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Unit Book J6

The Northeastern End of the Temple Terrace and the Betili (Version 1a)

J6f275

Processed on 2025-01-08

1. OVERVIEW
2. IDENTIFICATION
- Designation
3. STRATIGRAPHY
6. REFERENCE
- Analogical Record

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1. OVERVIEW

Roster	Date	Author	Record
Included in other label	2009-07-17	pC	^glacis8 (escarpment) [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]

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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]

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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]
Argument	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	2009-08-10	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 (mx) 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]
Type of contact: earliest events	2010-07-27	pC	f275 (glacis) abuts f256 (isolated stone) [Input: U125PC.J]

Time Sequencing

Roster	Date	Author	Record
Stratum (to which element belongs)	2010-07-29	pC	s50^J6A [Input: U815PC.J]
Phase (to which element belongs)	2010-07-29	!!	h4m^J6A [Input: U815PC.J]
Stratigraphic reasons of assignment	2010-07-30	pC	is tentatively dated to Late Third Millennium on the base of the elevation, location and characteristics of the soil, very similar to ^glacis3 [Input: U730PC.J]

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6. REFERENCE

Analogical Record

Roster	Date	Author	Record
View/drawing of features	v191a 2009-08-09 pC [Input: T819PC.J] v195 2009-08-11 pC [Input: T819PC.J] v195a 2009-08-11 pC [Input: T819PC.J] v196 2009-08-11 pC [Input: T819PC.J] v198 2009-08-12 yM [Input: T819PC.J] v198a 2009-08-12 yM [Input: T819PC.J] v200 2009-08-12 yM [Input: T819PC.J] v209 2009-08-18 yM [Input: T819PC.J] v217 2009-08-25 yM [Input: TX04PC.J] v217a 2009-08-25 yM [Input: TX04PC.J] v218 2009-08-25 yM [Input: TX04PC.J] v218a 2009-08-25 yM [Input: TX04PC.J] w110 2010-07-17 pc [Input: U726PC.J] w206 2010-07-17 pc [Input: U726PC.J]