Friday, September 29 2023
Gold concentrations are spotty, even in known gold-bearing areas, so most prospectors sample and test often using a simple gold pan. They keep moving until they get good results. Once you find a spot with fairly large amounts of gravel that yields good gold, then it’s time to bring in a sluice box. A sluice is simple to operate and has been used all across the world for thousands of years. A sluice is often the first large-scale concentration device purchased by miners. The advantages include low cost, versatility over a wide range of material and water conditions, and ease of setup and use.
Proper Setup of your sluice is by far the most important aspect of gold separation and recovery. Some common mistakes too watch out for are:
Matching material classification and processing speed/volume of material to your sluice is critical to maximize gold recovery. First pan test the material you run through the sluice to provide you with both the size and quantity of gold in the material. In order to capture small gold in quantity, finer classification is usually necessary. While it takes more time, miners get the benefit of removing more material that is not gold bearing - making each bucket both more valuable and easier to run through the sluice box. Processing speed and volume of material to put in sluice (by hand or by scoop) must be matched to the volume and velocity of the water. If too much material is introduced into the flow, the water velocity will slow down and cause the sluice to back up and lose gold. It is much better to gradually add smaller amounts of material to the flow. If you are adding material into the sluice using a scoop, avoid adding material like an ice cream scoop because that disrupts the water flow. Instead, turn the scoop into the flow and gently move the scoop side-to-side while the water pulls material.
Tuesday, May 23 2023
Garrett has announced a new promotion for summer 2023 — buy the Ace 300, Ace 400, or Ace Apex metal detector and get a Pro-Pointer pinpointer for a LOW price! Big savings over purchasing the detectors and pinpointers separately! LIMITED TIME OFFER WHILE SUPPLIES LAST.... or until Garrett says it's over! ACE 300 SPECIAL - Includes an ACE 300 detector + AT PRO-POINTER for $369.95 — SAVE $27.95 compared to purchasing each item separately.
Thursday, April 13 2023
Over the years you may have tried many different types of mats, carpets, riffles, and miners moss, but Dream Mat was inspired solely to help prospectors work less to get more gold! The Dream Mat is the first sluice mat ever to be scientifically engineered and designed using advanced fluid dynamic principles and physics. The mini Hydro-Cyclone inspired vortex cells classify, separate, capture and hold gold naturally. Dream Mats vortex cells exploits natures own forces in a patented system to bring the finest gold recovery ever created. These mini cells are engineered to capture the finest of gold without needing huge amounts of water to maintain good exchange. Big gold is really heavy and Dream Mat captures and holds the bigger gold in its vortex holding cells, just like it does with fine gold. Made in the USA. US patent 9168536 B2. Mini Dream Mat is ideal for sandy areas and black sands. Great for 1/4"-3/8" screened runs. Catches the gold everyone is missing! Mini Mat is great for that hard to catch gold!
Browse Now — Dream Mats for Stream Sluices, Power Sluices, and Gold Cube. Wednesday, March 29 2023
Did you know that “bad” weather can be really GOOD for gold prospectors? Of course no one ever hopes that Mother Nature causes catastrophic loss of life and property, but the ups and downs of weather events in any gold-bearing area are something to take advantage of. Nature can help all of us in our quest for the shiny stuff— especially in light of recent atmospheric rivers causing flooding and lots of snow in California, eastern Idaho, northeast Utah, northwest Colorado, the Cacade Ranges, portions of the northern and central Rockies, and portions of Arizona and Nevada. Atmospheric rivers are large, narrow sections of the earth's atmosphere that carry moisture from the earth's tropics near the equator to the poles. On average, the earth has four to five active atmospheric rivers at any time. A vast majority of atmospheric rivers happen in the fall and winter. The northern Pacific Coast receives the bulk of activity in the fall, and the California coast receives more in the winter. Since December 2022, the U.S. West has been slammed with back-to-back-to-back atmospheric rivers. These events provide as much as half of the region’s annual precipitation, bringing much-needed water to parched lands and adding to the snowpack in the high mountains. This year’s storms have done a lot to restore the landscape drought and is “greening up” the landscape and refilling many smaller reservoirs. How does this help you get more gold? Primarily, multiple weather events cause large amounts of gold to move and replenish areas that already have been worked. And even when the atmospheric rivers die down, the higher than normal snowpack will cause water levels in rivers to flow well into the summer instead of drying up in late spring. Higher water levels extend your mining season, and allow you to run high-production equipment such as highbankers and power sluices. Miners can also work stream bank deposits once the water recedes back to normal flows. Typical winter storms that regularly occur in gold-bearing areas usually do not create enough havoc to force substantial amounts of "new" gold into movement. However, when Mother Nature really goes to work as we’ve seen lately, a great deal of gold can be set free, creating a bonanza for gold hunters. Gold veins that have been hidden for decades suddenly can be exposed. Floods can also sweep gold out of abandoned mines and wash it downriver. Known gold digs can be washed out, trees uprooted, and the landscape eroded— all pluses for prospectors! When tons of rock, cobble, and boulders are swept downstream along bedrock during a huge storm, quite a bit of destruction occurs. Plants, weeds, and trees that normally grow along the river and gravel bars are washed away. And when a major storm or flood tears up large portions of a streambed, a fair amount of this newly-released gold, because of its weight, will be deposited along the riverbed and settle into cracks and crevices (hand dredges are an ideal tool in this situation).
Friday, February 24 2023
Whether it’s mining for gold, silver, lead, zinc or other precious metals, it’s always fun to follow in the historic footsteps of the old time miners. To do exactly that and learn how copper and other ore was first mined in Bisbee, Arizona, take the underground Queen Mine tour. Outfitted with hard hat, miner’s headlamp and a neon vest, visitors ride 1,500 feet into the mine and learn about equipment, techniques, dangers and a century worth of history. Tour guides are actual retired miners, so you know you’ll get the real highlights of working underground. You’ll learn about blasting with dynamite, the role of mules, and even how miners went to the bathroom while working in the mines! Electricity changed the world from a predominantly rural society to the industrial age, and copper wire was needed to carry that electricity— and lots of it. Thanks to the insatiable demand for electricity, Bisbee was one of the greatest copper camps in the world. In nearly 100 years of continuous production (late 1880s until the mine closed in 1975), the local mines produced metals valued at $6.1 billion (at 1975 prices). This staggering amount of wealth came from the estimated production of 8,032,352,000 pounds of copper, 2,871,786 ounces of gold, 77,162,986 ounces of silver, 304,627,600 pounds of lead and 371,945,900 pounds of zinc. The story of Bisbee mining began in the late 1870s when Lt. Dunn, in charge of a cavalry detail from the frontier Army post of Fort Huachuca, was on a scouting mission against the Apache Indians. Lt. Dunn and his men camped on a spot that is now occupied by Old Bisbee, only several hundred yards from the beginning of today’s mine tour. On a walk after dinner, Lt. Dunn picked up an interesting rock. He found a few more pieces along the slope of the south wall of the canyon. Unable to do anything about it because of military duties, Dunn took a prospector by the name of George Warren into his confidence and struck up a deal by which Warren would locate claims and work the property with Dunn as a partner. But on his way to the site, prospector Warren stopped to enjoy his favorite pastime—drinking whiskey with friends. Warren soon had new partners and staked a group of claims with them, leaving Dunn completely out of the deal. Copper production began on a limited basis around 1880. At the time, those who toiled in subterranean tunnels beneath the Mule Mountains were mostly immigrant miners from Europe. Individuals and then companies with capital gradually became involved and took over individual claims and brought them into production. Phelps Dodge Corporation, through a subsidiary the Copper Queen Consolidated Mining Company, became the dominant force and eventually the sole operator of the mining district. Building on its base in Bisbee, Phelps Dodge had long been one of the largest copper producers in the United States. Although mining was closed in 1975, the Queen Mine Tour was officially opened in 1976 to keep the story of mining alive in Bisbee. Since then, millions of visitors from around the world have enjoyed the trip into the mountain on the underground mine tour train.
Tuesday, February 14 2023
There are a variety of searchcoil sizes and shapes and configurations. The correct one to use depends on the environment it will be used in as well as the targets being sought. A change in any one of these variables may require a different searchcoil. Sometimes changing the search coil on your metal detector is the next best thing to buying a whole new machine! It is possible that merely changing the coil on your detector will lead you to a host of new targets. CONFIGURATIONS Concentric Mono Imaging DD Search coils have two smaller “D” shaped coils housed inside to penetrate heavily mineralized ground that is commonly encountered while gold prospecting and relic hunting. The Double-D configuration is designed to significantly reduce ground interference and, thereby, recover the performance lost by a concentric coil over mineralized soil. With the Double-D, it is the arrangement of the TX and RX coils that produce a canceling effect of ground signals. This configuration is called DD because both TX and RX coils are in the shape of a “D”. The positive detection fi eld of the DD runs beneath the overlapping center section from front-to-back. The remaining portion of the coil actually produces negative (i.e. canceling) detection fields. It is this canceling field that allows the DD coil to maintain performance over mineralized ground. Because of its small positive detection field, the DD is inherently less sensitive than a concentric searchcoil of the same size, over non-mineralized ground. The Double-D will, however, significantly outperform the concentric coil over mineralized ground. For this reason, it is highly recommended when hunting over mineralized ground commonly found when prospecting and relic hunting.
Monday, February 13 2023
The searchcoil is a vital part of your metal detector. It generates a magnetic field and senses metallic targets in the surrounding environment. The size and depth of the magnetic field is determined by the shape and size of the searchcoil. Understanding the purposes behind the various sizes and shapes of searchcoils will empower you with the ability to choose the best coil for each application. HOW SEARCHCOILS WORK SEARCHCOIL DEPTH SEARCHCOIL SIZES
Garrett is the global leader of ground search metal detectors, pinpointers, coils, and other accessories. Browse Garrett detectors and more. Wednesday, February 08 2023
Grab your Garrett metal detector and accessories and head to Canton, Texas, April 14-16 for their Memorial Hunt! Ticket registration for the Garrett Memorial Hunt closes in less than a month, and with over $100,000 worth of prizes, you don't want to miss out. The more hunters who sign up, the more this value will increase! Tickets are limited, so be sure to secure your spot before they sell out. Sign-ups end March 1, 2023! Details: Friday, April 14, through Sunday, April 16 in conjunction with Texas Association of Metal Detecting Clubs (TAMDC). The event will be held at: First Monday (flea market grounds) 800 First Monday Lane Canton, TX 75103 Basic Hunt Package:
Plenty of Fun for All Ages!
Whether it's time to buy your first Garrett metal detector, an upgraded model, or additional coils, headphones, carry bag or other accessories, check out the selection of Garrett treasure hunting items here. Saturday, November 19 2022
If you’re used to water mining, having success in the desert might seem challenging— that is until you start thinking of desert ground as a massive sluice box. Many of the principles you’re used to when prospecting and mining in waterways, will translate into desert mining. The most important thing to remember is that water is crucial to gold movement. Unlike a running river or creek with highs and lows, desert placers are much different in that gold is moved quickly during a flash flood, leaving gold stranded as opposed to being moved further by continual water flow in a creek. During a river high-water event in a non-arid area, gold is moved over a larger area by massive water flows that continue until the water slows as the source dissipates its energy. Spring snow runoff is a good example. Rivers rise and sometimes flood based on the upstream water source. When the snow has melted, the river will slowly get back to normal. In the desert, gold is moved in the exact same way with the exception that water powerful enough to move gold does so and then just simply stops. In a flash flood, gold is moved very violently and often a very short distance, sometimes percolating into valuable pockets. Here’s where the difference between water and desert mining principles comes into play generally flood gold will concentrate in areas that do not meet the standard thought of inside bends and where the water flow becomes lower. For the most part, desert mining experts recommend staying out of the washes, gulches and dry river beds— that is unless you clearly see exposed bedrock. Gold will settle fairly quickly when it is trapped behind jagged bedrock and small fault lifts that have not been worn down over time by constant water flow. It IS true you can find areas of concentrated gold-bearing material in the washes, however, the amount of time and energy to get through feet of overburden is usually just not worth it, especially when there are higher values to be found outside of the wash. Follow the leads out of the wash to where the gold lives in higher concentration. Test and sample areas you see with a great deal of runoff from a tributary coming into the main wash. Here you are only digging through the current flood layer and testing for flood gold. Make your way out of the wash carefully looking at the bottom of the tributary and the areas where the water flowed into the tributary. Look closely for jagged bedrock and slight lifts in the ground and then prospect. Continue to test each of those spots. What started as a few specks of flood gold in the main wash can lead to larger and larger deposits on the flats or in slight inclines across the desert floor. Keep in mind that when a flash flood is dissipating, there is not enough energy to move a lot of rock, but the sand will continue to flow a bit, creating great clues. In general, cool season precipitation (October through April) is the most extensive source of rain in the desert regions. Rainfall is more widespread and of relatively long duration during the cool season. On the other hand, warm season precipitation (May through September) results largely from short monsoon-type thunderstorms. If you’re ready to head to a sunnier climate this winter, keep these tips in mind and you just might find enough similarities between water and desert mining to make you return every year. Good luck! Friday, September 30 2022
In an area either rumored or known to hold gold, where should you look first? The creek, the surrounding hills, washouts, or just where? The characteristics of the gold in that area will help you to know where to start. If the gold is flat and pounded, that indicates it’s been in the water a long time. If the gold is coarse and chunky, you know you’re getting closer to the source. When gold is smoother, stop and go back to the coarsest gold and start working upwards until you find the source.
Keep in mind that gold is gold, so there isn’t necessarily a better type of gold. Some is just easier to recover. There are only two types of gold deposits. The first type is “lode” which is simply everything that is still in the matrix and in the ground, and the other is “placer” —or everything else. Lode deposits refer to gold that is still locked within its original solid rock formation. This formation of gold generally starts as a vein in rock and is formed over millions of years. Since the gold is locked up in rock, and can be mixed with quartz, calcite, pyrite, and other minerals, lode gold usually requires specialized mining techniques to extract. Lode mining takes a lot more equipment and generally a lot more expense and is usually undertaken by large commercial operations instead of the average prospector. Placer gold is the gold that most prospectors are more familiar with. Placer gold isn’t really any different than lode gold. It is simply a concentration of that same gold that has eroded and traveled away from the vein. Since gold is very dense, it will move downhill much slower than the surrounding sediment. It tends to become concentrated on or near the surface of the lode, forming a “residual placer” close to the original bedrock exposure. Gold found downhill from the immediate outcrop above the nearest watercourse is called an “eluvial placer.” Once it reaches the nearest waterway and is transported by flowing water, the gold now is known as “alluvial placer.” The origin of the dust, flakes and nuggets found by panning and sluicing is usually from a vein up on a nearby mountain. Bench placers were originally stream placers. Benches are simply where the water used to be, maybe even millions of years ago. They are formed by erosion or geological events such as uplifts, earthquakes or plate drops that changed the stream flow. Some of the most profitable mining is performed on benches. Many benches are highly concentrated by the alluvial deposits that still feed them. Stream deposits are the last resting place for gold. Once the gold has been released from the lode, gravity and nature does the rest. And unless gold gets stranded on a bench, it will find its way to the water someday. It may take a million years, but it will get there. When deciding where to begin prospecting, most of the time you’ll want to start panning in a water way, or a wash in the desert where water once flowed. Then let the gold tell you where to go from there. When the gold gets coarse and ragged, start to move up, looking in reverse of how it got to the spot where you found it. In addition to panning and sluicing you may wish to upgrade your mining efforts with a highbanker or power sluice, dredge or trommel. Moving soft soil or river gravel is obviously much easier than breaking rock, but for small scale miners, a rock crusher can pulverize 2 or 3 inch sized rocks into powder in no time. Move more material faster— get more gold! |
Nugget of News Blog |