1. OVERVIEW
| Roster | Date | Author | Record |
|---|---|---|---|
| Included in other label | 2009-07-17 | pC | ^glacis8 (glacis) [Input: U717PC2.J] |
| Category | !! | !! | installation |
| Best definition | 2009-08-12 | pC | glacis [Input: T727YM.J] |
| Best image | 2010-08-04 | pC |  v195 [Input: U804PC.J] |
2. IDENTIFICATION
Designation
| Roster | Date | Author | Record |
|---|---|---|---|
| Description (summary) | 2009-08-12 | pC | a red compact accumulation, friable once exposed for several days it brakes off easily when it dries. It begins directly south of wall f218 and after about 1 meter it slopes down [Input: T810PC.J] |
3. STRATIGRAPHY
Recovery/Assignment
| Roster | Date | Author | Record |
|---|---|---|---|
| Argument | 2009-08-12 | pC | most probably a series of layers of earth were laied at the base of wall f218 and f219, protecting the base: those layers are f265, f276, f275, f309, f314, f260, f242: they slope toward south and are intentionally layed. They are not wind blown accumulations for the reasons above mentioned [Input: T810PC.J] |
| 2009-08-12 | pC | to me seemed that f275 could be the same of f164 in k83 for the following reasons: 1) the top surface of f275 has a clear shape, beginning south of wall f218 and sloping down after 1 meter; 2) the consistence and coloration is very similar to f164; 3) it is located also directly east of f129, as f164 and if one follows the slope of f275 one reaches f164: if wall f218 is not deep f275 would continue in f164; 4) it could have the same function as f164, as an escarpment to protect walls f129 and f218. Another plausible possibility is that is the same as escarpment f260, which is a reddish friable earth located also directly against wall f219 (which is the same wall as f218) and having the same characteristics and location [Input: T810PC.J] |
Volumetric Localization
| Roster | Date | Author | Record |
|---|---|---|---|
| Locus | 2009-08-12 | pC | k82 [Input: T727YM.J] |
Contact Association
| Roster | Date | Author | Record |
|---|---|---|---|
| Type of contact: latest events | 2009-07-31 | pC | f199 (cut) cuts f275 (glacis) [Input: ZJ116pC.j] |
| 2009-08-10 | pC | f269 (cut) cuts f275 (glacis) [Input: T810PC.J] | |
| 2009-08-10 | pC | f283 (cut) cuts f275 (glacis) [Input: U125PC.J] | |
| 2009-08-12 | pC | f278 (lens) intrudes f275 (glacis) [Input: T810PC.J] | |
| 2009-08-10 | pC | f274 (mix feature) rests on f275 (glacis) [Input: T810PC.J] | |
| 2009-08-10 | pC | f265 (accumulation D) covers f275 (glacis) [Input: T810PC.J] | |
| 2009-08-12 | pC | f276 (glacis) overlays f275 (glacis) [Input: T810PC.J] | |
| Type of contact: earliest events | 2009-08-12 | pC | f275 (glacis) abuts f218 (wall) [Input: T810PC.J] |
| 2010-07-27 | pC | f275 (glacis) abuts f256 (isolated stone) [Input: U125PC.J] |
Time Sequencing
| Roster | Date | Author | Record |
|---|---|---|---|
| Stratum (to which element belongs) | 2025-05-30 | pC | s630J6B [Input: ZJ530pC.j] |
| Phase (to which element belongs) | 2025-05-30 | !! | h3pJPD [Input: ZJ530pC.j] |
| Stratigraphic reasons of assignment | 2010-07-30 | pC | ^glacis8 [Input: ZJ703pC.j] |
