Just to add to Timmyk reply , we did not know this before ….
The fragile clasts and boulders of RVK preserved within the gravel also provide evidence that the terrace
or “confluence target” is both alluvial and elluvial in origin and that the primary source of the clasts is
proximal. This view is also supported by the coarse kimberlite nature of the diamonds being recovered.
Elluvial being the key word there .
glta
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