Finds from the pavement area, encountered lying higher than the pavement are registered as planum
b. Stratigraphic information describing the exact position of finds from the diluvial fan are not
available. In particular, objects encountered in the channels, overlain by the travertine sands of the
diluvial fan sensu stricto, often cannot be related to those channels.
For some selected finds, the stratigraphic position inside the diluvial fan is described in the cited
literature. Most finds from the Chara limestone are not well documented and so have been deduced as
Finds >5cm that are not mapped in the documentation mostly come from the Chara limestone horizon or the fault (if one of the numerous faults disturbing the excavation area is located in the same grid square, and the material from the fault was considered to have been dislodged, then these finds are not documented).
Differential decay does not always help solve the question of provenance for those finds, nor do the excavation finds reports. If provenance cannot be ascertained from the documentation, or if finds from the diluvial fan cannot be further located within the travertine sands or the channels below, then these are indicated by a question mark.
Also see the locational data set entries for each find - view via the links in the Spatial provenance field.