The use of a track mounted sonic drill has resulted in the recovery of till for the first time under the lake in the up-ice direction from the high grade boulder trains on Isle Brochet and resulted in the recovery of a complete intersect of the underlying glacial till. Initial interpretation of this unit is favorable and suggests less post depositional disturbance than assumed, supporting the theory that the glacial till in which the historic high grade boulder trains on Isle Brochet occur, does extend up ice under the lake towards a source location.
Importantly, this suggests that it will be possible to use the subglacial till sampling method to trace the dispersion of uraniferous till under the lake, and thus directly back to the source of the historic Isle Brochet high grade boulder trains.
The two previous sub glacial till programs completed by the geomorphological experts at
Figure 1 is available at https://www.globenewswire.com/NewsRoom/AttachmentNg/e5fb2810-f200-4200-b193-6b68cef060ec
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Figure 1
Drilling Updated
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