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alluvium
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alluvium

Sediments laid down by streams and rivers. The most common constituents are clay, silt, and gravel. The loose, unconsolidated material forms features such as river terraces, flood plains, and deltas.

Alluvium is deposited along the river channel where the water's velocity is too low to transport the river's load – for example, on the inside bend of a meander.



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The property is favourably situated in the uplands shedding alluvial material to rivers immediately north of the property boundary, which are the sites of alluvia gold workings.
Last year's drilling in this area defined a broad, relatively thick zone of sub-ore grade gold mineralization that may be proximate to higher grade, steeply dipping gold bearing structures masked by alluvia.
 
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