equals other label | 2008-2-02 | jW | f50 | [Input File: S202jW.J] |
2008-2-12 | jW | f140 | [Input File: S212jW4.J] | |
2008-2-12 | jW | f174 | [Input File: S212jW4.J] | |
includes other label | 2021-3-07 | jW | ^EDIIIinstal | [Input File: ZF307jW.j] |
category | !! | !! | installation | [Input File: !!] |
definition (typological label) | 2006-8-14 | eF | glacis | [Input File: Qx06eI.j] |
summary | 2012-10-07 | jW | Layer of baqaya that forms the glacis of the temple mound and that protects the revetment wall f11 from erosion. | [Input File: Wx07jW1.j] |
best image | !! | !! | p34 | [Input File: !!] |
description (summary) | 2006-10-09 | jW | A thick surface of baqaya sloping sharply down the surface of the temple mound from the BA temple to the north to the revetment wall to the south in k13. It links with an identical surface, f50, discovered to the south in k12 in season MZ18. It formed the original surface of the mound when it was constructed and undoubtedly facilitated the runoff of water during periods of rain. Baqaya, the local virgin soil, has the property of percolating slowly any water which sits on its surface. | [Input File: Qx09jW.j] |
best view | 2007-4-03 | jW | v52 | [Input File: R403jW.j] |
daily notes | 2010-9-13 | jW | After thoroughly cleaning the surrounding area, we removed the portion of the baqaya surface which formed the top of k110. Few sherds were recovered. | [Input File: U914jW.j] |
argument | 2010-9-13 | jW | For the following reasons we determined that the baqaya surface, f109, provided an excellent seal to the material below it: It was contiguous over the entire locus; It was at least 5cm thick everywhere; It was extremely hard. |
[Input File: U914jW.j] |
relays (applicable to elements) | 2006-9-27 | bL | 2528 (41014 48947 - 9053 / Relay location: SW) | [Input File: Q927BL-R.J] |
2006-9-27 | bL | 2525 (41638 49174 - 9287 / Relay location: NW) | [Input File: Q927BL-R.J] | |
2006-9-27 | bL | 2526 (41505 49544 - 9295 / Relay location: NE) | [Input File: Q927BL-R.J] | |
2006-9-27 | bL | 2527 (40926 49323 - 9086 / Relay location: SE) | [Input File: Q927BL-R.J] | |
m#/elev @top | 2006-8-14 | eF | m3933 | [Input File: Qx06eI.j] |
height @top | 2006-8-14 | eF | 33 | [Input File: Qx06eI.j] |
h-eye @top | 2006-8-14 | eF | 163 | [Input File: Qx06eI.j] |
elevation | 2010-9-13 | jW | 9301 (NW corner) | [Input File: U914jW.j] |
2010-9-13 | jW | 9244 (W middle) | [Input File: U914jW.j] | |
2010-9-13 | jW | 9215 (SW corner) | [Input File: U914jW.j] | |
2010-9-13 | jW | 9211 (SE corner) | [Input File: U914jW.j] | |
2010-9-13 | jW | 9247 (E middle) | [Input File: U914jW.j] | |
2010-9-13 | jW | 9294 (NE corner) | [Input File: U914jW.j] | |
2010-9-13 | jW | 9244 (locus center) | [Input File: U914jW.j] | |
notes on volumetric localization | 2010-9-13 | jW | Took seven elevations with the level to accurately determine the slope. | [Input File: U914jW.j] |
type of contact: contemporary events/movable items | 2010-9-13 | jW | q409 (pottery) sits in f109 (glacis) | [Input File: Ux05jW2.j] |
2010-9-16 | jW | q416 (pottery) sits in f109 (glacis) | [Input File: Ux05jW2.j] | |
type of contact: earliest events | 2012-4-14 | jW | f109 (glacis) covers f346 (fill) | [Input File: W414jW.j] |
stratum (to which element belongs) | 2012-9-09 | jW | s650aJ3B | [Input File: W909jW.j] |
stratigraphic reasons of assignment | 2012-10-07 | jW | Baqaya layer sloping down from north to south that forms the glacis that meets the top of the EDIII revetment wall. It is the northward extension of f50. | [Input File: Wx07jW.j] |
typological reasons for assignment | 2012-10-07 | jW | Only a small segment of this feature was excavated, yielding a small number of sherds which have not been fully analyzed. | [Input File: Wx07jW.j] |
other reasons, reservations, qualifications | 2012-10-07 | jW | This impervious layer of baqaya formed the surface of the temple mound above (north) of the revetment wall. It served both as a decoration and as a protective surface to direct precipitation water over the wall top, thus preventing erosion and weakening of the stone structure. It must have been an integral part of the EDIII remodeling of the temple mound. | [Input File: Wx07jW.j] |
phase (to which element belongs) | 2012-9-09 | jW | h3mJ3B | [Input File: W909jW.j] |
strata (included within phase) | 2012-10-07 | jW | s650aJ3B | [Input File: Wx07jW.j] |
review of ceramics | 2010-9-13 | jW | A preliminary analysis of the ceramics by mKB, dated this feature to the LC3 period. | [Input File: U914jW.j] |
full analysis of ceramics | 2010-9-14 | mKB | Late Chalcolithic 3 | [Input File: U914mKB1.j] |
color | 2006-8-14 | eF | light gray | [Input File: Qx06eI.j] |
color number (Munsell) | 2006-8-14 | eF | 10YR 7/2 | [Input File: Qx06eI.j] |
hardness, compaction | 2006-8-14 | eF | 4.5+ | [Input File: Qx06eI.j] |
texture, surface finish | 2006-8-14 | eF | hard layer | [Input File: Qx06eI.j] |
full analysis of ceramics | 2010-9-14 | mKB | body sherds and shape sherds all typical for LC3. One LCF body sherd, no shape sherds in this ware. Shape sherds in LCH ware include 4 typical bowls but not of the very common hammer rim type/ | [Input File: U914mKB1.j] |
view/drawing of features |
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