By Victoria Pease

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To Dionysius my most dear friend," it reads. "I ask that you send the money if you are able. Send it with Serapion since I need it, and do not fail. " The writer's name is broken off the shard, so we will never know who had such a pressing need for money in a place where, it would seem, money could buy nothing. The westward march from Badi'a moves between Jabal Qattar's red granite massif on the left and Abu Dukhan's black basalt on the right, the two hills placed like navigational buoys on a river.

51. , 2006). Left: Relative probability histograms for all U–Pb SHRIMP ages of detrital zircons (Israel onleft, Jordan on right). The relative probabilities of weighted mean ages of all data are limited by the black curves, whereas the concordant ages histograms are filled grey. Arrows indicate correlative formations. 2 Ga. The superimposed bar graphs indicate the results of mixture modelling, namely each age subgroup with its 95% confidence limits and relative abundance. , 1991) or in sediments preserved in the post-accretionary basins of the Arabian Shield (Johnson, 2003).

It is also worth noting that detrital zircons from Cambro-Ordovician sandstones of southern Israel and Jordan show very similar age distributions (Fig. 51). 0 Ga zircons, an age that is rarely observed in Neoproterozoic samples from Egypt but is more common in Neoproterozoic samples from Arabia. 0 Ga age is unknown from the ANS or its flanks and is not encountered in the EAO north of Tanzania. 0 Ga zircons. Fig. 51. , 2006). Left: Relative probability histograms for all U–Pb SHRIMP ages of detrital zircons (Israel onleft, Jordan on right).

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Eastern Desert Field Workshop by Victoria Pease

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