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33

Bear Lodge Property – Location Map

Geological Setting

The Bear Lodge Mountains of northeast Wyoming are composed primarily of the upper levels of a

mineralized Tertiary alkaline

igneous complex that is a component of the Black Hills Uplift of western South

Dakota and northeast Wyoming. Tertiary alkaline intrusive bodies in the northern Black Hills occur along a N70-

80W trending belt that extends from Bear Butte in South Dakota, through the Bear Lodge Mountains, to Devil’s

Tower and Missouri Buttes in northeast Wyoming. The Bear Lodge mining district is in the Bear Lodge Mountains,

near the western end of the northern Black Hills intrusive belt. The Bear Lodge Mountains expose and are underlain

by multiple alkaline plugs, sills, and dikes and intruded into Precambrian basement and Paleozoic and Mesozoic

sedimentary rocks approximately 38–52 million years ago. Rare earth and gold mineralization are found in separate

areas of the central crest and northern part of the Bear Lodge Mountains.

The Bear Lodge alkaline-igneous complex is a northwest-trending alkaline intrusive dome with dimensions

of approximately 10 kilometers NW-SE by 6 kilometers NE-SW. The complex consists predominantly of multiple

intrusions of phonolite, trachyte, and other alkaline igneous rocks, and a variety of associated breccias and

diatremes.

Exploration and Drilling

Historical exploration in the Bear Lodge district, including REE exploration carried out by the Company

from 2004 through 2012, is summarized in the Technical Report.. Exploration activities carried out by the Company

in 2013 through 2015 were limited as the focus turned to development drilling at the Bull Hill and Whitetail Ridge

deposits. These exploration activities included geochemical, geophysical, geological and mineralogical modeling of

the district and individual deposits.

The 2013 drilling program was conducted in two phases. The first phase took place in June and July and

involved infill drilling at the Whitetail Ridge deposit in order to upgrade a significant portion of the resource from

the Inferred Mineral Resource category to the Indicated Mineral Resource category. During this phase, 14 core holes

were drilled for a total of 3,556.3 meters (11,697.5 feet). The second phase was designed to upgrade part of the

high-grade resource at the Bull Hill deposit to the Measured Mineral Resource category, develop a more detailed

model of the REE grade distribution and provide additional material for bulk metallurgical testing. It consisted of

21 core holes totaling 3,247.1 meters (10,650.5 feet) and six reverse circulation (“RC”) twin holes totaling 832.3

meters (2,730 feet). The RC twin holes were drilled using a center return hammer with the objective of minimizing

hole erosion and obtaining assay data directly correlative to that from the adjacent core holes.