1. OVERVIEW
| Roster | Date | Author | Record |
|---|---|---|---|
| Category | !! | !! | fill, dumping, collapse |
| Best definition | 2009-08-09 | lC | collapse [Input: T819MM2.j] |
| Best image | 2009-09-15 | lC |  [Input: T915LC5.j] |
2. IDENTIFICATION
Designation
| Roster | Date | Author | Record |
|---|---|---|---|
| Description (summary) | 2009-08-17 | lC | Collapsed stones, likely from walls f259 and f288. It is just the first level of stones, probably showing a collapse happened in different moments. It forms a sort of alignment running north to south, parallel to wall f259, about one meter far from it. The stone are medium to big in size and some lay flat, other are slightly inclined to the east. [Input: T815LC.j] |
3. STRATIGRAPHY
Recovery/Assignment
| Roster | Date | Author | Record |
|---|---|---|---|
| Argument | 2009-08-17 | lC | Could these stones be something different from a collapse? Unfortunatly we can't date exactly the collapse of the eastern part (and if it's natural or a volontary manmade action) of ^str1, because of the later cuts. So could these stones be stored for the construction of the revetment wall? It seems that the accumulations below are still dating to the EDIII as shown by the sounding in k130. It is an interesting question, but so far we didn't get a clear answer, and the hypothesis of the collapse remains the most plausible. [Input: T815LC.j] |
| Evolution | 2006-10-04 | lC | Further excavation will clarify if this large stone collapse can be divided in different levels, corresponding to different moments, of the collapse. From a stratigraphic point of view with some of the stones resting on f362 and other covered by f362 it seems plausible. [Input: V114LC.j] |
Volumetric Localization
| Roster | Date | Author | Record |
|---|---|---|---|
| Locus | 2009-08-09 | lC | k127 [Input: T819MM2.j] |
| M#/elev @top | 2009-08-09 | lC | m6103 [Input: T819MM2.j] |
Contact Association
| Roster | Date | Author | Record |
|---|---|---|---|
| Type of contact: latest events | 2009-08-22 | lC | f354 (accumulation D) abuts f336 (collapse) [Input: T822LC2.j] |
| 2009-08-22 | lC | f358 (accumulation D) abuts f336 (collapse) [Input: T822LC2.j] | |
| 2009-08-22 | lC | f359 (accumulation C) abuts f336 (collapse) [Input: T822LC2.j] | |
| 2009-08-22 | lC | f278 (accumulation D) overlays f336 (collapse) [Input: T822LC2.j] | |
| 2009-08-22 | lC | f345 (accumulation C) overlays f336 (collapse) [Input: T822LC.j] | |
| Type of contact: earliest events | 2009-08-22 | lC | f336 (collapse) rests on f362 (accumulation D) [Input: T822LC.j] |
Time Sequencing
| Roster | Date | Author | Record |
|---|---|---|---|
| Stratum (to which element belongs) | 2011-02-10 | lC | s651J1A [Input: V211LC.j] |
| Phase (to which element belongs) | 2011-02-10 | !! | h3mJ1A [Input: V211LC.j] |
| Stratigraphic reasons of assignment | 2011-02-11 | lC | Sitting on top of Mixed ED III and LC material, are covered by the the same type of material. Beside their possible use or intepretation the stones date to the construction of Revetment Wall and Early Escarpment. [Input: V212LC.j] |
4. TYPOLOGY
Morphology
| Roster | Date | Author | Record |
|---|---|---|---|
| Ware or Material, species | 2009-08-09 | lC | st [Input: T819MM2.j] |
| Color | 2009-08-09 | lC | white [Input: T819MM2.j] |
| Hardness, compaction | 2009-08-09 | lC | >4.5 [Input: T819MM2.j] |
