| 2008-08-11 |
lR |
A compact layer originally defined as brickmelt since the appearance resembled clay that had been melted from the rain, then baked by the sun forming a crust. We later redefined this feature after excavating it as the ancient tell surface at abandonment, with the compaction resulting from walking on the surface and natural rain and sun exposure. f27 was created to subsume all the compact brickmelt layers in A20 for ease in reference an event although the discrete feature numbers are still present according to loci. f20 was found on the western half of k14, not as compact and solid as in other loci, eventually diminishing towards the east turning into patches. [Input: S811LR6.j] |