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The stochastic nature of burial depth and hence in nuclide production in these clasts during exhumation and fluvial transport, and during post-depositional stirring, results in great variability in clast nuclide concentrations.

We present a method for dealing with the problem of pre-depositional inheritance of cosmogenic nuclides.

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Depth profiles show the expected shifted exponential concentration profile that we attribute to the sum of uniform mean inheritance and depth-dependent post-depositional nuclide production.

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That the depth-dependent parts of the profiles are exponential argues against significant post-depositional displacement of clasts within the deposit.

Our technique yields Be age estimates of 60±9, 102±16 and 151±24 ka for the three highest terraces, corresponding to isotope stages 4, 5d and 6, respectively.

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