. It pays to dig deep, past areas that have already been searched.
Another method is searching ledges for pockets and working the rock. Observe how plants grow, often roots will follow crystal bearing pockets and seams because they are open space easy for them to take hold in. Breaking the granite is hard work and requires a lot of hammering and chiseling. An assortment of wedges, chisels, hammers, and prybars would be a good idea to bring. Use large, flat wedges to exploit cracks in the rock.
This location is remote, so bring food, water, and bug spray especially if you plan on staying there for a while.

Finding Your Own Green Pyromorphite and Orange Wulfenite in Western Massachusetts!

Pyromorphite and wulfenite are highly sought after by collectors because they are some of the most intensely colored species in the mineral kingdom. Pyromorphite is known for its diverse hues and shapes ranging from vivid green, to yellow, to orange and from hoppered hexagon, to hexagonal prism, to semispheroid. Wulfenite almost always forms yellow to orange-red square shaped tabular crystals. When mineral collectors think of these minerals, exotic international locations pop into their heads like China, Arizona, Idaho, Namibia, Morocco, and Mexico. Little do many mineral enthusiasts in the Northeast US know, there is a wonderful site to dig these minerals in Massachusetts. It is just rarely represented in the specimen market because the crystals are smaller and less abundant than the really famous spots. Regardless of that, most collecting sites in New England don’t provide vibrantly colorful and diverse oxidized minerals like this place, and none exist where you can pan for wulfenites in the river like you can at Loudville!

Pyromorphite with Wulfenite

Beautiful combo of pyromorphite and wulfenite dug by my friend Alex Kim (@dirty_minerals on insta). Finding this piece is what inspired him to dig minerals. Check out more of his collecting adventures and amazing finds on his page!

History: The name “Loudville Lead mines” is used to refer to the many mines in a small district adjacent to the Manhan river in Northampton, Mass. Loudville is the name of a small village in the area on the Easthampton and Westhampton line that was the nearest settlement during mining activity (2). The Loudville Lead mines are some of the oldest colonial mines in the US. Discovered by Robert Dyer in the late 1670s (1), they experienced several periods of mining from the 17th through 19th century. The first phase was from discovery until the American Revolution, which halted operations. I have heard though I cannot confirm that lead from Loudville was used in Revolutionary munitions like musket and cannonballs. Ethan Allen, famous hero of the American Revolution worked Loudville in the late 1700s after giving up prospecting Mine Hill in Roxbury, CT for silver (3). This mine was worked intermittently throughout the 19th century, last in 1865.

Map of mineral deposit of Loudville Massachusetts

an early sketch of the geology of the lead ore vein at Loudville from
Richardson, Charles (1854): Northampton District. The Loudville Mine (Mining Magazine Vol. 2 pp 13-20.

Mineralogy: Pyromorphite and Wulfenite are the most sought after minerals at this location and often they are hard to see. When you find material that shows any hint of green or orange, save it and delicately clean it at home. Do not use chemicals on minerals from Loudville with the exception of quartz. Many of these minerals will react even with iron out.

Secondary, oxidized minerals like Wulfenite and Pyromorphite are extremely rare in New England. Many of the oxidized zones (called supergene zones) of metal deposits in the region were removed by glaciers leaving mostly just sulfides which generally are massive and not aesthetic at the majority of locations in the region. Finding just one pyromorphite or wulfenite crystal at a lead deposit almost anywhere else in New England is a very rare experience.

Pyromorphite with Wulfenite

Gorgeous specimens of pyromorphite collected by my friend Dustin Bartlett (@themodernnaturalist on instagra,) Dustin has collected Loudville extensively and his page is a good place to go to see what collectors are still finding there!

Lead secondary minerals such as cerussite, anglesite, and the rare leadhillite are also found at Loudville. Cerussite is expecially common and overlooked. The best way to spot it is by its high luster and understanding its unique crystallography. Frequently it exhibits twinning. Even though it is colorless, its appearance makes it immediately distinguishable from quartz and baryte- the two other colorless minerals here. The author has collected numerous fine cerussites at Loudville to nearly 2cm long.

Quartz is another very common mineral at Loudville that can be very pretty. Beautiful clusters of milky, smoky, amethystine, and combos of these three varieties of quartz can be found, crystals getting quite large! Many of the similar lead mines in the Northeast such as the closed to collecting Canton Lead Mine in Ct are known for colorful amethyst and smokies with lead secondaries. At Loudville, you will often find other minerals, especially pyromorphite and wulfenite coating the quartz.

Pyromorphite on Quartz

Beautiful combo of pyromorphite on dark smoky quartz dug by Dustin Bartlett @themodernnaturalist on insta

The list of minerals at Loudville is extremely extensive and represents so many interesting combinations of lead, zinc, copper, sulfate, carbonate, silicate, etc. Under the microscope, a whole world of collectible material becomes available. Please see Mindat if you want to learn more: https://www.mindat.org/loc-3832.html

Directions and Equipment:

When digging here, please respect the boundaries to the collecting area! There has been a lot of digging outside of it and if it continues, the site may be closed within the next few years. Saying that, there are many strategies to collecting there, I will discuss two of them.

The first strategy involves digging into the dump and breaking rock to expose vugs. Use a shovel, hand rake, etc to turn over the dump and a crack hammer and chisel to break the material. The river is a convenient source of water to wash pieces off you can’t see clearly. Often the mud can obscure the crystals. Move slow and be careful.

An especially interesting technique people have been successful with here is panning for wulfenite in the river using a gold pan. Wulfenite is very dense compared to other minerals and will readily separate out in your concentrate. Use tweezers to pluck them out and I strongly advise you put them into a vial of water since they are fragile and very easy to lose.

In addition to the tools I outline above, other things you will want to bring is food, water, bug spray (it gets bad in the summer), sunscreen, and waterproof footware. This is a great place to bring dogs as many of them love swimming in the river. Just keep them on leash and be respectful to other dog owners.

To get to the site, it is very simple. Navigate to the pin on the embedded map and look for a small parking area. Park there and make your way down to the edge of the river. The collecting areas are clearly marked.

Article By Jeremy Zolan

Sources:

https://www.mindat.org/loc-3832.html

(1) Trumbull, James R. (1898): History of Northampton Massachusetts from its Settlement in 1654, Gazette Printing Company, Northampton Massachusetts: 358-368.

(2) Robinson, G.R. Jr., and Woodruff, L.G. (1988): Characteristics of Base-metal and Barite Vein Deposits associated with Rift Basins, with Examples from some Early Mesozoic Basins of Eastern North America, in Studies of Early Mesozoic Basins of the Eastern US, Frolich, T.J. and Robinson, G.R. Jr., Editors, USGS Bulletin 1776: 377-390.

(3) Hall, Henry (1895). Ethan Allen: the Robin Hood of Vermont, Appleton and Company, New York.

Pecos Valley Diamonds: the Desert is Paved with Diamonds

Pecos Valley Diamond in situ

Pecos Valley Diamonds, also called Pecos Diamonds, have been collected by New Mexico rockhounds and mineral collectors for well over one hundred years.

Like many other colloquial mineral monikers (another well-known example is “Herkimer diamonds”), these “diamonds” are not diamonds at all, but quartz crystals. The glint of reflected sunlight off the faces of these quartz crystals can give the barren desert the appearance of being “paved with diamonds” (Albright and Bauer 1955).

 

Article and Photos by Phil Simmons and Erin Delventhal at Enchanted Minerals LLC – enchantedmineralsLLC@gmail.com

Outcrops of Pecos Valley Diamonds are often densely concentrated. Each "pebble" in this image is a quartz crystal, most measuring ~1-2cm. Many crystals are broken. Field of view is approximately 1 meter.

Outcrops of Pecos Valley Diamonds are often densely concentrated. Each “pebble” in this image is a quartz crystal, most measuring ~1-2cm. Many crystals are broken. Field of view is approximately 1 meter.  ©Enchanted Minerals LLC

 

Pecos Valley Diamonds are found in the southeastern region of New Mexico, exposed in dispersed outcrops that span 100 miles long by as much as 25 miles wide. Though the area where outcrops are found is expansive, Pecos Valley Diamonds are limited to a very specific geologic unit: the Seven Rivers Formation, a back-reef segment of the Guadalupe reef sequence. The crystals are authigenic, meaning they have formed in place with no transportation via water or wind, though they often have weathered out of the much softer massive gypsum host rock. Though authigenic quartz crystals are known in ancient shallow marine carbonate and evaporite series across the world, Pecos Valley Diamonds are of note for their variety of colors and forms and for their impressive size (up to ~12cm, though more often ~2-3cm) for this type of deposit.

 

Surface outcrops of the Seven Rivers Formation (highlighted in yellow) in Southeastern New Mexico. Modified from Albright and Lueth 2003.

Surface outcrops of the Seven Rivers Formation (highlighted in yellow) in Southeastern New Mexico. Modified from Albright and Lueth 2003.  ©Enchanted Minerals LLC

 

 

Habits and Variations of Crystals

One of the most appealing aspects of Pecos Valley Diamonds is the immense variety. They occur as doubly terminated crystals (less often in radial groupings) in a multitude of colors ranging from reds, oranges, and yellows, to whites, blacks, browns, and sometimes even hues of purples, pinks, and greens, and a variety of habits including prismatic, quartzoid, pseudocubic, and pseudotrigonal.

Coloration

 

A grouping of Pecos Valley Diamonds showing some of the range of coloration in the quartz crystals. Center crystal is 2.5cm.

A grouping of Pecos Valley Diamonds showing some of the range of coloration in the quartz crystals. Center crystal is 2.5cm.  ©Enchanted Minerals LLC

 

The wide variety of colors in Pecos Valley Diamonds has not yet been fully explored. Observational evidence indicates the coloration is largely due to inclusions: Pecos Valley Diamonds found still embedded in the host rock take on the color of the gypsum, even to the point of preserving the color banding found along laminations or fracture joints (Tarr and Lonsdale 1929).

 

Crystals displaying color variations within individual crystals. Top crystal is 3.5cm.

Crystals displaying color variations within individual crystals. Top crystal is 3.5cm.  ©Enchanted Minerals LLC

 

The geological setting (see Geology below) of these crystals allows for the transition between gypsum and anhydrite, and zonal inclusions of anhydrite rather than gypsum have been reported (Nissenbaum 1967). However, the exact nature of those inclusions is still somewhat enigmatic: early reports refer to “ferruginous” (iron-rich) quartz or hematite inclusions in quartz, but analysis of similar quartz crystals from Spain indicate the red coloration is due to clay inclusions rather than hematite (Gil Marco 2013). Nearby occurrences of aragonite crystals also show coloration determined by inclusions of clay. Additionally, some coloration is suspected to be related to hydrocarbon inclusions (Albright and Lueth 2003). Of further interest, many of the quartz crystals are fluorescent, though the source of that phenomenon has not been explored.

 

A Pecos Valley Diamond embedded in the host rock of massive gypsum. These crystals appear to take the color of the surrounding gypsum, though the crystals tend to universally be darker. Specimen is 15.2cm across; crystal length is 3.4cm.

A Pecos Valley Diamond embedded in the host rock of massive gypsum. These crystals appear to take the color of the surrounding gypsum, though the crystals tend to universally be darker. Specimen is 15.2cm across; crystal length is 3.4cm.  ©Enchanted Minerals LLC

 

 

Prismatic Habits

An example of a fairly "typical" Pecos Valley Diamond - a doubly terminated prismatic crystal. The red coloration is also fairly common. Crystal is 5.9cm.

An example of a fairly “typical” Pecos Valley Diamond – a doubly terminated prismatic crystal. The red coloration is also fairly common. Crystal is 5.9cm.  ©Enchanted Minerals LLC

 

The predominant habit found is single doubly terminated prismatic crystals with the regular m prism topped by hexagonal pyramids of equal or near equal r and z rhombs. This habit of quartz is common all over the world, although the majority of crystals worldwide are not doubly terminated. This habit tends to have the most color variations of Pecos Valley Diamonds. Elongated crystals are more rare than short, stubby crystals, though they can be found in several known locations.

 

Elongated prismatic crystals are unusual in Pecos Valley Diamonds. Longest crystal is 5.5cm.

Elongated prismatic crystals are unusual in Pecos Valley Diamonds. Longest crystal is 5.5cm.  ©Enchanted Minerals LLC

 

Equant Habits

Though Pecos Valley Diamonds are most often found as prismatic crystals, the variety of equant (length, width, and depth are roughly equal) habits of quartz are of particular note.

 

Crystal diagrams of equant forms found in Pecos Diamonds. Modified from Albright and Lueth 2003.

Crystal diagrams of equant forms found in Pecos Diamonds. Modified from Albright and Lueth 2003.  ©Enchanted Minerals LLC

 

Crystals that display equal or near equal r and z rhombs, but significantly lacking m faces display a quartzoid, or Cumberland, habit. This habit is often erroneously referred to as beta-quartz, which is a high-temperature polymorph of SiO2 that is unstable at room temperatures. The presence of this habit in the low-temperature environments of Pecos Valley Diamonds indicates that the quartzoid habit is not tied exclusively to high temperature deposition.

Two unusual equant habits in worldwide deposits are relatively common in Pecos Valley Diamonds: the pseudocubic habit and the trigonal habit. Both are described by dominant development of r-faces with minimal z-faces and next to no presence of mfaces, though the latter two forms are never completely absent. The pseudocube and the trigon can be differentiated crystallographically by the orientation of z-faces: the pseudocube features alternating r– and z– faces across the a-axis, while the trigonal form shows r– and z– faces mirrored across the a-axis (see crystal diagrams above).

 

Comparison of equant forms with the left-hand side viewing the crystals down the c-axis and the right-hand side viewing roughly perpendicular to the c-axis. Top: quartzoid (Cumberland) habit; Middle: pseudocubic habit; Bottom: trigonal habit. Largest crystal is 2.1cm.

Comparison of equant forms with the left-hand side viewing the crystals down the c-axis and the right-hand side viewing roughly perpendicular to the c-axis. Top: quartzoid (Cumberland) habit; Middle: pseudocubic habit; Bottom: trigonal habit. Largest crystal is 2.1cm.  ©Enchanted Minerals LLC

 

Pecos Valley Diamond pseudocubic crystals are of particular note: while the pseudocubic habit is very unusual worldwide, Pecos Valley Diamonds boast an unusually high percentage of crystals in this habit and crystals can reach sizes in excess of 5cm. Given the tendency for crystals to be fully formed and doubly terminated, coupled with availability, it can be argued that Pecos Valley Diamonds are the world’s best source for pseudocubic quartz.

 

Various orientations of the pseudocubic form in Pecos Valley Diamonds. Left-hand crystal is 2.5cm; largest crystal in center grouping is 2.7cm; right-hand crystal is 1.5cm.

Various orientations of the pseudocubic form in Pecos Valley Diamonds. Left-hand crystal is 2.5cm; largest crystal in center grouping is 2.7cm; right-hand crystal is 1.5cm.  ©Enchanted Minerals LLC

 

Other Features

Pecos Diamonds often display different lusters on different quartz faces. This is typically found in lustrous terminations (r– and z– faces) and dulled, or pitted, m-faces. Luster can also vary between r– and z– faces, creating alternating finishes on terminations.

 

Two prismatic crystals displaying lustrous terminations (r- and z-faces) and dulled, or pitted, m-faces. Left-hand crystal is 3.0cm.

Two prismatic crystals displaying lustrous terminations (r- and z-faces) and dulled, or pitted, m-faces. Left-hand crystal is 3.0cm.  ©Enchanted Minerals LLC

 

Somewhat similarly, some Pecos Valley Diamonds are found with differing degrees of quality of quartz within the same specimen: very crudely crystalline “knobs” give way to well-formed and lustrous crystals. These are currently poorly understood and more research into the relationship between the crude crystals and their well-formed counterparts is needed.

 

Examples of Pecos Valley Diamonds displaying both crudely crystalline "knobs" and well-formed, lustrous crystals. Clockwise from top left: crystal is 5.1cm; terminated crystal is 4.6 tall; crude crystal is 7.2cm across; crude crystal is 7.6cm across; right-hand crystal is 4.7cm.

Examples of Pecos Valley Diamonds displaying both crudely crystalline “knobs” and well-formed, lustrous crystals. Clockwise from top left: crystal is 5.1cm; terminated crystal is 4.6 tall; crude crystal is 7.2cm across; crude crystal is 7.6cm across; right-hand crystal is 4.7cm.  ©Enchanted Minerals LLC

 

 

Groupings

Though Pecos Valley Diamonds are predominantly found as single crystals, crystal groupings can also be found. The dominant arrangement of multiple crystals is in a radial orientation, often with one central crystal oriented perpendicular to the rest.

 

Radially oriented grouping of crystals; specimen shown front and back. Crystal is 3.8cm across.

Radially oriented grouping of crystals; specimen shown front and back. Crystal is 3.8cm across.  ©Enchanted Minerals LLC

 

Previous reports (Albright and Lueth 2003) have indicated the presence of Japan law twinned Pecos Valley Diamonds, though it is the opinion of the authors that further examination is needed to determine whether these geometries are truly Japan Law twins. There are a number of other unusual relationships between multiple crystals that are also worth further investigation, including crystal pairs that show indications of potential relationships along the c-axis.

 

Unusual geometries in groupings of multiple crystals. Top left crystal is 3.1cm; top right crystal is 2.6; bottom right crystal is 3.1cm.

Unusual geometries in groupings of multiple crystals. Top left crystal is 3.1cm; top right crystal is 2.6; bottom right crystal is 3.1cm.  ©Enchanted Minerals LLC

 

For more information on the History and Geology of Pecos Valley Diamonds, see the full-length article from Enchanted Minerals LLC: Pecos Valley Diamonds: the Desert is Paved with Diamonds.

 

Where to Go!

As mentioned earlier, outcrops of Pecos Valley Diamonds are prevalent throughout the Seven Rivers Formation – this means that anywhere in the yellow area below is prime territory to find them.

 

Surface outcrops of the Seven Rivers Formation (highlighted in yellow) in Southeastern New Mexico. Modified from Albright and Lueth 2003.

Surface outcrops of the Seven Rivers Formation (highlighted in yellow) in Southeastern New Mexico. Modified from Albright and Lueth 2003.

 

We’ll give you directions to a few  of our favorite spots, but we encourage you to take some time to explore on your own!  You never know what you might find – though please  be sure to check land status of where you’re at and obtain proper permissions.

BLM land is fair game for surface collecting, but private land is not.  Many cattle ranches operate in this part of New Mexico – many times you can simply ask permission and you’ll be good to go.  Many oil and gas operations are also active in this area – surface collecting is legal around these operations, but be respectful of equipment (re: do not touch it), and also be very aware of any signs or warnings posted indicating the presence of H2S gas – it can and WILL kill you.  In short: be smart and be safe while you’re out!

 

Location 1: East of Artesia (click for map)

Location 1 features small to medium dark red crystals – mainly equant crystals, sometimes pseudocubic!

Location 2: East of Roswell (click for map)

Location 2 features druzy crystals ranging from light to dark red.

Location 3: Acme – northwest of Roswell (click for map)

Location 3 is the site of the first professional paper published on Pecos Valley Diamonds (Tarr, 1929) – crystals are white to pink and usually do not exceed more than 2 cm in length, but this is a fun spot for the history!

 

Other things you need to know:

The southern region of New Mexico is barren desert.  There’s usually not a tree, and if there is, it’s probably a short and stubby one.  If you are going to this area during the summer, be sure to be prepared for the heat: pack lots of water, bring sunscreen, etc.  Surface collecting without shade in July can be pretty miserable even with all these preparations, so we  recommend that you take this trip in the spring or fall.  Winter is also an option, but just as the desert is prone to extreme heat in the summer, it has a tendency to be bitterly cold in the winter.  New Mexico in the spring time is also known for wind – this is an unpleasant thing when your face is inches from the ground and you can’t see anything except the sand grains in your eyes.  There’s not much to be done about the wind, but be aware that it is a possibility.

 

Other things to do in the area:

If you’re making this trip, there are some other really fantastic things in the area worth checking out.  Schedule some of these into your trip, or keep these as a backup option if the weather is poor for collecting.

Number 1 for us on this list is Carlsbad Caverns National Park – this is arguably New Mexico’s pride and joy, and is around 2 hours from Roswell, New Mexico.  This National Park protects hundreds of miles of natural cavern systems, including it’s namesake Carlsbad Cavern.   There are many things to do while in this park: walking trails, cave tours, historical stops, etc., but we absolutely recommend that you try to make it for one of the Bat Flight Programs that are held from late May through October – this experience is absolutely magical.

Rock of Ages in the Big Room, c. 1941; photo by Ansel Adams

Rock of Ages in the Big Room, c. 1941; photo by Ansel Adams

Number 2: you’re near Roswell, New Mexico.  You know what that means.  Make a stop at the International UFO Museum and Research Center to explore your alien curiosity or grab some great knickknacks featuring little green men.

There are some other museums and parks in the Roswell area worth considering, including art museums, an aviation museum, and a number of wildlife refuges and bird sanctuaries.  Check out some of the options here: Roswell Area Attractions.  If you’re up for going out a little further, also consider: Carlsbad Area Attractions, and if you’re up for a real jaunt, consider White Sands National Monument and the White Sands Missile Range Museum.

 

Collecting Tourmaline at the Himalaya Mine, California

Tourmaline - 5.7cm - photograph from Rob Lavinsky, iRocks.com

The Himalaya Mine is a location that rock and mineral collectors dream of: rich mineralization featuring gem minerals in stunning color!  The extraordinary minerals that come from this mine have made it world famous – lucky for you, the mine offers a pay dig site where you can keep all you find!

Before we get to the pictures of pretty minerals, let’s talk a little about the history of the Himalaya Mine!  (If you really can’t handle this part, you could scroll past, but you’d be missing out on some cool stuff!)  The Himalaya Mine was officially located in 1898, though early reports indicate that local Indigenous Peoples knew of the gem crystals.  Legend has it that white settlers located the mine after noticing Indigenous children playing with tourmaline crystals!

Gail Lewis was the original claim holder on the mine, though only held the property for four years.  In 1902, J.L. Tannenbaum, an employee of Tiffany & Company and a very controversial man, acquired the property through claim jumping.  Keep in mind, this is the original usage of the term “claim jumping,” meaning Tannenbaum filed another claim over the top of Lewis’ existing claim.  Much legal to-do ensued over this, but Tannenbaum retained the property.  The mine was then operated by Tannenbaum with J. Goodman Braye as mine superintendent.  Braye is a very interesting figure in mining history, as his position as superintendent was one of significant power and respect and he also happened to be an African American in the early 1900s.

First workings on the Himalaya Mine

Original caption: “First workings on the Himalaya mine at Mesa Grande, which was later to become one of the greatest tourmaline producers in the world. Left to right: Heighway, who filed on the Himalaya for Tannenbaum of New York; Vance Angel (center above) who was foreman 1900 – 1912; J. Goodman Bray, Jr., colored protege of Tannenbaum who was in charge of the Himalaya; Lohrer, first foreman of the mine; La Chapa, Indian worker. Photo courtesy Vance Angel, Mesa Grande.”  Reprinted from the bimonthly magazine Calico Print, Vol. IX, No. 4, July 1953, 40pp. The Calico Press, Twentynine Palms, California.

In the following ten years, reports indicate that 6 tons of tourmaline were shipped for use as lapidary material out of an estimated production of 110 tons produced by the Himalaya Mine and neighboring mines.  This would equal value at the time of more than $750,000!  By 1904, the surface workings were mined out and work had moved underground.

One of the principal demands for tourmaline was overseas in the Chinese market, where pink and red gemstones were highly prized by the Dowager Empress.  This drove a highly speculative market until the overthrow of the Chinese aristocracy in 1911.  The downfall of the Chinese aristocracy caused the tourmaline market to crash and ended the early production period at the Himalaya Mine.

Pink Tourmaline snuff bottles – 19th century – Qing Dynasty – photograph from Christie’s Auction House.

Sporadic small scale mining operations continued between 1913 and the early 1950s.  In 1957, Ralph Potter began another attempt at systematic mining at the Himalaya, including rehabilitating several older underground workings and driving several new tunnels.  Potter operated the mine for several years, but a collapse of the main tunnel in the winter of 1968-1969 ended underground mining.

In 1977, Bill Larson of Pala Properties International leased the property, later purchasing it in 1988.  This period saw extensive tunneling and underground expansion, and produced a relatively consistent stream of minerals in comparison to earlier projects.

The Himalaya Mine is now operated by High Desert Gems & Minerals, who also facilitate the pay dig site.

Over its life, the Himalaya Mine has produced an estimated 250 thousand pounds of tourmaline and mineral specimens.  In its most active 15 years, it produced more tourmaline than any other tourmaline mine in the world, including 5.5 tons in 1904 alone (the most tourmaline ever produced in a year).

For more on the history of the Himalaya Mine, see:

Fisher, J., Foord, E. E. and Bricker, G. A. (1999), The geology, mineralogy, and history of the Himalaya mine, Mesa Grande, San Diego County, California. California Geology 52(1): 3-18.

Jacobson, Mark Ivan (September 2010): Lippman Tannenbaum: President of the Himalaya Mining Co. and a Difficult Person, Mineral News, Vol. 26, No. 9.

Jacobson, Mark Ivan (January 2017): The Early History of the Himalaya Pegmatite Mine – San Diego County, California, Mineral News, Vol. 33, No. 1.


So, what you really want to know: what can you find?!

Tourmaline – Elbaite:

Tourmaline, Lepidolite, and Quartz - 14 cm across - photograph from Rob Lavinsky, iRocks.com

Tourmaline, Lepidolite, and Quartz – 14 cm across – photograph from Rob Lavinsky, iRocks.com.

The Himalaya Mine’s most notable mineral is tourmaline, a complex hexagonal boron-aluminum-silicate mineral group.  Most tourmaline from the Himalaya Mine is the species elbaite.  The tourmalines can range in color from black to vivid pink to apple green, and some crystals even feature multiple colors!  Blue tourmaline is also present, but is rarely found.

Approximately 5% of tourmaline from the Himalaya Mine are gemmy, meaning they have the high translucency that allows them to be faceted into glassy gem stones.

Elbaite - a gemmy crystal showing greens and pinks - 3.9cm tall - photograph from Rob Lavinsky, iRocks.com

Elbaite – a gemmy crystal showing greens and pinks – 3.9cm tall – photograph from Rob Lavinsky, iRocks.com.


Lepidolite:

Lepidolite on Hambergite - 4.5cm tall - photograph from Rob Lavinsky, iRocks.com

Lepidolite on Hambergite – 4.5cm tall – photograph from Rob Lavinsky, iRocks.com.

Lepidolite is a series of the mica group minerals.  Lepidolite is rich in lithium, though the pink to red color of lepidolite is usually attributed to manganese content.  Because lepidolite is a mica group mineral, it is often very flaky, but some material can be used in lapidary work.


Quartz:

Quartz on Microcline - 7.8cm - photograph from Rob Lavinsky, iRocks.com

Quartz on Microcline – 7.8cm – photograph from Rob Lavinsky, iRocks.com.

Since the Himalaya Mine is a pegmatite mine, quartz is common throughout the deposit.  It can occur as clear “rock crystal” quartz, milky quartz, and even smoky quartz.  Some top specimens feature tourmaline or other minerals attached to quartz in beautiful ‘combination’ specimens.

Elbaite on Quartz - 6.0 cm - photograph from Rob Lavinsky, iRocks.com

Elbaite on Quartz – 6.0 cm – photograph from Rob Lavinsky, iRocks.com.


Microcline:

Microcline (Carlsbad twin) - 6.0 cm - photograph from Rob Lavinsky, iRocks.com

Microcline (Carlsbad twin) – 6.0 cm – photograph from Rob Lavinsky, iRocks.com.

Like quartz, feldspar is an integral part of the mineralogy of the Himalaya Mine.  The most common feldspar species found is microcline.  Microcline from the Himalaya Mine is often beige to colorless, and can featured etched surfaces as well as crystallographic twinning.  Microcline is rarely gemmy from anywhere in the world, and this is also true at the Himalaya: it will likely appear as blocky opaque white-ish crystals.

Etched Microcline (twinned) with Albite and Lepidolite - 10.1 cm - photograph from Rob Lavinsky, iRocks.com

Etched Microcline (twinned) with Albite and Lepidolite – 10.1 cm – photograph from Rob Lavinsky, iRocks.com.


Albite – variety Cleavelandite:

Albite on Orthoclase with Tourmaline – 8.6cm – photograph from Rob Lavinsky, iRocks.com.

Albite is another of the feldspar species present at the Himalaya Mine.  It often occurs as the variety Cleavelandite, which occurs as thin, platy crystals.  Cleavelandite at the Himalaya Mine often occurs in beautiful rosettes of colorless to very faint blue, and can often be somewhat translucent.

Albite on Microcline with Quartz and Lepidolite - 25.0 cm - photograph from Rob Lavinsky, iRocks.com

Albite on Microcline with Quartz and Lepidolite – 25.0 cm – photograph from Rob Lavinsky, iRocks.com.


Fluorapatite:

Apatite - 2.3cm - photograph from Rob Lavinsky, iRocks.com

Apatite – 2.3cm – photograph from Rob Lavinsky, iRocks.com.

Fluorapatite from the Himalaya Mine is a uncommon, but is worth looking for!  Colors range from colorless to blue to intense pink.  Fluorapatite from the Himalaya Mine is light sensitive, so be prepared for colorless crystals on the surface and be sure to protect any colored crystals you happen to find.

Apatite on Quartz - 4.1cm - photograph from Rob Lavinsky, iRocks.com

Apatite on Quartz – 4.1cm – photograph from Rob Lavinsky, iRocks.com.


Beryl, topaz:

Beryl (etched) - 2.9cm - photograph from Rob Lavinsky, iRocks.com

Beryl (etched) – 2.9cm – photograph from Rob Lavinsky, iRocks.com.

While beryl and topaz do occur at the Himalaya Mine, they are exceedingly rare.  Keep an eye out for oddities though – you could get lucky!  Beryl can occur as etched “floater” crystals, though fully formed crystals have also been found.  Beryl colors at the Himalaya include goshenite (colorless), morganite (pink), and aquamarine (blue).  Topaz is so rare at the Himalaya that we couldn’t even find a photo to share with you!  Both beryl and topaz will likely look much like quartz, though there are physical qualities to help distinguish them – be sure to make use of the staff at the mine to help answer questions you have about your finds!

Beryl (morganite) - 11.7 cm - photograph from Rob Lavinsky

Beryl (morganite) – 11.7 cm – photograph from Rob Lavinsky, iRocks.com.


Hambergite:

Hambergite - 4.4cm - photograph from Rob Lavinsky, iRocks.com

Hambergite – 4.4cm – photograph from Rob Lavinsky, iRocks.com.

Hambergite is another relatively rare pegmatite mineral that often occurs with beryl.  Well-formed crystals of hambergite are hard to come by from anywhere in the world, but they can be found at the Himalaya Mine.  They occur as creamy white crystals, but can also range from an orange-ish tint to a salmon orange-pink.  They are sometimes opaque and sometimes gemmy, sometimes etched and sometimes sharp.  Again, if you have questions about what you are finding, ask the staff – they’ve seen a lot of this material and have a lot of knowledge to share!

Hambergite – 2.9cm – photograph from Rob Lavinsky, iRocks.com.


Stilbite:

Stilbite-Ca - 5.5cm - photograph from Rob Lavinsky, iRocks.com

Stilbite-Ca – 5.5cm – photograph from Rob Lavinsky, iRocks.com.

Stilbite occurs at the Himalaya Mine as white to cream colored crystals often found in “wheat sheaf” shaped sprays of crystals.  Stilbite is technically a super group of zeolite  (framework alumosilicate) mineral species, but that chemistry makes it even more interesting at this locality!  Stilbite rarely makes stand-alone specimens at the Himalaya (though that’s still possible!) – but look for it in combination with other minerals!

Stilbite on Tourmaline - 2.8 cm - photograph from Rob Lavinsky, iRocks.com

Stilbite on Tourmaline – 2.8 cm – photograph from Rob Lavinsky, iRocks.com.


Stibiotantalite, Columbite-(Mn), and other “ugly” minerals:

Stibiotantalite (zoned) - 1.8cm - photograph from Rob Lavinsky, iRocks.com

Stibiotantalite (zoned) – 1.8cm – photograph from Rob Lavinsky, iRocks.com.

For those of you who also love the “ugly” minerals of the world, keep an eye out for some of other pegmatite rarities: stibiotantalite and columbite-(Mn)!  These minerals will occur as black to root beer brown colored crystals, usually with a somewhat flattened shape.  Some stibiotantalites even exhibit a beautiful color zoning!  These minerals, though lacking the vivid colors of some of your other possible finds, have a fascinating chemistry (they include rare elements like tantalum and niobium!) and are fairly rare in worldwide deposits – don’t throw them away!

Stibiotantalite on Tourmaline - 6.0 cm - photograph from Rob Lavinsky, iRocks.com

Stibiotantalite on Tourmaline – 6.0 cm – photograph from Rob Lavinsky, iRocks.com.

There are a few other minerals we haven’t mentioned (mostly because they’re super rare or uninteresting or both), but you can see a complete list and more photos on mindat.org here: Himalaya Mine, Gem Hill, Mesa Grande Mining District, San Diego County, California, USA.


Dig info:

Himalaya Mine Finds! - photograph from Himalaya Tourmaline Mine

Himalaya Mine Finds! – photograph from Himalaya Tourmaline Mine.

So now that you’re ready to pack the car and go, here’s the rest of the important information you need to know!

The Himalaya Mine dig site is open year round on Thursdays through Sundays from 10am to 3pm (Monday digs can be arranged by reservation only).  The mine is located near Santa Ysabel, California and is open to the public.  Visitors can dig and screen through ore from the mine in search of pink, green, and black tourmaline, quartz, garnet, lepidolite, cleavelandite, and more!

Screening for Gems - photograph from Himalaya Tourmaline Mine

Screening for Gems – photograph from Himalaya Tourmaline Mine.

The cost for adults is $75/day, 13-15 years old is half price ($37.50/day), children 12 years and under are free with a paying adult, and additional children are $20/day.  Senior and active military discounts, rain discounts, and group rates are available.

Be prepared to go digging: it’s going to be dirty and weather is going to happen.  Be sure to bring appropriate gear (sunscreen, raincoats, shoes that can get muddy, etc.) as well as food and water.  Sorting through material can be made easier with toothbrushes and rubber gloves.  Don’t forget baggies/buckets and wrapping material for your finds!

How to Get There:

LISTEN UP, FOLKS!  Do NOT use Google Maps or Map Quest to take you to the “Himalaya Mine” – this will NOT take you to the right location and you will end up LOST!

Instead, use the address Lake Henshaw 26439 Hwy 76, Santa Ysabel, CA 92070 to take you to Lake Henshaw Resort.  You will need to go into the store (across from the lake and in the same building as the restaurant), ask for the mine dig, and the cashier will give you a code and further directions.

Make use of the MAP provided by High Desert Gems & Minerals by clicking here.

Be sure to check out High Desert Gems & Minerals’ website for any further information on the dig: Himalaya Tourmaline Mine Dig.

Himalaya Mine Tourmaline - photograph from the Himalaya Tourmaline Mine

Himalaya Mine Tourmaline – photograph from the Himalaya Tourmaline Mine.

 

Rocks and Minerals Very First Issue! – Free PDF of this Mineral Magazine

Many years ago we came across a fun find – one of Peter Zodac’s leftover copies of Rocks and Minerals first issue published in 1926.

This magazine is now and has been for decades, a bold, colorful magazine, since 1979 under the direction of Marie Hunzing.

Back in the 1960’s it was a digest sized black and white magazine with short articles and monthly articles devoted to sand and fossils.

Here is the very first issue, purchased from Alfredo Petrov, who got it from Tony Nickischer, who got it from Peter Zodac’s house.

Rocks_and_Minerals-1926-September

It is a curious document, showing that the first issue was heavy on personal advertising, more of a catalog than a magazine.

Exploring the North Calico Mountains, Barstow California

Justin Zzyzx inspecting boulders at the Noble Prospect.

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

Click the Cover and Order your copy today!

Justin Zzyzx inspecting boulders at the Noble Prospect.

Justin Zzyzx inspecting boulders at the Noble Prospect.

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.

View looking out to Coyote Dry Lake from the un-named Nickel deposit

View looking out to Coyote Dry Lake from the un-named Nickel deposit

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.

Long fiber Wollastonite crystals on the surface of massive Wollastonite

Long fiber Wollastonite crystals on the surface 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.

Spessartine garnet masses found in conjunction with the wollastonite deposits of the North Calico Mountains

Spessartine garnet masses found in conjunction with the wollastonite deposits of the North Calico Mountains

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.”

View from on top of un-named Nickel deposit

View from on top of un-named Nickel deposit

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.

Tumbled nickel quartz from the un-named Nickel deposit

Tumbled nickel quartz from the un-named Nickel deposit

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.

Entrance to the Arsenic Mine, the Puerto Negro

Entrance to the Arsenic Mine, the Puerto Negro

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.

Rockhounds collecting Garnets at the Nobel Prospect

Rockhounds collecting Garnets at the Nobel Prospect

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.

Sliced Travertine from the large travertine outcrop in the North Calico Mountains

Sliced Travertine from the large travertine outcrop in the North Calico Mountains

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.

At the Noble Prospect, Boulders of Calcite with Crystals growing in vugs can be found.

At the Noble Prospect, Boulders of Calcite with Crystals growing in vugs can be found.

Calcite crystals plucked from the walls of the Noble Propsect.

Calcite crystals plucked from the walls of the Noble Propsect.


Rockhound Barstow (California) Book Cover

If you like this article, check out the 28 page full color field guide “Rockhound Barstow” for sale online at the following links
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Or, hey, here is the map…

Finding the Princess Pat Mine, lighting up Shadow Mountain California

Princess Pat Mine Short Wave UV Rocks

I enjoy seeing rocks light up under Short Wave Ultra Violet light, so do millions of other people in the world. It is exciting to see brilliant colors coming from, what commonly is, a not very visually stunning rock. While large exotic crystals can fluoresce, many times it is something drab and visually unappealing that shows brilliant reaction to “black light”. As the field trip leader for an active group of rock hounds, my monthly trip for February of 2017 was to the area known for brightly fluorescent rocks in the Shadow Mountains, just West of highway 395, in the high desert of Southern California.

Cars parked to go collecting in California

Every month we lead a field trip for the Mining Supplies and Rock Shop in Hesperia California, visit the shop and join us!

Princess Pat Mine Short Wave UV Rocks

This photo shows the typical rocks found at the Shadow Mountain Tungsten District under normal light and under SW UV light.

To start out my planning for this trip, I did a basic Google search for what I thought the name of the mine was, the “Princess Pat Mine”. Google brought up some pages with various bits of information, some photographs, but no real indication of where the mine was specifically located. I then turned my attention to MRDS, as talked about in Rockhounding 101, this site can give me a list of mines, pinpointed on a map, showing what has been found in the area. It was a surprise to see that while there were a dozen or more deposits for Scheelite, the highly UV reactive mineral we were after, none of the mines were called “Princess Pat”. However, looking at the Google map, I noticed the road that takes you right to the majority of the scheelite deposits was called “Princess Pat Mine Road”. In fact, you simply turn west off the 395 onto this unmarked road and go for 5 miles until you hit the collecting area. But, why was I having such a pain finding the “Princess Pat Mine”?

I broke open Pemberton’s “Minerals of California” to find an entry for the Shadow Mountain Tungsten deposits on page 337, where it states “6. In the Shadow Mountains, on the northwest flank of Silver Peak, there are a number of scheelite deposits consolidated as the Just Associates quarries. The scheelite occurs in quartz veins cutting garnet-epidote-quartz tactite.” – however, no mention of the “Princess Pat Mine” – So, could it have been that the name “Princess Pat” was older or newer than this 1983 tome of California minerals? With this, I pulled out the Murdoch and Webb version of “Minerals of California”, 1966 edition, which leaves out the Shadow Mountain tungsten mines from the entries on scheelite in San Bernardino County.

Luck would serve me up a reference to “California journal of mines and geology”, Volume 49, which featured a fantastically in depth article on ore bodies of San Bernardino County, which reads

Just Tungsten Quarries (Just Associates, Princess Pat, Shadow Mountains Mines). Location: sees. 30 and 31, T. 8 N., R. 6 W., S.B.M., on
the northwest flank of Silver Peak, Shadow Mountains, about 13 airline miles west of Helendale and 14 airline miles northwest of Adelanto.
Ownership : Just Associates, E. Richard Just and Oliver P. Adams, 726
Story Building, Los Angeles, California, own unpatented claims totaling 440 acres. The property is leased to Just Tungsten Quarries, E.
Richard Just and associates, 726 Story Building, Los Angeles, California.

The deposit, now known as the Just Tungsten Quarries, was discovered in 1937. Operations from late 1937 to early 1938 by the Shadow
Mountains Tungsten Mines and W. A. Trout and C. A. Rasmussen re-
sulted in the recovery of about 750 units of W0 3 from nearly 3000 tons
of selected ore treated in a 40-ton mill on the property. The operation
was not successful and the mill was dismantled. During the mid-1940 ‘s
lessees mined about 400 tons of ore, and during the late 1940 ‘s the
Princess Pat Mining Company leased the property but apparently produced no ore. Operations from April 1952 to mid-1952 have yielded a
few hundred tons of ore of undisclosed grade.

The scheelite occurs in quartz veins cutting garnet-epidote-quartz
tactite bodies which exist at the contact between a Mesozoic granitic
rock and Paleozoic ( ?) metamorphic rocks, mostly impure limestone and
schist. The foliated rocks strike slightly north of east and dip gently
south. Scheelite-bearing tactite also has been developed, away from the
contact, along beds in the limestone, to form thin bodies of ore separated by barren limestone beds.

The deposit was explored during 1937-38 by 1800 feet of zig-zag
trenches, 10 feet wide and 6 to 10 feet deep, excavated by a power shovel
up a moderate slope in a southwesterly direction. A 65-foot vertical shaft
was sunk near the lower end of this trench system, but no mining was
done underground.

Employed in the early prospecting was a large field-type lamp requiring a 110-volt current, and a portable gasoline-powered motor generator set. This may have been the first practical application of a lamp
of this type.

Ore is being mined from a bench cutting into a trenched area about
50 feet north of the shaft. Mining operations are carried on at night,
and the ore is sorted with the aid of ultra-violet light. Shipments have
been made to both the Jaylite and Parker custom mills in Barstow.

There you go, the “Princess Pat Mine” has the distinction of being a mine that produced no ore.

As it was, the tungsten mines produced little more than some naming confusions and quite possibly some bad debt, as the scheelite riches would never quite materialize from this deposit. Tungsten is an element that was listed by the United States Government as a strategic reserve, as most of our Tungsten comes from China, during WWII it was known that it would be scarce, so efforts were made to ensure production could be met at home. Plenty of trenches and tunnels were driven in this 140 acre unpatented claim, in the end, producing nothing more than a playground for collectors with an UV light.

Princess Pat Mine Short Wave Minerals

The mostly smooth desert road is littered with rocks that glow under SW UV light

There is often a little confusion as to what kind of Ultra-violet light one needs to get the enjoyment out of collecting UV minerals. I have used many varieties of products and I’ve found what I like and what I do not like. Obviously, a light with ample power is what one wants. Small hand held units are commonly available in 6 watt and under, which gives you a reaction when you hold the light VERY close to the specimen. However, the difference between a low wattage light and something in the 9, 18, or even, 36 watts will astonish every viewer. If you want maximum enjoyment out of UV collecting, a dual wave 18 watt light is a sound investment. Some minerals glow under Long Wave (365nm) range, but honestly, I find Long Wave to be the most limited, while Short Wave (285nm), produces amazing effects. When it comes to companies, well, some come and some go, while some are longstanding companies that I do not personally enjoy, when it comes to price vs. what you get, so, I would like to steer you in the right direction. At this time, in winter of 2017, there are no good companies to purchase a UV light from on Amazon.com. In fact, I would push you in two directions. #1, UVTools.com – They have been producing some fine lights, which come accompanied by a great informative kit. I highly recommend all the units they sell, even the sub-9 watt lights. #2, on eBay, the seller topazminer_minerals_and_fossils has been having great deals on a fine selection of high powered lights, at very reasonable prices. I would suggest viewing their offerings when looking for a great UV light.


Rockhound Barstow (California) Book Cover

If you like this article, check out the 28 page full color field guide “Rockhound Barstow” for sale online at the following links, now including the Princess Pat Mine Area, indepth!
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As part of the field trip series that I lead for the Mining Supplies and Rock Shop in Hesperia California, we took a trip out to the “Princess Pat Mine” area, or, as it should be known, the Just Associates Tungsten area, or, even still, the Shadow Mountain Tungsten area. You simply follow Princess Pat Mine road from highway 395 for 5 miles and you will find yourself facing the various prospect pits and trenches filled with cobbles and boulders of mostly white rocks that will glow readily under short wave light. You will see bright orange from the potassium rich calcite caliche, you’ll see bright green from the uranium included quartz. The bright white/blue scheelite is the real winner, appearing as belts of star-like dots in the rocky background. Rarely, one can find bright red from the wollastonite found in the area.

Cars parked to go collecting in California

We have lead field trips for various groups and organizations

Tailing pile of minerals at the Shadow Mountain Scheelite Deposit

This pile of ore rubble was waiting for us at the parking area 1/10th of a mile from the start of the major trenching. This pile of rocks glows brightly if you do not wish to go into the rocky tailings beyond.

A group of about 30 of us descended on the mine area around 5pm, getting a view of the area before the sun set, by 6pm we were ready to see some rocks glow! Many of us came equipped with various powered UV lights. Some of the inexpensive LED Longwave lights were causing the calcite to glow a slight pinkish, but that was all, while the Shortwave lights were causing the whole area to light up. Everything around the area was glowing light wild, which lead to lots of happy rockhounds and many people remarking that they could not wait to come back and bring friends to show this wonderful area to. In this lonely desert, with no lights besides the moon and the stars, one can get some amazing results with a short wave ultra-violet light!

Collecting at the Princess Pat Mine

There were plenty of trenches pushed into the mountain which make great areas to illuminate the walls in search of black light rocks

Collecting Short Wave Ultra Violet Rocks

In the dark, scanning for rocks that react to SW Ultra Violet Light is a blast!

Short Wave Light glowing Rocks

Here is a rock responding to SW UV light on the mine dump at the Princess Pat Mine/Just Associates Mine

So, go out and enjoy a day or night at the Shadow Mountain Tungsten District. There are no active claims, there is no ore of worth, it is just you and the coyotes, howling at the moon and looking down at the twinkling scheelite stars…

Rockhound Barstow – Collect Agates, Onyx, Dioptase, Celestite and more in this Mojave Desert Town

Check out the new expanded Rockhound Barstow, in full color and larger size!

UPDATED 3rd Edition Released August 2020 – Get it now direct on a PayPal link, or check it out on Amazon, eBay and Etsy





The Mojave desert is a mineralogically rich area. One small town of less than 30,000 people serves as a great jumping off point for dozens of fantastic collecting sites. Many of these locations are Southern California classics, found in field guides dating to the early 1940’s and surprisingly, still producing to this day. The Cady Mountains are an endless source of material. You can be sure that enough time spent in the loving folds of the Cady mountains will reveal some mind blowing treasures to the lapidarist.

Top Notch Agate being cut into slabs.  The Cady Mountains produce beautiful treasures you'll love working with!

Top Notch Agate being cut into slabs. The Cady Mountains produce beautiful treasures you’ll love working with!





A sampling of cabochons made from material found in the Cady and Alvord Mountains

A sampling of cabochons made from material found in the Cady and Alvord Mountains

Just a few miles outside of Barstow you hit the Calico Mountains with a vast silver district, an amazing series of borate deposits, celestite for days, tons and tons of fine selenite and ample supplies of petrified palm root just pouring out of the hills…and silver lace onyx and calcite concretions that can have celestite and quartz replaced spiders and flies inside! That is just the things you can find in a small mountain range just four miles north of highway 15!

Polished Celestite from one of the many celestite deposits found along with the Borates of the Calico Mountains

Polished Celestite from one of the many celestite deposits found along with the Borates of the Calico Mountains

Gem crystal clusters of Colemanite are found in the Calico Mountains, ready to come home with you!

Gem crystal clusters of Colemanite are found in the Calico Mountains, ready to come home with you!

Colemanite glows bright in Short Wave Ultra Violet Light, like MANY of the minerals found in the area.

Colemanite glows bright in Short Wave Ultra Violet Light, like MANY of the minerals found in the area.

One of the reasons Barstow is such a great starting point for rockhounding in this area is the prime location. Just 2 hours north-east of Los Angeles and 2 hours south-west of Las Vegas, this town has most everything you need for traveling in this area. Gas, groceries, hotels, restaurants, even the Diamond Pacific Rock Shop, attached to the Diamond Pacific Lapidary Equipment factory. Emergency services, like tire and vehicle repair can be found in Barstow so that even in the worst of conditions, there is somewhere “local” to take care of any problems. Convenience is what Barstow provides and there is no reason why that is not a good thing!


Rockhound Barstow (California) Book Cover
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Who better to write and produce this Barstow rockhound field guide than the field trip leaders, Justin and Brandy Zzyzx – locals to the area and avid rockhounds, each of the locations in Rockhounding Barstow have been visited by Justin and Brandy. Justin wrote the text and Brandy designed the maps, as you can see in the sample below.

Sample page from the Rockhound Barstow Field Guide - Lead Mountain, just a couple miles from highway 15, a great place to visit and collect colorful crystals!

Sample page from the Rockhound Barstow Field Guide – Lead Mountain, just a couple miles from highway 15, a great place to visit and collect colorful crystals!

Many of the locations have been written about before, while some of them are being published in this field guide for the very first time. One of the locations that is very exciting is the North Cady Mountain collecting, including the Top Notch claim, prospected by Bill Depue and John Pickett, of Diamond Pacific. This spot has been producing some really lovely material, bright red, golden siderite, fortification and banding of clear and lavender agate. Oh, a day collecting here just can not be beat! You are going to get directions to this very spot and over 30 more locations, just waiting for you to come visit.

Bright Red and Golden Top Notch Agate from the North Cady Mountains, featured in the Rockhound Barstow Field Guide

Bright Red and Golden Top Notch Agate from the North Cady Mountains, featured in the Rockhound Barstow Field Guide

Siderite is not a common inclusion in agates so it is a welcome site to see this material, rich with gold and red along with beautiful gel agate from the North Cady Mountains

Siderite is not a common inclusion in agates so it is a welcome site to see this material, rich with gold and red along with beautiful gel agate from the North Cady Mountains

Another interesting feature is the interactive rockhound map provided in the guide. Simply type in the website address and on your phone google maps will open up and you’ll be provided with a pinpointed map featuring all the locations in the book PLUS additional locations, each of them showing you EXACTLY where to collect. Most of the locations in the books will have cell phone service, allowing you to use the interactive google map as a guided satellite directly to the collecting location. Truly a first in terms of mineral collecting field guides!

This fun "Nickel Quartz" comes from the North Calico Mountains now printed in the pages of the Rockhounding Barstow!  Nickel Quartz, Wollastonite, Garnet, and so much more await you, with new locations added occasionally.

This fun “Nickel Quartz” comes from the North Calico Mountains Nickel Quartz, Wollastonite, Garnet, and so much more await you, with new locations added occasionally.

By now I’m sure you are chomping at the bit to find out how to get your copy of this booklet. This digest sized field guide, with a color cover, color photographs of what you can expect to find, over 20 collecting locations, all this can be yours for $14.99 plus shipping and handling! That’s right, just $14.99 plus shipping gets you a fountain of information, right at your fingertips!

Simply use PayPal to order directly by Credit Card or your PayPal account or purchase a copy from Amazon, Etsy or eBay.






The abundant Gypsum/Selenite in the Calico Mountains is great for tumbling, polishing, carving and collecting.  We use it as a water softener.

The abundant Gypsum/Selenite in the Calico Mountains is great for tumbling, polishing, carving and collecting. We use it as a water softener.

The Lavic Sidling Jasper location is not just limited to the classic areas, but also spilling out to the West and North of Pisgah Crater, as you'll see in the Rockhounding Barstow Booklet

The Lavic Sidling Jasper location is not just limited to the classic areas, but also spilling out to the West and North of Pisgah Crater, as you’ll see in the Rockhounding Barstow Booklet

Chalcedony Roses are very abundant out in the Mojave Desert

Chalcedony Roses are very abundant out in the Mojave Desert





Collecting Zeolites around Marysvale, Utah

The noon sun hung in the sky with a dull yet irritating heat. It was early Spring, and I was traveling to a place nobody had any reason to be, an empty valley in Central Utah. I grabbed the canteen swaying from my hip, took a hearty swig, and wiped the small beads of sweat slowly forming on my brow. The dry earth crunched with each trod of my heel, one after another like a rhythmic drum, each thud forming a slow monotonous beat.

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I took in my surroundings. At surface level there was not much to see, canyon walls and plateaus, little wildlife, and less trees. What little vegetation was found here often amounted to sagebrush. It peppered the dirt in various shades of chartreuse, flowing lightly with the siblant hissing of the wind. I was two miles south of Marysvale, Utah, a small town with less than five hundred residents. On this particular expedition, I was alone.

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The area I was headed to was the now abandoned Elbow Ranch. On my shoulders slung a backpack stuffed lightly with supplies: a fold up shovel, a pair of gloves, a chisel, a spray bottle of water, a rag, the morning newspaper, a loupe, and a geologists hammer. I also made sure to leave some empty space for any of the various specimens I hoped to collect.

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I’d spent the earlier half of the day in the Durkee Creek area. Durkee Creek was much easier to reach than the hike to Dry Canyon had to offer. Most Rockhounds with already impressive collections probably wouldn’t have bothered spending the time there. The red-brown earth of Durkee Creek offered an abundance of zeolite, but they were often small specimens that didn’t equivocate to the effort involved.

It wasn’t until one o’clock that I found an area that had seemingly been untouched. I unfolded the shovel, wedged it between the cracked earth, and began digging. With each downward stroke I hope for the sound of metal scraping rock. It was four feet down where I found it: mordenite, an orangeish pink rock like rusted iron. With my chisel and rock hammer I chipped at the rock, a tedious process requiring delicate precision. When I’ve made enough of the outline I wedge the pick in and remove the specimen like a loose brick.

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A quick spray from the bottle and a wipe of the rag gave the rock a quick polish. The mordenite was about half a centimeter thick, forming a crust for the interior of crystalized white quartz. I held it over head where the light could reach, twisting it in hand, watching it blink and shimmer in the afternoon sun. I recall thinking a familiar thought, an image of this same area long ago. A memory strung together from vague recollections of scientific studies and my own personal imagination. It was a hostile world, fiery and volcanic, but one small pocket of that world had been preserved. A fracture of time lying dormat, imprisoned and pressurized for thousands of years, found by me after a series of seemingly coincidental happenstances.

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I tore a page from the classified section of the day’s paper and wrapped the mordenite with care, then I climbed my way out of the hole. The sun stood due west, glaring. My wrist watch read 4:00 pm. In Marysvale Utah many of the residents are returning from work, preparing for dinner and the days end. I grab the canteen, and wipe my brow. Then I gather my gear and continue on. I’ve yet to try my luck at the Blackbird Mine.


Gem Trails of Utah Book Cover
Gem Trails
by Various Authors

The Must Have, if nothing else than to have an IDEA about the collecting spots in your state, the gem trails books are a wealth of information at a low price. The perfect beginner guides that are refrenced by serious field collectors! Click on the book covers to view them on Amazon, or search the eBay link below.

Gem Trails on eBay

How to prepare your 4×4 for rock collecting – Rockhounding Preparedness Series

How to prepare your 4×4 for rock collecting.

Rock collecting may be a popular, family oriented activity, but how often do you think of the safety of your family first when you go off the beaten track to hunt for that one, perfect example of a billion-year-old rock? How often have you heard of people being stranded without food and water for days, just because the driver did not check his vehicle before leaving home? Don’t let this happen to you and yours! Simply follow the few easy-to-follow tips listed here to reduce the possibility of vehicle breakdowns when you could be hundreds of miles away from the nearest repair shop.

Check radiator hoses.
This might appear to be self evident, but according to the AAA, engine overheating is the leading cause of vehicle breakdowns in America. Radiator hoses must be firm to the touch, and free of oil, and even oil residue. Oil degrades the rubber of radiator hoses, which makes it imperative that oil contaminated hoses be replaced before your next trip.

Check all V-, and other drive belts.
You may think your belts are OK, but the most damage occurs when the pieces of a broken drive belt work themselves in under the other drive belts. This can cause all your belts to jump their pulleys, and because of their high rotational speed, the flying pieces can destroy the radiator, the battery, the radiator fan, and critically important wiring. When in doubt, don’t procrastinate, replace all the belts, and observe the proper tensions on all.

Check the charge rate.
The proper rate of charge on 12 V vehicles is 14.2 – 14.6 Volt. Anything above or below this value is indicative of a faulty alternator, or maybe worse, damage to wiring in places where you cannot repair it in the wilderness, so fix it now, while you can.

Check battery condition.
Don’t just look at the outside, and maybe clean off acid accumulations. A battery needs to be able to deliver specific currents at certain times, such as during starting. Have an authorized battery dealer perform a draw test, to determine the ability of the battery to deliver sufficient starting current. Also, compare the specific gravity of the electrolyte in each cell against the specs for your battery. Differences of one or two percent are normal, but differences or deviations that approach 5% are not, and you should replace the battery.

Getting Jump Started in the Desert

You don’t even want to THINK about how much it costs to get a jump start in the desert, 80 miles from nowhere.

Check the suspension.
Check the suspension and steering systems for excessive free play between related components such as ball joints, tie rod ends, steering dampers, draglinks and control arms. You may think that since the tie rod ends have been a little loose for the last two years, they are OK because they have not pulled from their sockets yet, but off-road driving places extreme loads on a vehicle, and the last thing you want to happen is to lose your steering while going down a steep, rocky hillside. Think of your family, and replace all worn components before you leave home.

Check the brake system.
Check the entire system for signs of leaks, and do NOT forget to check the slave cylinders inside the brake drums. These cylinders can lose up to 60% of their effectiveness before they even start to show signs of leaking, which means you could be driving around with less than 50% of your braking capacity. Moreover, if you had been topping the brake fluid reservoir regularly, but cannot see a leak, remove the master cylinder from the brake booster to check if the brake fluid is not leaking into the booster. If this is the case, replace the entire master cylinder because you can never be sure the rubber seal kits available today will not fail you when you need them most; such as when you are going down a steep, very narrow mountain pass, with a 1000-foot drop off, and no safety barrier.

Basic Preparedness is Essential for Rockhounding!

Better safe than sorry.
Performing basic vehicle maintenance procedures before heading into the wilderness is not a hassle: it is a vital precaution against being marooned hundreds of miles from the nearest repair facilities. It is also great way to prevent potentially fatal accidents caused by parts that failed because they should have been replaced months ago, but was not. Think of the safety of your family, if not your own, get your vehicle into great shape, and enjoy the rock hunting, which is what you go into the wilderness for, right? Only make sure that by taking care of your vehicle, you can safely make it out again!

Collecting Copper in Michigan’s Copper Country

Field Trip: Copper Country Collecting in Michigan’s Keweenaw Peninsula

By Jeremy Zolan

Difficulty Level: Easy to Moderate

Supplies Needed:
Safety Goggles
Water
Sunscreen
Insect Repellant
Crack Hammer
Chisel
Shovel
Wrapping Paper for Specimens
Bucket
Sledgehammer (optional)
Prybar (optional)
Metal Detector (optional)

Description:

The Keweenaw Peninsula of Michigan has been nationally famous for over 100 years for its history of highly productive copper mining. The local basalt is criss-crossed with many thick veins of native copper that made up the main ore of many of the mines. Solid natural masses of copper weighing hundreds of pounds were found with relative frequency at the mines. Though these pieces certainly were the most valuable ore, the best specimens from the area are clusters of well formed copper crystals. Other metallic minerals can be found with the native copper such as silver, domeykite, mohawkite, and chalcocite. Many other interesting minerals like datolite, analcime, prehnite, agate, and thomsonite are also abundant in the Keweenaw Peninsula. While all the mines of the region are closed to copper production, many are maintained as museums and fee dig sites. There are also many abandoned mines in the area that can provide good digging in the dumps but be sure to acquire permission from landowners before visiting any location on private land.

Localities:

Central Mine:
US 41
Central, MI 49950

central_mine_Michigan
Photo by Dave Maietta

Map:

The large tailings piles of the Central Mine are visible from US 41 in Central, Michigan. Many collectors have had good luck recently working this location. Occasionally, contractors remove large quantities of tailings for construction purposes and this exposes fresh material. In addition to the standard copper specimens, copper included calcite and prehnite can be found here. Silver has also been found with copper here but it is rare. A metal detector is very helpful for sorting trough dump piles like those found at the Central Mine.

central_mine_calcite
Caption: Calcite with copper inclusions. Central Mine, Central, MI 4.9 cm x 4.6 cm x 4 cm Ex. Rukin Jelks Rob Lavinsky Photo

Caption: Unusually large copper crystal. Central Mine, Central, MI. George Vaux collection at Bryn Mawr College. Scale bar is 1” long with rule at 1cm. Rock Currier Photo.central_mine_copper

Caledonia Mine:
Website: http://www.caledoniamine.com/
906-370-1131
202 Ontonagon St,
Ontonagon
Michigan 49953

The Caledonia Mine is a fee dig site that requires an advance reservation. When digging at this site, collectors are given a large pile of stockpiled copper ore and tools to go through it. Weekly collecting events on Thursdays and Saturdays are also held from the first Thursday in June to the last Saturday in August on the ore pile. Advance reservations are needed for these too. The workings of the Caledonia Mine are impressively preserved and tours are offered too. The mine tours aren’t necessarily just geared for casual guests. Many kinds of tours are offered, some with a very in depth historical or scientific focus. It is best to check the museum calendar to see if any events are happening during the time of your visit.

caledona_copper
Caption: Representative specimen of native copper from the Caledonia Mine’s recent workings. 5.6cm wide. Rob Lavinsky Photo

A.E. Seaman Mineral Museum
Website: http://www.museum.mtu.edu/
Michigan Technological University
1404 E. Sharon Avenue
Houghton, Michigan 49931-1295
E-mail: tjb@mtu.edu
Telephone: (906) 487-2572

Michigan Tech’s A.E. Seaman Mineral museum is among the finest mineralogical museums in the world. Its laboratories are also critical in performing much of the cutting edge mineral research currently being performed. During the period of most intense copper mining in Michigan, many specimens of local minerals were donated to the museum. Their collection of Michigan minerals is the finest in the world and there is a strong local emphasis on their displays.

Check out our custom search and view all the minerals from Michigan for sale on eBay. Not only will you see lots of neat stuff for sale, you’ll also get an idea of what localities are producing in the region.