.bk A20
.fl S903lC2.j
.fd Feature description
.ed S903
.ei lC
.rd S826
.ri lC

f 144
ds Floor with a white surface due to the organic material on top of it. The floor is medium compacted and it is quite disturbed from animal holes. This floor is just few cm thick and in general it is quite badly preserved, because it is also disappearing toward west. It is not clear in which relationship it was and with which structures

f 145
ds This accumulation is a layer of brown clay soil with numerous small broken pieces of orange and gray bricks, probably coming from the mud brick wall f125, right west to this accumulation. In its lower part  these inclusions of brick pieces seem disappearing, while to the east there are less orange bricks and the soil is more gray. The accumulation is medium compacted and easily removable with the small pick. Some quite big sherds have been found inside it.

f 142
ds Floor quite compact with some traces of lamination that could be part of some kind of plastering. In some points there are traces of burning, as showed by the surface that appears from black to reddish in color. There are also traces of burnt clay, orange in color. Despite it seems plastered it is not very compacted, and it is just few cm thick. Some sherds and small traces of charcoal are visible in the surface. Also some traces of white due to organic material are recognizable in the surface. It has been uncovered for about 400cms north to south, in part underneath the brick installation f138, and for about 150 cm east to west, but it should cover originally all the room of a5.

f 146
ds Accumulation on top of the stone pavement f108. This accumulation is not very different from the accumulation above, f145, except for the smaller number of brick pieces. It is brown in color, with some sherds, small charcoals and components of fine orange clay. In some points, just on top of the stones of the pavement, there are patches of fine lime, trace of water stagnation.

f 147
ds Accumulation below the floor f142, brown to light orange in color. It is compacted, but easily removable with the small pick. It is a sandy soil probably in part coming from the crumble of orange mud bricks, despite no pieces of bricks are visible. There are some darker ashy lens and light brown patches. Just few sherds were found.