Professor Michael Fuller examines shoreline erosion in Area 10 during June of 2004. The water has begun to erode the squares in the north edge of the grid and the rainstorms have eroded the plaster in the wine press and fermentation vat. The rate of erosion will be slower than in Areas 9 or 10 because most of the squares in Area 10 were backfilled with excavated soil from Area 11. The main mound of Tell Tuneinir can be seen in the distance.

Photographic Credit: Professor Michael Fuller Last updated 28 February 2004.