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Return to the Rockhound Rambling Center. The Ventura Gem & Mineral Society, Inc. (VGMS)
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ALMOST EVERYTHING YOU NEED TO |
There seems to be much confusion about the proper way to care for and clean opals. This is a simple guide that will let you preserve your beautiful opals and keep them looking their best.
To care for Opal correctly, two of the basic physical properties of this unique and beautiful gemstone must be understood.
Precious Opal contains around 6%-10% water (sometimes higher). Opal has a hardness of 5.5 - 6.5 on the "Mohs" scale of hardness. First and foremost you must determine if your opal is a natural occurring solid, doublet or triplet. The care instructions for each can differ significantly.
When purchasing Opal, buy quality stones only from knowledgeable dealers or jewelers, preferably someone who is a cutter. The reason for purchasing from a cutter is, many jewelers don't understand Opal, and therefore cannot offer you the right care advice for a particular Opal. If you know precisely the type of Opal you have purchased, you will know how to care for it.
What can I do if my stone loses its polish or becomes scratched?
This is the main reason for recommending you buy from people who cut Opal. For example, if you get an Opal from a cutter and after prolonged periods of wear and tear your Opal may need repolishing (in most cases it can be re-polished at a reasonable price). Or alternatively, if you have damaged the opal and it needs to be "reworked", then this is the person to do it for you, or at least give you the best advice.
Can I put Opals in water?
Yes! Solid Precious Opal should be placed in a dish of clean room temperature water for at least 10 - 15 minutes, every 12 months or so.
From personal experience (gained from over 27 years of cutting, collecting and handling opals) this allows the gemstone to absorb moisture it may require therefore preventing any crazing or cracking caused by drying out (especially if the opal has been subjected to harsh or dry conditions).
Basic Care Practices:
Always remove rings when "Washing Up". Even solid Opals can be adversely affected if subjected to sudden temperature changes (such as being placed in very hot water).
It the stone is an opal doublet or triplet, it is unwise to place it in water (particularly hot water with detergent, as in washing up) for any length of time as it may effect the cement that is used to bond the stone segments together (Doublet - 2, Triplet - 3).
Don't wear OPAL when gardening. Sand or soil is abrasive and will wear the polish off the stone over time. Also there is the chance, if you are doing any sort of work that could bring the stone in contact with hard surfaces, a flick of the wrist in the wrong direction could chip it.
How do oily substances affect an opal?
It is recommended you do not place Opal near oils or oily substances, however oily hand and face creams will usually not damage Opal (except that they may "build up" around a ring and make it look unsightly).
How do I store Opals for long periods of time?
De-humidified atmospheres, (such as bank vaults and safety deposit boxes) are to be treated with caution when storing Opals for long periods, as they can extract the water content from an Opal over time, causing the Opal to crack or craze.
If Opal must be stored in these conditions, it is strongly advised to put them in a sealed plastic bag with a little water to prevent drying out.
Also it is advisable to check your Opal every 6 - 12 months to ensure it has not "dried out". Otherwise, it is generally safe to store them away, as long as the area is not overheated.
Displaying Opal:
Don't store Opal for prolonged periods of time under hot lights, as this could crack the stones if the heat builds up and is magnified (as in a showcase).
If Opal is to be displayed under these conditions it is strongly advised to place the Opal in or near a source of moisture (ie; a bowl of clean water or wet sponge).
Cleaning Opal:
Opal can be cleaned in soft detergent (washing up detergent) in lukewarm water using a cloth or soft brush. After cleaning, Opal should be rinsed in clean room temperature water.
By following these few simple rules on basic Opal care, your Opals will last forever as a source of enjoyment and natural beauty.
Author - Ron Fulmer,
Director of Processing and Sourcing,
Gemstone Services Australia Pty Ltd,
via The Tumble Rumble 7/01,
via Rocky Review Aug/Sept 2001.
Table of Contents.
Emma Mayer, Anthony and Matthew Beinar.
Having been an avid white water adventurer before children (BC), I have looked forward to the day when they could join me in this passion. Several months ago I noted an article about Sherri Griffith Expeditions out of Moab, Utah which took children as young as five (my Anthony being five). I immediately researched the company and found they had an exceptional reputation.
Our five days on the Green River during the 4h of July holiday exceeded all my expectations. The trip began in a Cessna 207 6-seater flying from a tiny airstrip flying over gorges deeper than the Grand Canyon and noted for Butch Cassidy and much other Western folklore. We landed on gravel atop a mesa and then hiked 2 hours down to the river where paddle boats, duckies, and oar boats awaited. The region is completely "red rock", similar to Sedona but so much more striking. Six families came from five states and included eleven children, eight of which were young boys, so you can imagine the energy level. We traveled ninety miles of river and camped on its banks each night. At camp we always went searching for adventure and were never disappointed. The first stop had bear prints and so we moved on to find a new spot. The next stop had authentic Indian petroglyphs. At the next my other son Matthew just happened to notice a fish fossil; we later entered it in the County Fair and earned a blue ribbon! At another stop we stumbled on a dead horse's head; I gathered the kids and set out on a bone collecting expedition. The photo displays some of our findings of both a horse and several bighorn sheep. Incidentally, Moab hosts an incredible rock store where we spent three hours exploring prior to the trip.
The tales are endless but most noteworthy was our last night after the trip was over. We drove to nearby Arches National Park to witness one of the most spectacular sunsets. We then hung around to witness a typical hot Western summer lightning storm whose "fireworks" rivaled any 4th of July. As if that wasn't enough, a full moon, which seemed to fill the enormous western sky in a great ball of yellow, presented itself and could be viewed through many of the arches. It is at those moments in nature that I feel like an intruder on the beautiful earth we live on and feel so lucky to be alive.
I have always enjoyed the camaraderie of all my rafting experiences but Moab will always hold a special place in my heart, for it was there that my sons shared my joy for the first time. Whatever your expectation for a dream filled vacation, I know Moab will never disappoint you.
Trekking Fossils in California's "Deep South"
by Jim Brace-Thompson.
When plans for a two-week fossiling adventure to Colorado became impractical, Nancy, Hannah, Alex and I opted for a scaled-down week-long trek to San Diego and the deserts to the east over the Fourth of July. We had never been fossil collecting in California's "Deep South" before, and I was also looking forward to visiting the San Diego Natural History Museum. As for Hannah and Alex, well, they wanted to visit such mundane spots as Marine World, the San Diego Zoo, and San Diego's surfing beaches. Kids just can't seem to get a sense of perspective as to what's important in a vacation.
We started out bright and early (well, maybe not so early) Saturday morning, June 30, cutting through a dramatic gap in the Santa Monicas to Malibu and heading south while hugging the coastline as much as possible, including a beautiful circuit around the Palos Verdes Peninsula. We had decided we'd take it slow and easy, not that we had much choice: half of California seemed to be heading south along with us that weekend!
We eventually made it to Stop 1: near the intersection of El Camino Real and Carmel Valley Road (the San Diego equivalent--not the one in Monterey with fossil crabs). I had read of the Pleistocene Bay Point formation (100,000-120,000 years old), reportedly richly fossiliferous with Ice Age mollusks described by paleontologist Ulysses S. Grant, IV, grandson of President Grant. The fossils were supposed to be past a drainage ditch opposite a Shell gas station. Given that my source was a 30-year-old fieldtrip guidebook, I was thrilled to find a Shell station still there! However, not only was there a Shell station, newer buildings were everywhere, with bulldozers clearing still more land. We scoured the ground and did come up with a few small Venus shells, an oyster, scallop, keyhole limpet, and snails. But given the pace of development, I think it's safe to say we may well have conducted the last field trip to a site that's soon to be a time capsule capped by concrete and tarmac. We packed away our meager finds and hopped back onto Carmel Valley Road, but headed west to the ocean this time, past the Los Penasquitos Marsh and Lagoon and on to Stop 2: Torrey Pines State Beach, where a pair of dolphins frolicking offshore greeted us with arching leaps from the waves.
Collecting is not allowed at this state reserve, so we came for the education and photo opportunities this site offers. It's vividly described in Sharp and Glazner's Geology Underfoot in Southern California, in a chapter entitled "A Migrating Shoreline: The Story in the Bluffs at Torrey Pines State Reserve." Just as we see a shoreline with a lagoon and estuary here today, so it was 45-50 million years ago, during the Eocene Epoch. At that time, the ocean was advancing across the land. As it did so, a sandy barrier island slowly moved across and over lagoonal deposits, and the sequence is written in bluffs that now rise 300 feet above the ocean.
Here, you see pages of prehistory written in bold strokes. The bottom layers (the Delmar formation) are greenish and densely filled with fossil oysters, clams, and turritella snails. As you "read" up the cliff, the greenish layers alternate with yellow layers of coarse sand. The sand layers (the Torrey sandstone) grow ever thicker until they force out the lagoonal deposits altogether. About three-fourths of the way up the bluff, you see a strikingly different deposit: red-brown sands and silts rise from a sharp line and have been fluted into badland formations. This is the Bay Point formation of Stop 1, and the contact between the Torrey sandstone and the Bay Point records a major discontinuity in the rock record. A gap of some 45 million years exists along that pencil-thin line, a period wiped clean by erosion before the deposition of the Bay Point formation during the recent Ice Ages. (It tugs at the heartstrings to think of all the fossils deposited yet eroded into dust over the course of those 45 million years!) After snapping up a roll of film, we climbed into the Explorer and made our way through a tremendous traffic jam for a night's rest in a room on San Diego's "Hotel Circle" although food poisoning from dinner made it something less than a night of rest for me.
Bright and early Sunday morning (well, maybe not so early), we enjoyed a leisurely drive to Stop 3: LaJolla. Cypress trees and a fog-shrouded shoreline crowded with harbor seals reminded us of our past life on the Monterey Peninsula. But whereas waves crash on unfossiliferous (and thereby worthless) granite in Monterey, at LaJolla they crash on dinosaur-era Cretaceous sediments of the Point Loma formation, capped by our friend, the Bay Point formation. This time, the gap between formations records a missing period in the rock record of about 75 million years. This was another site for photos only, but the view of the deposits and the stories they tell is worth the trip. The stories are nicely written up in Patrick Abbott's book The Rise & Fall of San Diego: 150 Million Years of History Recorded in Sedimentary Rocks. Abbott reveals some fascinating tidbits. For instance, although these marine deposits hold mostly clams and ammonites, rare California dinosaurs have also been found (one of only six locations in California to report dinosaur remains). The first was a vertebra found in 1967 and the second was a jaw fragment protruding from a beach cobble in 1989. Both are from hadrosaurs (duckbilled dinosaurs) that apparently had been washed to sea after death.
In addition to the geologic history, we enjoyed a bit of human history. The waves have pounded coves, arches and caves into the soft sediments. These have colorful reputations as hideaways for pirates and bootleggers. The most famous is "Sunny Jim." From inside a souvenir shop and museum at the top of the sea cliffs, you can walk down a dark, damp staircase carved through the solid rock to the ocean cave itself. It's called Sunny Jim after a 1920s cartoon character whose profile matches that of the cave entrance when viewed from the staircase.
As the sun burned away the morning fog, we headed for Stop 4: Balboa Park and its many museums. One section is devoted to the local crafts community, with potters, sculptors, etc., along with the San Diego Mineral & Gem Society museum. It's a one-room affair with mostly minerals and a gift shop of lapidary arts created by club members, along with some fossils from around the world. I had been hoping to see and gather info about fossils of San Diego but came away a bit disappointed. They had only a single, rather small case of local fossils in a dark corner. I do admit, though, that a fossil whale skull on prominent display was pretty cool! My biggest disappointment, however, was just down the sidewalk. For years, I've wanted to visit the San Diego Natural History Museum. I had read about fantastic fossils on display, including California's only armored dinosaur-an ankylosaur discovered in Carlsbad in 1987. Much to my dismay, the museum has recently undergone a major expansion. The vast bulk of the building is shut down and will remain so for 7-8 more months. All that was open was their gift shop and a special exhibit on diseases. I picked up a couple geology books at the gift shop, but we decided to pass on the diseases, especially since they were charging full admission to get a somewhat less than full museum experience.
With Stop 4 more-or-less a bust, we headed for Stop 5 posthaste: Kate Sessions Park. Jim Parish of the San Diego Mineral & Gem Society had advised me of this site during a phone conversation. It's not far west of I-5, between La Jolla and Mission Bay. Soledad Road runs along the park's western border. While the southern tip is gussied up with manicured lawns and other manifestations of a civilized park, the rest is rugged canyonland that strikes a curious pose in an area that's otherwise completely developed. Within these canyons, you spot sections of white sandstone, and after you figure out how to make your way to such an outcrop down the steep embankments, an assortment of pecten (or scallop) fossils awaits you. The fossils are beautifully preserved, with both valves intact. They've been leached a mustard yellow and are a bit delicate, so you need to wrap them carefully and coat them with a preservative once you've had a chance to clean them. One species we found is 3 inches across. In addition, we found tiny Lingula brachiopods and sea urchin spines. I scooped up samples of the sediment and have been picking out intricately patterned microfossils back home ever since. According to Parish, some of the pecten here are up to 6-inches wide and shark teeth have been found. Although I'm not certain, I believe this is the San Diego formation, a Pliocene deposit 1.5-3 million years old. This is definitely a site I'd like to return to! (Field trip, anyone?)
It got hot at the bottom of that canyon, collecting on sandstone that reflected sun into your face, so to cool off before dinner, we headed for Stop 6: Tourmaline surfing beach and more of the San Diego formation. This beach was also recommended to me by Jim Parish and is described in Abbott's The Rise & Fall of San Diego. It's another great spot to see "textbook" geological features spread out in plain view. A short walk reveals different geological epochs, a variety of sedimentary structures (angular unconformities, small faults, etc.) and a host of fossils weathering from the sandstone. The layers in the cliffs represent the Cretaceous Period and the Eocene, Pliocene, and Pleistocene Epochs. The Pliocene sediments drew us, for they hold profuse concentrations of a large fossil scallop, Patinopecten healeyi. We found the beds, but there were signs warning against climbing on the cliffs and the scallops were well embedded and delicate. I made a stab at getting a well-exposed 6-incher, but it began to crumble before I could make much progress, so I reluctantly left it. Still, we found several smaller species of pecten weathered free on the surface, as well as cream-colored shells of a large wenteltrap snail, Opalia varicostata. I also filled a bag with sediment and have found it to be rich in microfossils. We even had a bonus: for once, the kids didn't complain about being dragged to a fossil site! They frolicked in the beach, and Hannah seemed to enjoy (perhaps a bit too much?) watching young surfer dudes, commenting that this would be a nice place for her to vacation when she gets older.
The next two days, Monday and Tuesday, are a blur to me: Marine World and the San Diego Zoo. Didn't see a single fossil at either place. Enough said.
There was one saving grace to Tuesday. On the way to the hotel, we stopped in "Old Town" for dinner. Adobes and Victorian homes have been restored and turned into tourist traps that were fun to explore. You can buy homemade soap, blueberry candles, and any of 1,000 varieties of coffee in an old apothecary shop (Highlander Grog, with its hint of scotch, isn't so bad). But the best part was an overpriced rock shop (Stop 7). In addition to minerals and jewelry, it held an uncommonly large selection of fossils. Still, like I said, it was grossly overpriced, so I did more gawking than buying, although I did come away with a g-shaped ammonite from Montana. A whole courtyard of Mexican restaurants and ice cream shops blazed into life as the sun set, and that's where we had our dinner while I admired my new ammonite and Alex tried to set the table on fire.
Bright and early Wednesday morning (well, maybe not so early), we packed our bags and departed Hotel Circle not a moment too soon. Fourth-of-July traffic was already picking up on San Diego's freeways. Our plan was to head for the Anza-Borrego Desert after one quick stop at Crown Point, which juts southward into Mission Bay like a thumb. Abbott's book noted the Pleistocene Bay Point formation could be seen here at Stop 8: bluffs along Riviera Drive. Sure enough, walking the beach, where people were already claiming territory for the night's fireworks, we found rich layers including a coquina deposit made entirely of millions of tiny fossil clams. We also located a sand dollar deposit in dense, hard sandstone directly beneath the road. We didn't think the two traffic cops nearby would take kindly to our excavating directly under asphalt, so those sand dollars are still there for anyone with a sledgehammer and prybar.
After all this "urban collecting," I was chaffing to get to wide open desert spaces, and the drive there was beautifully scenic. I had expected to see a dry wasteland as soon as we got east of the city but was thrilled to find lush mountain country for a good bit of the drive through the Cleveland National Forest. We seemed to be the only folks lunatic enough to be heading east into the desert in July, so we encountered only a single delay when we found ourselves behind two buffalo being carted alongside a troop of cavalrymen in blue uniforms in a small-town Fourth-of-July parade.
Anza-Borrego Desert State Park was easy to spot from our mountain entry point on Highway 22: it was that big flat spot with heat waves shimmering below us. The mountains host bighorn sheep, but we didn't see any, most likely because they had the good sense not to be climbing about in an area where the thermometer read 105 degrees in the shade that day! The desert literally hit us in the face like a blast furnace. Along with a German couple, we found respite in Stop 9: Anza-Borrego Visitor's Center, buried underground and air conditioned. They sell a huge assortment of maps and books on desert wildlife, history, and geology, and a small museum shows life as it existed here during the Ice Ages on back to the late Miocene, along with a couple of examples of local fossils. We leaned how this is one of the most geologically active areas of California, with the desert floor representing a great block between rising mountains.
We found the only cafe in Borrego Springs open that day for lunch and settled into a new hotel, cranking up the air conditioning and taking a swim. With evening, it cooled all the way down to 95 degrees, we headed for Stop 10: Font's Point. This dramatic drop-off to the Borrego Badlands looks like a miniature version of the Grand Canyon. The rangers at the visitor's center had told us that picture-taking was best here during sunrise and sunset, and I clicked my way through yet another roll of film. The striped sediments of the fluted badlands span a period from 120,000 to 4 million years ago. The sandstones, clays, and volcanic ash hold Ice Age horses, camels, mammoths, sloths, and bears that roamed a lusher Anza-Borrego of streams and meadows. Still older sediments tell of an ancestral Colorado River, with fossils of freshwater snails and clams amid pieces of petrified driftwood. With night falling, we enjoyed dinner at a local tavern where everyone seemed to know your name, the waitress was friendly, the food delicious, and the music of a Country Western band was loud and lively.
Bright and early Thursday morning (well, maybe not so early), we awoke to the smell of sulfur in the air and decided we'd taken enough photos of fossils and were itching to collect some more of our own, so we lit out southeast across the park. We were fortunate it had clouded up overnight, and it remained cloudy through much of the day, with occasional sprinkles, which made the desert downright comfortable. We followed old stagecoach routes and kept a lookout for those bighorn sheep, which continued to elude us. (The only wildlife we were to see would be lizards, a big roadrunner, some red velvet ants, and that Country Western band from the night before.) Before leaving the park, we pulled over for another photo op at Stop 11: an overlook of the Carrizo Badlands. Similar to the Borrego Badlands, these fluted hills hold fossils from half a million to five million years old. They tell of lakes and grasslands and scattered forests that supported mastodons, llamas, horses, and tapirs, as well as a period when the Gulf of California covered this land with tropical marine reefs.
Leaving the borders of the park, we finally found ourselves in BLM territory and followed directions from S2 to Shell Canyon Road in Mitchell's Gem Trails of Southern California to locate Stop 12: Fossil Canyon (or Shell Canyon, the Coyote Mountain Fossil Beds, or Alverson Canyon, depending on the source you consult). Bergen, Clifford, and Spear's book Geology of San Diego County also provides directions to this site and fills you in on the geologic history. Briefly, this is the Imperial formation. The yellow muds and sandstones tell of a tropical to subtropical sea from late Miocene to early Pliocene epochs when the Gulf of California covered this part of our state, leaving behind 300 species of marine invertebrates: corals, cone shells, scallops, oysters, turret snails, clams, sand dollars, barnacles, and more. Some layers are "coquina ledges," made up entirely of fossil oysters in a cement-hard matrix. The Bergen book says collecting isn't allowed (and the entrance to Fossil Canyon itself is gated to prevent vehicular traffic), but officials at the BLM office assured us collecting is legal here so long as you confine your activity to surface collecting and don't dig or dislodge boulders in the canyon walls. The prohibition against manual labor suited us just fine, and we managed to come home with a nicely representative assortment of Imperial formation fossils, both from Fossil Canyon itself and from the many canyons twisting up to Fossil Canyon.
After a morning collecting at Fossil Canyon, we headed to El Centro for lunch and to check at the local BLM office to confirm the collecting status of Fossil Canyon and to ask about directions to the Imperial Valley College Museum and Yuha Wells fossil oyster beds near Ocotillo. The ranger offered us "good luck" in locating the oyster beds since he could never find them himself, and he gave directions to the museum, which he assured us would be open. We started at the museum: closed for the summer...From what I've heard, they're supposed to have a nice collection of Imperial formation and other fossils from area badlands. I've also heard a new desert museum may be in the works. Guess I'll just have to make another visit to check back on all this hearsay.
Backtracking, we made our way to I-8 and headed west to the area of Plaster City and Ocotillo. All along the freeway, we could see poles topped with blue flags. At the base of each pole was a box of bottled water. With immigration officials cracking down on illegal border crossings in the San Diego/Tijuana area, more Mexicans are making a far riskier crossing here in the inhospitable desert, where individuals have become lost and have died from heat and dehydration. When an entire extended family was found dead, a local group spearheaded this blue-flag program as a humanitarian effort to prevent such tragedies from recurring.
Following "Yuha Basin" directions in the Mitchell guidebook, we entered this austere landscape, and its dangers became evident. Our cloud cover had dissolved, and the desert was shimmering with heat waves. Although the Mitchell map made it look like a straightforward jaunt to the oyster beds, but it was anything but straightforward, just as the BLM ranger warned. Unmarked roads shoot off in all directions, and it's easy to get disoriented. Still, by some miracle, we crossed a wash, wound our way through some hills, and suddenly entered a wide open plain with low ridges stretched out before us: Stop 13. The ridges looked as if they had been sprinkled with pepper, but up close we saw the specks were actually large, 6-inch oysters. Thousands of these fossils rested atop a muddy white matrix as if the tide had just receded from the desert floor. If you tried hard enough, you could almost hear a big sucking sound of an ocean draining away, leaving these fossils high and dry. It was an amazing sight!
Amazing as it was, we didn't stay long because there are only so many oysters you can collect (except for some barnacles attached to the oysters, no other fossils were apparent) and the air was heating quickly. We decided to swing by Fossil Canyon for just a little more collecting where the diversity of fauna was greater before hitting the road back to Borrego Springs and a beckoning hotel swimming pool.
On the way back, rolling along an empty stretch of the Yuha desert, we saw a stone obelisk rising from the side of the roadway. Curious, we pulled over to read the inscribed plaque: "This is the desert. There's nothing out here. Nothing. -N. Karavasiles." I shouldn't have stopped. Our kids kept repeating this and have adopted it as their mantra. Now, whenever I so much as think of a desert trip, I hear: "But Dad, there's nothing out there. Nothing." I no longer stop to let my kids read plaques.
Bright and early Friday morning (and this time, it really was early!), it was time to wind up our week-long adventure. We cut across Anza-Borrego and up the Imperial Valley, skirting the Salton Sea and passing groves of fig trees and rich green agricultural fields that gave way in startlingly stark contrast to barren desert mountains at the sharp edge of the valley. Our final destination: Stop 14, the San Bernardino County Museum, where we parked next to a car with a bumper sticker reading "I collect, therefore I am." (Whenever Hannah and Alex remind me that "there's noting out there. Nothing." I now have a ready reply.) The museum is a major research repository of the fabulously fossil-rich California desert, so I was surprised to find so few fossils actually on display. They have the biggest bird-egg collection on the planet (immortalized in an episode of California's Gold), plus great wall displays of local minerals, but the fossil displays are disappointingly few. What was on display was interesting, such as a complete Shasta ground sloth skeleton, Jurassic dinosaur trackways from Clark Mountain (the only dino tracksite in California), and an extremely well-done display of Mule Canyon fossil insect concretions, as well as a fairly extensive display of the disputed Calico Early Man Site.
Maybe I'm just picky, but the rest of the fossil displays left something to be desired, and I itched to know what they had tucked away in their research collections rather than on display to share with the general public. It's bad enough we amateurs can't collect in half the fossil localities of San Bernardino County anymore; the least you could ask is that they display what the scientists have found! But that's just my opinion. I could be wrong. A stop in the museum gift shop set my wallet back when I found a couple specimens to add to my thumbnail mineral collection as well as a couple more books and a satellite photo of southern California that includes Bakersfield, Santa Barbara, Ventura, the Mojave, San Diego, and the deserts we had just traversed. It'll serve as a great reminder of a great trip that has left me itching to return at a time when the desert sun doesn't shine so hot. Here's an open invitation to anyone who wants to join us. After all, we collect, therefore we are!
Table of Contents.
Field Trip Hint - Carry a small squeeze bottle (Sinex or nose spray bottle) filled with water on field trips. The bottles are small and light and handy for putting a drop of water or two on specimens you are checking. Never lick rocks; some are poisonous. Some may have other kinds of residues or deposits on them. - The Leaverite News via Moroks 8-01.
Picnic Safety Warning - Never use a limb from a tree whose fruit has a pit (stone) in it such as choke cherry, peach, apricot, or cherry to roast a hot dog or marshmallow. Apricot & choke cherry release cyanide when heated thus poisoning your food and you. Use a metal coat hanger or willow limb. It's much safer. - Psuedomorph & Breccia via Moroks 8-01.
Shield That Slab Saw - A good shield for a large slab saw is a bicycle fender. It is just the right size and shape to keep lubricant flying off the blade from spraying all over the shop. - The Rockcollector via Rocky Review June/July 1999.
If you have some favorite tips or secrets and are willing to share, please send them to me. - Editor.
Table of Contents.
AUGUST 31-SEPTEMBER 1; FORT BRAGG, CA -Mendocino Coast Gem & Mineral Society, Town Hall; Main & Laurel. Hours: Fri. thru Sun. 10-6, Mon. 10-4. Don & Karen McDonell (707) 964-3116.
SEPTEMBER 29; LOS ALTOS, CA - Penninsula Gem & Mineral Society, Los Altos Rancho Shopping Center, Foothill Expressway & So. Springer Rd. Hours: 9:30 -4:45; (No Dealers). Frank Dina (650)967-3424.
SEPTEMBER 29-30, ANTIOCH, CA - Antioch Lapidary Club, Contra Costa County Fairgrounds, Tenth and "L" Streets, Antioch. Hours: 10-5 both days. David Zabaldano (925) 516-0651 davez@cctrap.com.
SEPTEMBER 29-30, DOWNEY, CA - The Delvers Gem and Mineral, Woman's Club of Downey, 9813 Paramount Blvd. Hours: Sat. 10-5, Sun. 10-4. Manfred Dexling (562) 425-0192.
SEPTEMBER 29-30, MONTEREY, CA - Carmel Valley Gem & Mineral Society, Monterey Fairgrounds, 2004 Fairgrounds Road. Hours: Sat.10-6, Sun. 10-5. Co-chairs: John Wills (831) 394-9099 jbmarsha@aol.com. Sky Paxton (831) 663-6978 paxtons@jps.net.
OCTOBER 3-7: JOSHUA TREE, CA - Sportsman's Club, Sportsman's Hall, 6225 Sunburst Avenue. Hours: Wed.-Sat. 8-5; Sun. 8-3. Gary Palmer (760) 366-3430.
OCTOBER 13-14; TRONA, CA - Searles Lake Gem & Mineral Society, 13337 Main Street. Hours: Sat. 8-5, Sun. 8-4. Bonnie Fairchild (760)372-5356. www1.iwvisp.com/tronagemclub/.
OCTOBER 13-14; TURLOCK, CA - Faceters Guild of Northern Calif., Inc. Stanislaus County Fairgrounds, 900 N. Broadway Street. Hours: Sat. 10-5, Sun. 10-4. Marion Roberts (209) 538-0197.
OCTOBER 20-21; PLACERVILLE, CA - El Dorado County Mineral & Gem, El Dorado County Fairgrounds, 100 Placerville Drive. Hours: 10-5 both days. Jackie Ceratto (530) 677-2975.
OCTOBER 20-21; ANDERSON, CA - Shasta Gem & Mineral Society of Redding, Shasta District Fairgrounds. Hours: 10-5 both days. Alex or Kelly Stoltz (530) 474-4400.
OCTOBER 20-21; SANTA ROSA, CA - Santa Rosa Mineral & Gem Society, Veteran's Memorial Auditorium, 1351 Maple Avenue. Hours: Sat 10-6, Sun. 10-5. Bonnie Wood (707)869-9385. E-mail: steekue@ap.net.
OCTOBER 20-21; WHITTIER, CA - Whittier Gem & Mineral Society, Whittier Masonic Temple, 7604 Greenleaf Ave. Hours: 10 to 5 both days. Jay Valle (626) 934-9764.
NOVEMBER 2-4; EUREKA, CA - Humbolt Gem & Mineral Society, Redwood Acres Fairgrounds, 3750 Harris Street. Hours: Fri.(kids day) 9-6, Sat. 10-6, Sun. 10-5. Mike Martin (707) 839-5422.
NOVEMBER 3-4; CONCORD, CA - Contra Mineral & Gem Society Centre Concord, 5298 Clayton Road. Hours: 10-5 daily. Sam Woolsey (925) 837-3287.
NOVEMBER 3-4; FONTANA, CA - Kaiser Rock & Gem Club, California Steel Ind., 9400 Cherry Ave. Hours 9-5 both days. JoAnn Watson (909) 355-7455. Interstate 10 to Cherry exit then North about one mile on left.
NOVEMBER 3-4; OXNARD, CA - Oxnard Gem & Mineral Society, 800 Hobson Way. Hours: Sat. 9-5, Sun 9-4."Gems for the Holidays" (Jingle Bell Rocks). Laura Grayson (805) 482-3052. Website: http://www.ogms.net, e-mail: webmaster@ogms.net.
NOVEMBER 3-4, RIDGECREST, CA - Indian Wells Gem & Mineral Society, Desert Empire Fairgrounds, Mesquite Hall, 520 S. Richmond Rd. Hours: 9-5 both days. John De Rosa (760)375-7905.
NOVEMBER 17-18; LIVERMORE, CA - Livermore Valley Lithophiles, "The Barn", Pacific Ave. at So. Livermore Avenue. Hours: Sat. 10-5, Sun. 10-4. Bill Veiriger (925) 443-5769 zyzzx@zyzzx.com.
NOVEMBER 17-18; VICTORVILLE, CA - Victorville Gem & Mineral Club, 14800 7th Street. Hours: Sat. 9-5, Sun. 9-4. Gil Gilbert (760) 868-6900.
NOVEMBER 24-25; BARSTOW, CA - Mojave Desert Gem & Mineral Society, Barstow Community Center, 841 S. Barstow Road. Hours: 10-5 both days. Bob Depue (760) 255-1030.
DECEMBER 1-2; SAN BERNARDINO, CA - Orange Belt Mineralogical Society, Corner of "E" Street & "31st" Street. Hours: Sat. 10-6, Sun. 10-5. Tony Gilham (909) 820-2122.
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2001:
NORTHWEST FEDERATION,
August 30-September 1 - Enumclaw, WA.
MIDWEST FEDERATION,
September 7-9 - Rice Lake, WI.
SOUTHEAST FEDERATION,
November 3-4 - Pascagoula, MS.
2002:
SOUTH CENTRAL FEDERATION,
February 8-9 - Tyler, TX.
CANADIAN FEDERATION CONVENTION,
May 4-5; 25th Anniversary,
Calgary, Alberta, Canada.
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Just for the record any unsigned articles are by the Editor. Thanks to all who help make the bulletin more interesting by contributing articles and information for events. It is a pleasure for me to put them in! Please don't be bashful about writing something up and sending it in, giving constructive criticism, suggestions for items you would like to have included etc. I appreciate it all. I would also like to thank my husband Jim for all his help and support (and nagging) in getting the bulletin out.
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Searles Lake Gem and Mineral Society, Inc.,
P.O. Box 966, Trona, CA 93592-0966,
Member of the California Federation of Mineralogical Societies,
On the Internet: http://www1.iwvisp.com/tronagemclub/,
E-mail to: fairchil@iwvisp.com.
Dear Mineral Collector; August 2001.
If you are on the Internet and wish to get show information by browsing our web page (www1.iwvisp.com/tronagemelub/, note: number 1 in www1) instead of through the U.S. Mail, let us know by e-mail and we will take you off our Gem-0-Rama mailing list.
Gem-0-Rama 2001 Show Announcement.
Again this year, IMC Chemicals Inc. is allowing the collection of rare Searles Lake minerals from its private lands, but only during the October 13-14 show of the Searles Lake Gem & Mineral Society. This is a once a year opportunity for mineral collectors to participate in field trips to a very large, recently deposited, saline mineral ore body. IMCC does ask that visitors remember that Searles Lake not only has rare minerals, it is also a working mine producing over 1.7 millions tons per year of inorganic chemical products.
FIELD TRIP TIMES - same as last year. Last year on the 9 a.m. Saturday mud tour, 788 people collected from gooey, black mud containing very large hanksite and borax crystals and clusters weighing up to 100 pounds. The mud minerals should be good again this year. These specimens can be washed at the site or bottles of brine are sold at the show. During the 2:30 p.m. Saturday blow hole tour to Searles Lake, collectors can watch IMCC technicians jet a well to bring tons of specimen grade hanksite, borax, sulfohalite, trona, and cubic halite onto the dry salt surface for visitors to collect. Last year this tour drew 1,065 people and is believed to be the largest mineral collecting tour in the country. The 9 a.m. Sunday brine pool tour will be to brine pools containing the beautiful naturally pink, Searles Lake halite. To collect pink halite students will need a heavy spud bar (rent at show) or a crowbar and heavy hammer, and they may get your feet wet with the salt brine. Geologists, technicians or engineers knowledgeable in Searles Lake guide each tour. Registration for all Searles Lake tours begins one hour before departure and requires a $5 donation per vehicle. The Saturday tours will be 2 1/2 hours long, and provide 2 hours at the site. There will be an option of 4 hours at the brine pool site on Sunday for an extra $5. Good collecting is possible without special equipment, but the best collecting requires sacrificial clothes, sturdy shoes (rubber boots are better), gloves, garden tools, a heavy spud bar and hammer, a pad to kneel on, and bags or trays for your "loot". If desired, all necessary tools can be purchased at the show.
The show will again provide bus tours of the chemical extraction plants of IMC Chemicals Inc. These tours have knowledgeable guides to explain the complex procedures needed to recover products. We will also provide information for self-guided tours of the Trona Pinnacles National Scenic Area (site of the new "Planet of the Apes" movie).
In addition to mineral collecting tours, a free indoor mineral show is open from 8 am to 5 pm on Saturday and 8 am to 4 pm Sunday. This includes: 20 mineral dealers, auction and counter sales of Searles Lake minerals, general store, 50 hobby and mineral displays, demonstrations of arrowhead and gemstone faceting, catered cafeteria with large eating area which will serve lunch 10-4 both days and dinner, Friday 5-8 and Saturday 5-7, free bus tours through two of IMCC's large chemical plants, and geode cutting and sales. Also open will be the Old Guest House Museum and the Trona History House with its historic caboose and fire engine. The Trona Community Church will have a pancake breakfast both mornings. And IMC Chemicals and the SLG&MS will allow supervised dry camping (RV and tent) at the Valley Wells Area five miles north of the show. For RV'ers wanting full hook-up, the Trona Trailer Park has limited spaces.
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Definition of the Month - Edited by Steve Mulqueen,
Mining Terminology:
Adit - A nearly horizontal passage from the surface by which a mine is entered.
Drift - A horizontal underground passage which parallels the general trend of a vein of ore.
Headframe - A structure built over a shaft used for the purpose of hoisting ore, waste rock, equipment, miners, etc. by means of a cable operated system.
Incline - Similar to a shaft, developed at an angle other than vertical, often parallel to the dip of a vein of ore.
Level - A horizontal passage or drift into or within a mine.
Portal - The surface entrance to a drift, tunnel or adit.
Raise - A mine shaft developed from the bottom upward.
Shaft - A vertical excavation often used for hoisting ore, waste rock, equipment, miners, etc.
Stope - An underground excavation from which ore has been extracted, above or below a level.
Tunnel - An underground passage open at both ends.
Winze - A vertical or incline opening or excavation connecting two levels in a mine.
Source: Fay, Albert H., "A Glossary of Mining and Mineral Industry",
Bulletin 95, U.S. Dept. of Interior, Bureau of Mines, 1920.
The "Definition of the Month" will feature key words which are related to geology, paleontology, mining and desert history. Anyone who wishes to submit a word and definition for the bulletin, please see me.
Steve Mulqueen.
Illustration of the Month - Edited by Steve Mulqueen,
Methods of Locating Mineral Deposits in the 16th Century.

A print from a "woodcut" engraving depicting 16th century methods of exploring for mineral deposits. The following letters can be seen in the drawing at the upper left (A) and in the middle just below the center (A and B).
A. "Twig" or divining rod method used by those gifted with such talent for the purpose of locating ore deposits.
B. "Trench" method in which an excavation is made at the site of a mineral discovery in order to determine the extent of the deposit at depth.
Source: Agricola, Georgius, "De Re Metallica", page 40. Originally printed in Latin in the year 1556. Translated in 1912 by Herbert C. Hoover and Lou H. Hoover, printed in English 1912, reprinted 1950, Dover Publications, Inc., New York.
"De Re Metallica" is a book on the development of mining methods, metallurgical processes, geology, mineralogy and mining law from the earliest times to the 16th century.
Herbert C. Hoover was educated in mining engineering at Stanford University. He became famous when he served as the 31st president of the United States from 1929 - 1933. He and his wife Lou understood the Latin language and were the first to translate the entire book into English.
The "Illustration of the Month" will feature a drawing, sketch, pen & ink rendering or an engraving print found in old books, maps and manuscripts related to geology, paleontology, mining history and / or desert history. Anyone who wishes to submit an illustration for the bulletin, please see me.
Steve Mulqueen.
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Matthew Beinar proudly displaying the blue ribbon winning fish fossil he
found on their white water adventure.

Anthony and Matthew Beinar and friends with their set of "bones" found on
their white water adventure.

One of those field trip trophy's none of us want! These remains were owned
by Kathryn Davis after one and a half days into her trip to Wyoming and
Colorado! Fortunately she was only going 10 miles an hour. But the rest of
her trip was great!

A better experience on Kathryn's vacation! This is an abandoned
Travertine mine near Canyon City, CO. A chunk of Travertine anyone?
Looks very interesting.
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