| Roster |
Date |
Author |
Record |
| Locus |
2001-06-10 |
lR |
k6 [Input: L724LR.j] |
| Relays (applicable to elements) |
2001-06-12 |
lr |
r15 (41186 37385 - 8809 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r16 (41164 37702 - 8801 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r17 (41153 37523 - 8809 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r18 (41184 37516 - 8809 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r19 (41237 37646 - 8809 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r20 (41250 37406 - 8809 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r21 (41034 37714 - 8812 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r22 (40927 37544 - 8811 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r28 (40940 37413 - 8804 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r29 (40947 37413 - 8804 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r30 (40947 37353 - 8804 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| 2001-06-12 |
lr |
r31 (40939 37349 - 8804 / Relay location: see sketch 8) [Input: R7QFAB1R.j] |
| Roster |
Date |
Author |
Record |
| Stratum (to which element belongs) |
2000-12-18 |
!! |
s255AHH [Input: A-CUMUL.j] |
| 2015-05-20 |
!! |
s250AAH, s255AAH [Input: ZA520CJC.j] |
| Phase (to which element belongs) |
2000-12-18 |
!! |
h6hAAH [Input: A-CUMUL.j] |
| 2015-05-20 |
!! |
h6hAAH [Input: ZA520CJC.j] |
| Notes on time sequencing |
2001-06-17 |
fAB |
This aggregate is covered by brickfall f25 (which is actually in k5, but clearly is present in k6) which instead abuts a1 in k5. This means that a2 is earlier in date than a1, and a3 to the E seems to also be abutted (or even the point of origin) by a brickfall f21 which seems the same as f25. [Input: L617FAB.j] |
| 2001-07-04 |
fAB |
We are presented now with the problem of linking the several aggregates together into a meaningful stratigraphic sequence. As we understand it now, a2 is the oldest structure that we have, as it sits on the pit in the N section of A13. a2 is clearly below a1, separated by a gray layer. a1 is contemporary with a5 and a3, since all abut but are not covered by brickfall. Questions arise when we look at the differences in elevation: a5 is considerably higher than a1 and a3. This seems to indicate a terracing, which we would expect to result from extended building in the phase of a2. [Input: L704FAB.j] |
| 2001-07-23 |
sV |
a2 belongs to phase 5b and seems to be the only well preserved structure of this phase. The other structures to the West of a2 show a more complicated situation. [Input: L818LR.j] |