Rio Madeira
PROJECT
Porto Velho, located on the Madeira River, Brazil
The Madeira River valley, Rondônia, Brazil
More than 7Moz of gold mined over 20 years.
Discovery
Historic Mining
* ‘wildcat’ artisanal miners of Brazil
Rio Madeira Project: Amazonas / Rondônia, Brazil
Gold Dredges on Rio Madeira During Gold Rush in 1980s (Between Porto Velho and Guajará-Mirim, Rondonia
View of pilot house on the dredge.
Detail of cutter head at end of suction line.
Swarm of dredges working a bonanza on the river bottom.
The “Mocururu” gold-bearing duricrust can’t be mined by the artisanal dredges because it is lithified and too “hard” for them to deal with, so they just “throw it overboard.”
This duricrust, which protects the gold-bearing gravel and itself contains gold mineralization, probably formed from 10 to 6 Ma ago, in response to the onset of a dry climate period, subaerial exposure, and lateritic soil formation. (Mörner et al., 2001).
The extent of Mocururu beyond the river and throughout the Madeira river valley has been partially identified.
Determination of the full potential dispersal area is Canary Gold’s opportunity.
The regional geological setting is Precambrian basement overlain by Miocene to Pliocene Amazon Basin sediments consisting of semi-consolidated sands interlayered with silt and clay.
This Amazon Basin sequence includes a medium grained conglomerate known locally as “Mocururu” – a sandstone or conglomerate up to 5m thick.
The Mocururu is a hard ferrocrete/duricrust rock believed to have formed over thousands of years.
Previous studies concluded Mocururu mineralization was the result of the transport and deposition of gold and heavy minerals eroded during the uplift of the Bolivian Andes in a large alluvial fan complex.
Historic studies concluded Mocururu units could be regionally extensive and potentially represent a world class gold exploration target.
Gold gravel and conglomerate with laterite to the top (mocururu) at the exposed bottom of the Madeira River, during low-water.
The paleoplacer deposits are regionally covered by a blanket of argillaceous strata, associated with gravel deposits. The younger cover is 5 to 35m thick and was deposited from the Pleistocene to the Holocene.
Idealized geological cross-section depicting the hypothetical regional distribution of the gold-bearing sedimentary units that crop out to the bottom of the Madeira River. According with this hypothesis, the gold-placer deposits remain in buried channels (paleocanals) of pleistocenic age.
Alternative Interpretation(s)
Adds to potential of the whole region
Madeira River – AGA Interpretation
Stratigraphic Drill Program
A 2012 stratigraphic drilling program was designed to test the exploration model that the Mocururu had the potential to extend outside the immediate vicinity of the Madeira River.
Canary Gold has the technical capability to identify potential Mocururu mineralization through the identification of historic river channels buried under the Mocururu ferrocrete.
SRTM
JERS-1/SAR
Landsat/TM
Detail showing interpreted paleochannels
Interpreted paleochannels over JERS-1/SAR image
Map with interpreted paleochannels
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