MONTE ALTO
ULTRA HIGH-GRADE RARE EARTH AND CRITICAL MINERALS DISTRICT
BRE's first discovery was a groundbreaking deposit
Highly enriched with NdPr, DyTb, uranium, and other valuable co-products
Ultra-High-Grade Chevnikite-Apatite-Britholite (CAB)
Near-surface weathered regolith
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THE ANCHOR OF THE PLATFORM
ULTRA-HIGH-GRADE DEPOSIT THAT REMAINS OPEN AT DEPTH
The Monte Alto deposit is interpreted as a folded, laterally continuous, high-grade mineralised intrusive system. The drill-tested strike length of ultra-high-grade magmatic mineralisation currently extends for approximately 730 m, from near-surface ultra-high-grade mineralisation at the northern end of the deposit to down-plunge mineralisation toward the southeast, where the deposit remains open.
EXPANSION POTENTIAL
RECENT DISCOVERIES COULD ENLARGE MONTE ALTO'S SCALE
Prospecting within the Monte Alto District has identified an outcropping heavy rare earth-rich occurrence approximately 2.5 km south of the Monte Alto deposit. Surface sampling returned high-grade rare earth and heavy rare earth results, including a grab sample grading 14.6% TREO with elevated dysprosium, terbium, yttrium and uranium.
