Possibly accumulation of small to medium basalt and tufo stones over time; could also have been formed by the collapse of a nearby architectural feature, i.e. a wall. The deposit may have also been altered by later spoiliation events following the disuse, collapse, and abandonment of the SU.
Taken from the west.
Taken from the south.
Deposit of stones E. of 8122 and W. of 8075, 8074 and 8041