Rare Earths or Rare Metals?

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Wed, Jun 16, 2010
Feature Articles, Rare Earth Articles
Post by Melissa Pistilli, Rare Earth Senior Reporter

Rare Earth Elements: Key for Future Technologies

By Desmond McMahon–Exclusive to Rare Earth Investing News

Rare earth elements (REE) have occupied a quiet corner of the mining industry since the late 1950s, but their unique properties have made them crucial to a number of emerging and growing technologies, increasing their demand and strategic importance.

Despite their name, Rare Earth Elements are found in relative abundance around the world, but it is rare to find a commercially viable deposit. Officially, the International Union of Pure and Applied Chemistry defines Rare Earth Elements as the 15 Lanthanide elements, plus Scandium and Yttrium. These elements are grouped together on the periodic table and share similar chemical properties, often making them interchangeable in their commercial applications ranging from use in catalysts and computers, to magnets, cell phones and hybrid cars.

Rare Earth Elements can be further divided into two sub-groups using their atomic weight: Heavy Rare Earth Elements (HREE) and Light Rare Earth Elements (LREE). HREE are the more sought after of the two types and more valuable. Europium, Gadolinium, Terbium, Dysprosium, Holmium, Erbium, Thulium, and Ytterbium are all considered HREE; and due to their characteristics, Yttrium and lutetium are also sometimes included in this group.

LREE include Lanthanum, Cerium, Praseodymium, Neodymium, Promethium and Samarium, which are generally more abundant and less valuable than the heavier HREE.  Europium, Terbium and Dysprosium are exceptions and quite valuable.

It is also important to note the distinction between rare earth elements and similar terms used in the resource sector. Two classifications that are often confused with rare earth elements are Rare Earth and Rare Metals.  While the Rare Earth classification encompasses all the Rare Earth Elements, the term also includes the 15 metals in the Actinide group of the periodic table. Rare Metals are a loosely defined group of resources including tantalum, niobium and the platinum group of metals, which are genuinely rare and valuable, but not rare earth elements.

The Rare Earth Element market is inherently more complex than markets for more traditional resources, like gold or copper, because it is made up of so many different minerals, but it is the extraction process that truly complicates Rare Earth Elements, which are found clumped together in mineral deposits.

China currently produces over 95 percent of the world’s rare earth supply, mostly in Mongolia, but high concentrations have also been identified at Mountain Pass, California, and Mount Weld, Australia.

Once the rare earth ore has been removed from the mineral deposit, the difficult task of separating the different minerals into oxides begins.  Because the elements share similar characteristics, the separation process is complex and it can vary from one mineral resource to another. A deposit could contain a number of different metals; but, with no processes available to extract them all a company might have to focus on one element at the expense of another.

Thorium, Uranium and other radioactive elements can also contaminate Rare Earth Element deposits, making the elements more expensive to recover.

Once the different minerals have been refined into oxides they are formed into rare earth alloys before they are manufactured into their applications.

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  • http://www.usrareearths.com/eco/ kennedy200@sbcglobal.net

    UPDATE
    U.S. Rare Earths, Inc. Announces Strategic Review

    Press Release Source: U.S. Rare Earths, Inc. On Monday June 14, 2010, 8:01 am EDT
    SALT LAKE CITY–(BUSINESS WIRE)–U.S. Rare Earths, Inc. (“U.S. Rare Earths, Inc.” or the “Company”), a private company, announced today that it has initiated a review of strategic alternatives to enhance shareholder value, including those involving a possible merger, sale or other transaction. The Board of Directors of the Company has engaged Pope and Company Limited (“Pope”) to act as the Company’s financial advisor.

    U.S. Rare Earths, Inc.’s Chief Executive Officer, Edward Cowle, explained that growing awareness by the U.S. government of Chinese dominance in the rare earth element (“REE”) market continues to increase the value of the Company’s REE reserves. In particular, the U.S. Government Accountability Office (“GAO”) report issued in April demonstrates the need for the Department of Defense to mitigate REE supply chain risks. Cowle stated, “The GAO has recognized U.S. Rare Earths, Inc.’s resources as a key component in the effort to expand domestic production of light and U.S. Rare Earths, Inc.’s Chief Executive Officer, Edward Cowle heavy REEs.”

    U.S. Rare Earths, Inc. holds 169 unpatented mining claims of individual major vein deposits of REEs in the Diamond Creek and the Lemhi Pass areas of Idaho and Montana. The United States Geological Survey (“USGS”) reported total rare earth oxide (“TREO”) concentrations of 0.59 to 5.51% and an overall grade of resource of 1.22% TREO at Diamond Creek. TREO content of recent sampling of a number of the veins at Diamond Creek by U.S. Rare Earths, Inc. ranged from about 0.06 to 4.3% with an average TREO of about 1.2%. The USGS also reported average TREO concentration of 0.52% at Lemhi Pass.
    According to reports by the USGS, the Company’s REE deposits are:
    • one of the two largest reported historical estimates of REEs in the U.S.;
    • one of only six proven, substantial deposits of REEs in the world outside of mainland China or Chinese control; and
    • The only significant U.S. REE deposit that has heavy REE (“HREE”) concentrations.
    In addition, recent geologic investigation by the Company including age dating of mineralization and of igneous intrusive rock at Lemhi Pass indicates that the age of rare earth and thorium mineralization is Devonian (350 Ma) and that of previously unknown alkali complex intrusive rock as Cambrian (500Ma). Recent and ongoing work suggests the potential for a larger buried mineralized system possibly similar in nature to peralkaline REE-Th, IOCG/Fe-REE and/or carbonatite models of deposition. Historical and recent work by the Company at Diamond Creek suggests similarities to Lemhi Pass and also includes a potential for a larger buried Fe-REE-Th system.

    “We are committed to finding a partner or buyer that has the financial capability and resources to ensure that the properties are developed as rapidly as possible,” said Cowle.
    http://www.usrareearths.com/eco/

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