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A reminder of Fish Lake from Lithium Corporation. Lithium...

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    A reminder of Fish Lake from Lithium Corporation.

    Lithium Corporation acquired the Fish Lake Valley prospect in 2009. In the
    1800s, it operated as a producer of borates from a lithium/boron/potassium
    rich brine recovered from the east side of the salt flats. The prospect is
    currently comprised of one hundred and forty three - 80 acre Association
    Placer claims for a total of approximately 11,360 acres (4,597 hectares),
    covering the most prospective portions of the playa. These flats lie at an
    elevation of 4684 feet (1427 meters) above sea level and are ideally suited
    for a lithium brine operation. In addition to the flat geography, the valley
    is arid and there are considerably more evaporative days in the year than days
    where conditions are not conducive to evaporation. The property is easily
    accessible via Highways 6 & 773 and several miles of well maintained gravel
    roads. In addition to the road network, infrastructure is very good in Fish
    Lake Valley with power, fuel and phone service available locally, and most
    supplies available in Tonopah approximately 40 miles (60 kms) east.

    As the crow flies the property is only 22 miles (35 kms) west across the
    Silver Peak Range from Albermarle's Silver Peak lithium brine operation, the
    only active commercial lithium mine in the United States. LTUM's Fish Lake
    Valley lithium-in-brine prospect is quite analogous to the Silver Peak lithium
    brine operation as:

    * Hosts a documented lithium enriched brine both near surface and at
    relatively shallow depths – has not been fully delineated, and explored to
    depth.

    * Brine hosted in the same sediments/rocks as the mineralized brine at
    Silver Peak.

    * Proximal to lithium enriched geothermal waters which are likely at least
    in part responsible for the formation of the lithium-in-brine deposits
    that occur both here and at Silver Peak.

    * Structure conducive to the formation of a Silver Peak style deposit. At
    the junction of a possible splay of the northeasterly trending Death
    Valley - Furnace Creek fault system and the northwesterly trending Grand
    Central fault which is possibly related to, or an extension of, the Cross
    Central fault that is an integral part of the system at the Silver Peak
    mine.

    Gw
 
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