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Primary image for 1955 WHERE TO LOOK FOR URANIUM IN CALIFORNIA WESTERN MINING MAGAZINE ROCK HOUND
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1955 WHERE TO LOOK FOR URANIUM IN CALIFORNIA WESTERN MINING MAGAZINE ROCK HOUND

$199.00

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Estimated to arrive by Mon, May 5th. Details
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Shipping options

Estimated to arrive by Mon, May 5th. Details
Calculated by USPS in US.

Offer policy

OBO - Seller accepts offers on this item. Details

Purchase protection

Payment options

PayPal accepted
PayPal Credit accepted
Venmo accepted
PayPal, MasterCard, Visa, Discover, and American Express accepted
Maestro accepted
Amazon Pay accepted
Nuvei accepted

Item traits

Category:

Paper Items

Quantity Available:

Only one in stock, order soon

Condition:

Used

Country/Region of Manufacture:

United States

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Posted for sale:

More than a week ago

Item number:

757249056

Item description

1955 WHERE TO LOOK FOR URANIUM IN CALIFORNIA WESTERN MINING MAGAZINE ROCK HOUND 1955 WHERE TO LOOK FOR URANIUM IN CALIFORNIA WESTERN MINING MAGAZINE ROCK HOUND Click image to enlarge Description GREETINGS, FEEL FREE TO "SHOP NAKED" We deal in items we believe others will enjoy and want to purchase. We are not experts. We welcome any comments, questions, or concerns. WE ARE TARGETING A GLOBAL MARKET PLACE. Thanks in advance for your patronage. Please Be sure to add WDG to your favorites list! NOW FOR YOUR VIEWING PLEASURE… WHERE TO LOOK FOR URANIUM IN CALIFORNIA by LEE RAYMOND COPYRIGHT 1955 DONAL I. SEGERSTROM WESTERN MINING MAGAZINE SONORA CALIFORNIA 40 PAGE PAPERBACK / TRADE STAPLE BINDING COVER IS LOOSE SHOWS AGE COLORATION RARE / HARD TO FIND / HTF SOME CONTENT INCLUDES: MINERALS WHERE TO SEND SAMPLES FOR IDENTIFICATION FOR ASSAYING WHERE TO LOOK LIBRARY FIELD BASIN RANGES SOUTHERN DESERT SIERRA NEVADA KLAMATH MOUNTAINS COASTAL RANGES CASCADE RANGE COLOMBIA LAVA PLATEAU GREAT VALLEY DEPOSITS PEGMATITE CARNOTITE COPPER FLUORSPAR COAL LAKE BEDS VOLCANIC ROCK BY COUNTY... HOW TO FILE A CLAIM NATIONAL FOREST MAPS PHYSIOGRAPHIC PROVINCES COPPER DEPOSITS LEAD - SILVER - ZINC COBALT BISMUTH DEPOSITS AND MUCH MORE... INCLUDED IS A 6 PAGE TYPED COPY OF "CONFIDENTIAL TIPS ON GOLD PLACERING IN NEVADA" --------------------- FYI Uranium is a chemical element with symbol U and atomic number 92. It is a silvery-grey metal in the actinide series of the periodic table. A uranium atom has 92 protons and 92 electrons, of which 6 are valence electrons. Uranium is weakly radioactive because all isotopes of uranium are unstable, with half-lives varying between 159,200 years and 4.5 billion years. The most common isotopes in natural uranium are uranium-238 (which has 146 neutrons and accounts for over 99%) and uranium-235 (which has 143 neutrons). Uranium has the highest atomic weight of the primordially occurring elements. Its density is about 70% higher than that of lead, and slightly lower than that of gold or tungsten. It occurs naturally in low concentrations of a few parts per million in soil, rock and water, and is commercially extracted from uranium-bearing minerals such as uraninite. In nature, uranium is found as uranium-238 (99.2739–99.2752%), uranium-235 (0.7198–0.7202%), and a very small amount of uranium-234 (0.0050–0.0059%). Uranium decays slowly by emitting an alpha particle. The half-life of uranium-238 is about 4.47 billion years and that of uranium-235 is 704 million years, making them useful in dating the age of the Earth. Many contemporary uses of uranium exploit its unique nuclear properties. Uranium-235 is the only naturally occurring fissile isotope, which makes it widely used in nuclear power plants and nuclear weapons. However, because of the tiny amounts found in nature, uranium needs to undergo enrichment so that enough uranium-235 is present. Uranium-238 is fissionable by fast neutrons, and is fertile, meaning it can be transmuted to fissile plutonium-239 in a nuclear reactor. Another fissile isotope, uranium-233, can be produced from natural thorium and is also important in nuclear technology. Uranium-238 has a small probability for spontaneous fission or even induced fission with fast neutrons; uranium-235 and to a lesser degree uranium-233 have a much higher fission cross-section for slow neutrons. In sufficient concentration, these isotopes maintain a sustained nuclear chain reaction. This generates the heat in nuclear power reactors, and produces the fissile material for nuclear weapons. Depleted uranium (238U) is used in kinetic energy penetrators and armor plating. Uranium is used as a colorant in uranium glass, producing lemon yellow to green colors. Uranium glass fluoresces green in ultraviolet light. It was also used for tinting and shading in early photography. The 1789 discovery of uranium in the mineral pitchblende is credited to Martin Heinrich Klaproth, who named the new element after the recently discovered planet Uranus. Eugène-Melchior Péligot was the first person to isolate the metal and its radioactive properties were discovered in 1896 by Henri Becquerel. Research by Otto Hahn, Lise Meitner, Enrico Fermi and others, such as J. Robert Oppenheimer starting in 1934 led to its use as a fuel in the nuclear power industry and in Little Boy, the first nuclear weapon used in war. An ensuing arms race during the Cold War between the United States and the Soviet Union produced tens of thousands of nuclear weapons that used uranium metal and uranium-derived plutonium-239. The security of those weapons and their fissile material following the breakup of the Soviet Union in 1991 is an ongoing concern for public health and safety. The discovery of the element is credited to the German chemist Martin Heinrich Klaproth. While he was working in his experimental laboratory in Berlin in 1789, Klaproth was able to precipitate a yellow compound (likely sodium diuranate) by dissolving pitchblende in nitric acid and neutralizing the solution with sodium hydroxide. Klaproth assumed the yellow substance was the oxide of a yet-undiscovered element and heated it with charcoal to obtain a black powder, which he thought was the newly discovered metal itself (in fact, that powder was an oxide of uranium). He named the newly discovered element after the planet Uranus (named after the primordial Greek god of the sky), which had been discovered eight years earlier by William Herschel. In 1841, Eugène-Melchior Péligot, Professor of Analytical Chemistry at the Conservatoire National des Arts et Métiers (Central School of Arts and Manufactures) in Paris, isolated the first sample of uranium metal by heating uranium tetrachloride with potassium. Henri Becquerel discovered radioactivity by using uranium in 1896. Becquerel made the discovery in Paris by leaving a sample of a uranium salt, K2UO2(SO4)2 (potassium uranyl sulfate), on top of an unexposed photographic plate in a drawer and noting that the plate had become "fogged". He determined that a form of invisible light or rays emitted by uranium had exposed the plate. Worldwide production of U3O8 (yellowcake) in 2013 amounted to 70,015 tonnes, of which 22,451 t (32%) was mined in Kazakhstan. Other important uranium mining countries are Canada (9,331 t), Australia (6,350 t), Niger (4,518 t), Namibia (4,323 t) and Russia (3,135 t). Uranium ore is mined in several ways: by open pit, underground, in-situ leaching, and borehole mining (see uranium mining). Low-grade uranium ore mined typically contains 0.01 to 0.25% uranium oxides. Extensive measures must be employed to extract the metal from its ore. High-grade ores found in Athabasca Basin deposits in Saskatchewan, Canada can contain up to 23% uranium oxides on average. Uranium ore is crushed and rendered into a fine powder and then leached with either an acid or alkali. The leachate is subjected to one of several sequences of precipitation, solvent extraction, and ion exchange. The resulting mixture, called yellowcake, contains at least 75% uranium oxides U3O8. Yellowcake is then calcined to remove impurities from the milling process before refining and conversion. Commercial-grade uranium can be produced through the reduction of uranium halides with alkali or alkaline earth metals. Uranium metal can also be prepared through electrolysis of KUF 5 or UF 4, dissolved in molten calcium chloride (CaCl 2) and sodium chloride (NaCl) solution. Very pure uranium is produced through the thermal decomposition of uranium halides on a hot filament. (THIS PICTURE FOR DISPLAY ONLY) --------------------------- Thanks for choosing this sale. You may email for alternate payment arrangements. We combine shipping. Please pay promptly after the auction. The item will be shipped upon receipt of funds. Also, INTERNATIONAL CUSTOMS is the international buyers obligation and must be aware of their own customs laws. We cannot be responsible for seized or quarantine purchases. If your shipping costs seems high, it is because we ensure that your purchase is well packed, quickly delivered, and insured to arrive safe and sound. WE ARE GOING GREEN, SO WE DO SOMETIMES USE CLEAN RECYCLED MATERIALS TO SHIP. Please leave feedback when you have received the item and are satisfied. Please respond when you have received the item. ***** 5*'s ***** If you were pleased with this transaction, please respond with all 5 stars! If you are not pleased, let us know via e-mail. Our goal is for 5-star service. We want you to be a satisfied, return customer. Please express any concerns or questions. More pictures are available upon request. The winning bid will incur the cost of S/H INSURED FEDEX OR USPS. See rate calculator or email FOR ESTIMATE. International Bidders are Welcome but be mindful if your country is excluded from safe shipping. Thanks for perusing THIS and ALL our auctions. Please Check out our other items! WE like the curious and odd. BUY, BYE!! Images sell! 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