.bk J04
.fl U331sC.j
.fd ___ CHECK of all ff in k100
.ei sC
.ed U331

.rd U331
.ri sC

f 150
df same as J06^glacis 3
ev Thanks to the excavations carried out in k100 in 2008 and 2009 (during these excavation seasons k100 was incorporated within J06 unit as k84), it has been possible to understand the nature of J04 f150, J04 f158 and J04 f160 (and partially the lowest portion of f121), i.e., the layers found while doing the deep sounding in J04 k100. As seen, J04 f150, J04 f158 and J04 f160 are the same of J06f164 which is a glacis layer (cfr. J06^glacis 3) made to protect a stone wall located on the west, J02 f129. The pottery recovered within J06f164 revealed Chalcolithic sherds, dating this and other layers related with this (cfr. for example, J06 f158, J06 f168, J06 f164 and all the features within s49 in J06 unit) back to the 3rd millennium BC (cfr. analysis of the pottery on S901 by MKB) thus revealing that in this portion of the tell mound 3rd millennium BC layers were located right below Mittani accumulations.

f 158
df same as J06^glacis 3
ev Thanks to the excavations carried out in k100 in 2008 and 2009 (during these excavation seasons k100 was incorporated within J06 unit as k84), it has been possible to understand the nature of J04 f150, J04 f158 and J04 f160 (and partially the lowest portion of f121), i.e., the layers found while doing the deep sounding in J04 k100. As seen, J04 f150, J04 f158 and J04 f160 are the same of J06f164 which is a glacis layer (cfr. J06^glacis 3) made to protect a stone wall located on the west, J02 f129. The pottery recovered within J06f164 revealed Chalcolithic sherds, dating this and other layers related with this (cfr. for example, J06 f158, J06 f168, J06 f164 and all the features within s49 in J06 unit) back to the 3rd millennium BC (cfr. analysis of the pottery on S901 by MKB) thus revealing that in this portion of the tell mound 3rd millennium BC layers were located right below Mittani accumulations. This explains now better why, in the pottery analyzed during the 2006 excavation season, there were Mittani sherds mixed with Chalcolithis, which was not really clear at that time.

f 160
df same as J06^glacis 3
ev Thanks to the excavations carried out in k100 in 2008 and 2009 (during these excavation seasons k100 was incorporated within J06 unit as k84), it has been possible to understand the nature of J04 f150, J04 f158 and J04 f160 (and partially the lowest portion of f121), i.e., the layers found while doing the deep sounding in J04 k100. As seen, J04 f150, J04 f158 and J04 f160 are the same of J06f164 which is a glacis layer (cfr. J06^glacis 3) made to protect a stone wall located on the west, J02 f129. The pottery recovered within J06f164 revealed Chalcolithic sherds, dating this and other layers related with this (cfr. for example, J06 f158, J06 f168, J06 f164 and all the features within s49 in J06 unit) back to the 3rd millennium BC (cfr. analysis of the pottery on S901 by MKB) thus revealing that in this portion of the tell mound 3rd millennium BC layers were located right below Mittani accumulations.
;(which corresponded, in the 2006 Mozan Chronology, to Phase 3, cfr. q269 and q276)