.bk J07
.fl U807cJC.j
.fd Additional information regarding features
.ei cJC
.ed U807
.rd U807
.ri cJC

-sg This excavation was primarily designed to clear a large area over a short period of time. Because we knew that J7 was part of the large open area of the ancient site, or the plaza, we did not expect any floors, structures or other architectural remains. This proved true and the area was almost entirely composed of brickfall from J6. As we did not expect any features we were able to excavate quickly and with arbitrary layers instead of changing features with differences in soil etc. Therefore most features were excavated with the big pick and with little recording. This did not negatively impact our final understanding of the area however this book does not follow the traditional pattern of recording found in some of the other J books. No sections were drawn, instead they were photographed and templates were made.

f 1
sm This feature is mostly composed of topsoil. Like many of the features in J7 it was excavated in as an arbitrary 50cm feature (see strategy section). Several floating stones were found in this feature and the associated baulks - f25,f4,f5,f6. Because this first feature was primarily topsoil the undecorated body sherds were discarded and only the decorated sherds and shape sherds were kept for analysis. This feature covers the whole locus, k1, and so was not relayed separately. The locus is defined by m4843, m4842, m4837, and m4838, however, a line from m4856 to m4874 in k4 defines the western edge of the excavated area and the limit of f1. 
ad volumetric feature
=l f2
=l f3
=l f14
=l f15
rd S729

f 2
sm This feature was excavated as a 50cm volumetric feature as we did not anticipate any surfaces or structures in this area. f1 is primarily composed of topsoil. Some floating stones(f38, f29, f37)were found in this feature and in the equivalent portions of the baulks. For this feature only the decorated sherds and the shape sherds were kept for analysis. Body sherds were discarded. This feature covers the whole locus. 
ad volumetric feature
=l f1
=l f3
=l f14
=l f15
rd S729


f 3
sm This feature is mostly composed of topsoil. It was excavated as a volumetric feature of 50cm (see strategy section). Floating stones f35 and f36 were found in the baulks associated with this level in this locus. This feature covers the whole of the locus, k3. Only shape sherds and decorated sherds were kept from this level as it was known to be topsoil. 
ad volumetric feature
=l f1
=l f2
=l f14
=l f15
rd S729

f 4
sm Large floating stone. f21, an accumulation of pebbles, comes up alongside the stone. This stone sits between the upper topsoil layer (f1) and the next arbitrary layer (f8). It is likely associated with several other floating stones at similar elevations such as f5, f6, f25, f38, f29, f37, f35, and f36.
li The bottom elevation of this stone was not taken. The measurements were done by the surveyor hB because we did not have the markers or equipment to take relays - therefore we only took the 3 points and the top elevation. 
tc si f8
rd S730

f 5
sm This is a large floating stone. It is associated with several other floating stones at similar elevations such as f4, f6, f25, f38, f29, f37, f35 and f36. It sits in the topsoil layer of f1. 
li The bottom elevation of this stone was not taken. The measurements were done by the surveyor hB because we did not have the markers or equipment to take relays - therefore we only took the 3 points and the top elevation.
tc si f8
rd S730

f 6
sm Another floating stone, likely associated with other floating stones at similar elevations such as f4, f5, f25, f38, f29, f37, f35, and f36. It sits in the topsoil layer of f1. 
li The bottom elevation of this stone was not taken. The measurements were done by the surveyor hB because we did not have the markers or equipment to take relays - therefore we only took the 3 points and the top elevation.
tc si f8
rd S730

f 7
sm This feature was the second 50cm volumetric feature in k2. It is mostly natural accumulations. This feature covers the whole locus. 
;df ad
=l f8
=l f9
rd S730
ad Volumetric feature

f 8
sm This feature was the second 50cm volumetric feature in k1. Inside of this arbitrary feature were two small pebble surfaces (f21, f13) and a large floating stone f4 (see v4). 
H99 Because we were excavating in arbitrary layers features f21 and f13 sit inside of f8, however the actual depositional process was natural accumulations, deposition of pebbles, then more natural accumulations. 
;df ad 
=l f7
=l f9
rd S730
ad Volumetric feature

f 13
H99 Because we were excavating in arbitrary layers features f21 and f13 sit inside of f8, however the actual depositional process was natural accumulations, deposition of pebbles, then more natural accumulations. 

f 21
H99 Because we were excavating in arbitrary layers features f21 and f13 sit inside of f8, however the actual depositional process was natural accumulations, deposition of pebbles, then more natural accumulations. 

f 9
sm This feature was the second volumetric feature in k3, directly under f3. It covers the whole locus and is composed of natural accumulations. 
;df ad
=l f8
=l f7
ad Volumetric feature
rd S730

f 10
sm This feature is the third volumetric 50cm feature in k1. It is composed of natural accumulations. It covers the whole locus. 
sg As there was not enough time during the season to completely excavate all of J7 down to the level of the plaza the southern-most loci were not excavated as deeply as we shifted focus to the northern loci. Therefore, f10 is the last feature excavated in k1. 
;li No bottom elevation was measured during the excavations. 
P99 This was the last feature excavated in k1
ad volumetric feature
=l f11
=l f12
el 9079 @bottom
rd S803

f 11
sm This feature is the third volumetric 50cm feature in k2. It is composed of natural accumulations and covers the whole locus. 
;df ad
ad volumetric feature
;li No bottom elevation was measured during excavations
sg As there was not enough time during the season to completely excavate all of J7 down to the level of the plaza the southern-most loci were not excavated as deeply as we shifted focus to the northern loci. Therefore, f11 is the last feature excavated in k2. 
P99 This was the last feature excavated in k2. We stopped at about the level where we anticipated finding brickfall. 
=l f12
el 9081 @bottom
rd S803

f 12
sm This feature is the third volumetric 50cm feature in k3. It is composed of natural accumulations and brickfall. It covers the whole locus. 
el 9039 @bottom
ad volumetric feature
pb No ending elevation for this feature was recorded. The beginning elevation of the feature below it, f44, has a top elevation of 9035 which is lower than the expected end elevation of this feature. This could be due to the difficulty of measuring the deep cuts in J7 due to lack of markers and the reliance on the surveyor for measurements. 
ha By looking at the q-lots and the measurements of the surrounding features it appears that this feature became deeper than the anticipated 50cm and is closer to 80cm in depth. The end elevation has been added as 9039 based on q-lot measurements. 
=l f11
rd S730
.rd Ux21
ev Because this feature was excavated volumetrically it included both natural accumulations and brickfall. It has therefore been included under both the ^bf and ^accum specific labels. 

.rd U807
f 13
sm This feature is a lens of sherds and pebbles, not a floor but possibly a dump.
P99 S730

f 21
P99 S730

f 14
sm Volumetrically defined 50cm feature. It primarily consists of topsoil. This feature covers the whole locus. 
=l f1
=l f2
=l f3
=l f15
P99 S731

f 15
sm Volumetrically defined 50cm feature. It primarily consists of topsoil and covers the whole locus. 
=l f14
=l f3
=l f2
=l f1
P99 S731

f 16
sm This feature is a volumetrically defined 50cm feature. It is composed of natural accumulations and covers the whole locus. 
=l f9
=l f7
=l f8
P99 S731

f 17
sm This feature is a volumetrically defined 50cm feature. It is composed of natural accumulations and covers the whole locus. 
=l f16
=l f9
=l f7
=l f8
P99 S810

f 19
el 9052 @bottom
sm This feature is a volumetrically defined 50cm feature. It is composed of natural accumulations and covers the whole locus. 
P99 S810

f 20
el 9133 @top
el 9052 @bottom
nv This feature was intended to be 50cm in depth but instead is closer to 80cm in depth due to difficulties measuring. Despite the larger feature, the matrix is still uniform and the deposits can be considered part of the same feature. 
sm This feature was a volumetrically defined 50cm feature. It is composed primarily of natural accumulations but towards the bottom around elevation 9098 brickfall began to be encountered. This feature represents the end of the brickfall and the beginning of the natural accumulations on top of the brickfall. 

f 21
sm This feature was composed of both an accumulation of stones in the SE corner of k1 as well as the accumulations directly underneath it. 
nv This feature, because it was a pedestal, is equivalent to several other features in k1, see types of contact for the different features it is related to. 

f 22
sm This feature is the north baulk of k1. It was a meter thick and 1.35 meters deep. The baulk is equivalent to the features f1, f8 and f10. It is composed of natural accumulations. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features. 
A35 v6
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 

f 23
sm This feature is the east baulk of k2. It was about 2 meters thick and 1.35 meters deep. The baulk is equivalent to the feature f1, f8, and f10. It is composed of natural accumulations. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features. 
pr This baulk was especially thick as it bordered on the large trench and was used to protect the workmen while they worked high above the trench. We did not want to risk a portion of the edge of the trench collapsing. Once they had excavated down in k1 they had an area to work from and it was taken away by shafat  until the last edge which was collapsed into the trench. This was also taken out by shafat. 
A35 v14
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 

f 24
sm This feature is the north baulk of k2. It was one meter thick and 1.35 meters deep. The baulk is equivalent to features f2, f7 and f11 in k2. The baulk was composed of natural accumulations. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features. 
A35 v7
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
rd S810

f 25
sm Floating stone found in k2 north baulk. It is related to the other floating stones f4, f25, f37 and f19.
ds This feature was discovered when the north baulk of k2 was removed. It partially sits inside the east baulk of k2 as well. It is clearly related to the other stones as can be seen in the views.
el 9147 @top
li No bottom elevation was recorded for this stone as it was removed as part of the east baulk.
rd S817
tc si f1
tc si f8

f 26
sm This feature is the north baulk of k3. It is a volumetric feature, composed of natural accumulations. The baulk is one meter thick and 1.35 meters deep. The baulk is equivalent to features f3, f9, and f12. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features. 
A35 v8
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
rd S807

f 27
sm This feature is the east baulk of k3. It was excavated as a volumetric feature. It varies in width from 1-2 meters (as it bordered the large trench and was therefore irregular in shape) and is 1.35 meters deep. It is composed of natural accumulations. It is equivalent to features f3, f9 and f12 although we did not excavate by feature. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features.
el 9217 @top
el 9082 @bottom
A35 v18
df ld
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
rd S807

f 28
sm This feature is the north baulk of k4. It was excavated as a volumetric feature and it is 1 meter thick and 1.35 meters deep. It is composed of natural accumulations. It is equivalent to features f14, f17 and f20 although we did not excavate it by feature. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features.
A35 v10
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
rd S810

f 29
sm This feature is a floating stone in the east baulk of k2. It is 66cm across and 13cm high. It appears to be related to the other floating stones. 
A35 v22
rd S810
tc si f7


f 30
sm This feature is the east baulk of k5. Its width is irregular because it borders the large trench, k200. It varies it width but is 1.35 meters deep. It is composed of natural accumulations. This baulk is equivalent to features, f15, f16, f19 although we did not excavate by feature. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features.
A35 v19
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
rd S806

f 31
sm This feature is the north baulk of k5. It is 1 meter thick and 1.35 meters deep but k5 is very narrow so the total volume is smaller than the other baulks. The baulk is composed of natural accumulations and is equivalent to the features f15, f16 and f19 which are also natural accumulations. We did not excavate the baulk by separate features however, but as one large volumetric feature. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features.
A35 v10
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
rd S810

f 32
sm This feature is the east baulk of k4. Its width is irregular and it is 1.35m deep. This baulk is composed of natural accumulations. It is equivalent to the features f14, f17 and f20 although it was not excavated by feature but rather as one large volumetric feature. 
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features.
ad volumetric feature
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
A35 v20
rd S810

f 33
sm This feature is a baulk bordering the cement staircase. It was excavated as a volumetric feature and is not directly equivalent to any features although it covers the same depth as f15, f16, f19, and f42. It was an oblique cut and shaped like a triangle when viewed from the side. 
ds This feature was a baulk that bordered the cement staircase that was built in MZ20 by a team of workmen led by lC. The cement staircase was recorded as part of J2. This baulk was composed of natural accumulations and brickfall. A small border was still left next to the staircase (which was later removed in MZ22) to prevent erosion of the staircase.
sg This baulk was cut back to create a straight viewing line from the southern end of J7 to the monumental staircase. It was removed quickly as a large volumetric unit with only one q-lot. It was a conscious decision to value time over accuracy as we already had stratigraphically excavated features in k4 and k5 bordering this baulk. 
el 9238 @top
el 9018 @bottom
P99 S813
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
ha There are multiple elevations because this feature was cut to form an angle bordering the staircase. 

f 34
sm This feature is the east baulk of k1. It extends 500cm south of m4986 and 200cms east of the same marker. It is about 1.35 meters deep. It is composed of natural accumulations and is equivalent to the natural accumulations of f1, f8 and f10 although it was not excavated by individual feature. 
;lc k1
sg We did not excavate this baulk in features as we knew that all of these features were composed of indistinguishable natural accumulations. All of the pottery was collected together from the baulk, not separated by the features.
F99 Types of contact were not recorded for baulks as they were not excavated by feature but rather as large volumetric units. 
A35 v12
;el 9207 @top
;el 9072 @bottom
df ld
P99 S818
ad Volumetric feature

f 35
sm This feature is a large floating stone in the eastern baulk of k3. It is probably related to the other floating stones at similar elevations such as f25, f4, f5, f6, f38, f37, and f36. 
el 9154
nv Only one elevation was taken for floating stones. It is the elevation at the top. 
P99 S817
hd very hard

f 36
F99 Only one elevation was taken for floating stones. It is the elevation at the top. 
sm This feature is another large floating stone found in the east baulk of k3. It is probably related to the other floating stones at similar elevations such as f25, f4, f5, f6, f38, f37, and f35. 
el 9147
hd very hard
P99 S817
li This stone was not photographed as it was totally within the baulk and was removed as part of the baulk. It was relayed and its location is visible in p2 
A35 p2

f 37
sm This feature is a floating stone in the eastern baulk of k2. It is very large measuring 68x37cm. It is probably related to the other floating stones at similar elevations such as f25, f4, f5, f6, f38, f36, f39 and f35. 
A35 v22
hd very hard
tc si f7

f 38
F99 Only one elevation was taken for floating stones. It is the elevation at the top. 
sm This feature is a floating stone in the eastern baulk of k2. It is very large measuring 68x37cm. It is probably related to the other floating stones at similar elevations such as f25, f4, f5, f6, f37, f36, f39 and f35. 
el 9145
hd very hard
P99 S819
O99 This feature was only relayed and not photographed, as it was removed as part of the baulk. 
A35 p2

f 39
sm This feature is a large floating stone in the eastern baulk of k1. It is probably related to the other floating stones at similar elevations such as f25, f4, f5, f6, f38, f36, and f35. 
;el 9165 @top
;el 9144 @bottom
hd very hard
O99 This feature was only relayed and not photographed, as it was removed as part of the baulk. 
A35 p2

f 40
sm This feature is a floating stone in the eastern baulk of k1. It is probably related to the other floating stones at similar elevations such as f25, f4, f5, f6, f38, f36, and f35. 
O99 This feature was only relayed and not photographed, as it was removed as part of the baulk. 
hd very hard
A35 p2

f 41
sm f41 is a volumetric feature in the southern portion of k1. It was assigned to a new locus, k100, which is the area south of k1. Most of this feature was thrown down into k100 to create a viewing platform. This feature is composed of natural accumulations. This feature extends 150cms south of m4856 and 200cms to the east. 
ad ld
el 9079 @bottom

f 42
sm This volumetrically defined feature is partially composed of brickfall. Under the surface at elevation 9045 begins brickfall. This feature covers the whole locus extending 400cms South of m6027 and 145cms East. 
P99 S821
ad Volumetric feature
df bf

f 43
df bf
sm This volumetrically defined feature is composed of brickfall. The feature covers the whole locus extending 400cms north from m6028 and 270cms to the east. This feature is the beginning of the brickfall in k4. 
ds This feature is equivalent to the so-called dirty brickfall in J6 that slopes across the trench, k200. 
nv Although this feature was intended to be 50cm deep it is actually closer to to 1 meter. This was due to our desire to excavate quickly and work through the brickfall. Despite the large depth the feature is uniform brickfall. 
ad Volumetric feature

f 44
sm This feature is at the intersection of the natural accumulations and the brickfall. It is mostly natural accumulations. It is a volumetrically defined layer. 
el 8985 @ bottom
ha The lower bottom elevation is probably not correct based on the notes from the excavation so I have added the bottom elevation from the q-lot associated with this feature. 
sg After f44 had been excavated k3 was cut back one meter from the inside of trench k200. No features were assigned to that cleaning operation but ash and brickfall were seen in section. These are not assigned to f44, but rather were assigned feature numbers (f57 and f58) during the study season. They are directly below f44 although they were only exposed,  not excavated. 

f 45
pb This feature number was never assigned. 

f 46
sm This feature is composed of brickfall in k6. It is thinner than some of the other features because it was already cut down as part of J2. This feature covers the whole locus. 
ds This feature is equivalent to the so-called dirty brickfall in J6 that slopes across the trench, k200. 
sg k6 was originally part of J2 (formerly J2k4) but in order to completely remove the brickfall and create an even surface across the bottom of J7, k6 was added to J7 and excavated. We only removed the brickfall and stopped as soon as we reached floors. 
ad brickfall
tc co f51


f 47
sm This volumetrically defined feature is composed of brickfall. It covers the whole locus of k5 and is linked to the brickfall in J6 that crosses the trench, k200. 
ad brickfall
wm cl
P1 S819

f 48
sm This feature is a volumetric feature that was created to describe the trimming of the border of the cement staircase. It is composed of topsoil and natural accumulations and has no real stratigraphic significance. This feature is equivalent to f900 and the construction of the cement staircase in MZ20. 
sg This feature was part of the shaping and construction of the cement staircase. Once k5 was excavated there was a large portion of dirt still standing and it had to be cut down to match the slope of the staircase. It was not a stratigraphically important area but q-lots were kept. 
F99 Types of contact were not recorded for baulks and cleaning operations. 
O99 There are no views of this feature
li No elevations were taken for this feature. It is unclear if they were forgotten or if they were thought unnecessary for simple cleaning operations. 

f 49
el 8867 @bottom
sm This feature was a volumetrically defined layer composed entirely of brickfall. It covers the whole locus, k5, extending 400cms south from m6027 and 200cms to the east. It contained a partial human skull (i3) and a small cup (i2). It also has some unbaked bricks in it. It is the brickfall that slopes across the trench, k200 from J6. 
wm cl

f 50
el 8893 @bottom
sm This feature is a volumetrically defined layer composed entirely of brickfall. It covers the entire locus, k4, extending 400cms south from r38 and 250cms to the east. The brickfall is distinctive and contains some pieces of bricks as well as small items. 
wm cl
sg This was the last feature excavated in k4 and was excavated to a stopping point that would make it level with the other loci. 
ad brickfall
rd S807

f 51
=l f46
nr The jar rim was recovered during the winter of 2008 and was recorded as an item (i6) in 2009. 
ha This feature is the same as f46 based on elevations

f 52
sm This feature is the north baulk of k5. It was a very high baulk. The top portion was excavated with the big pick while the lower portion was more carefully excavated to recover any more bones that might be associated with the human skull. This feature is a mix of natural accumulations and brickfall. The baulk is 1 meter thick, extending 2 meters E-W and is 3 meters deep.
sg As it was one of the last features excavated during the season it had to be removed quickly and was thus taken down all as one piece rather than in smaller features. This resulted in a mixing of brickfall and natural accumulations but as we had the stratified deposits from k4 and k5 we did not think it was necessary to excavate the baulk in small sections. 
el 9080 @top
el 8780 @bottom
F99 No types of contact were assigned to large baulks as they were not excavated as stratigraphic units.
lc k5
df vm
ad mixed
pb At the end of MZ21 the records for this feature were lost. They have been reconstructed here from complimentary records such as q-logs, dailys and relays. 
A35 v31

f 53
lc k5
df vm
ad mixed
nv This feature extends 400cms south from m6027 and 100cms to the east. 
el 9077 @top
el 8777 @bottom
sm This feature was the west baulk of k5 where it bordered on the cement staircase that was constructed in MZ20. It is a mixed feature that is composed of both natural accumulations and brickfall. 
pb At the end of MZ21 the records for this feature were lost. They have been reconstructed here from complimentary records such as q-logs, dailys and relays. 
F99 No types of contact were assigned to large baulks as they were not excavated as stratigraphic units.
li There are no views of this feature. 

f 54
df vm
ad mixed
nv This feature extends 100cm west from m6005 and 100cms south
el 9077 @top
el 8777 @bottom
lc k3
sm This feature was a 1m x 1m baulk in k3. It was excavated as a volumetric feature down 3 meters. It is mixed accumulations of natural accumulations, brickfall and some ash at the bottom. 
pb At the end of MZ21 the records for this feature were lost. They have been reconstructed here from complimentary records such as q-logs, dailys and relays. 
F99 No types of contact were assigned to large baulks as they were not excavated as stratigraphic units.

f 55
df vm
ad mixed
lc k3
nv This feature extends 200cms east of m6028 and 100cms south
el 9077 @top
el 9042 @bottom
pb At the end of MZ21 the records for this feature were lost. They have been reconstructed here from complimentary records such as q-logs, dailys and relays. 
F99 No types of contact were assigned to large baulks as they were not excavated as stratigraphic units.
sm This feature is a small portion of the north baulk of k3. It was the portion remaining above where we stepped the loci in to save time in order to reach the bottom before the end of the season. It is at the beginning of the brickfall in k3 by elevation but it not certain to be only composed of brickfall so it is listed as mixed. It is probably a mixture of the level where f12 and f44 meet. 
A35 v42
rd S807

f 56
df vm
ad mx
lc k4
el 9079 @top
el 8729 @bottom
nv This feature extends 100cms north of r38 and 30cms to the east. 
pb At the end of MZ21 the records for this feature were lost. They have been reconstructed here from complimentary records such as q-logs, dailys and relays. 
F99 No types of contact were assigned to large baulks as they were not excavated as stratigraphic units.
sm This feature is the large northern baulk of k4. It is 1m by 3.5 meters thick and it is 3 meters deep. It was excavated as one volumetric feature and therefore is mixed natural accumulations and brickfall. 
sg As it was one of the last features excavated during the season it had to be removed quickly and was thus taken down all as one piece rather than in smaller features. This resulted in a mixing of brickfall and natural accumulations but as we had the stratified deposits from k4 and k5 we did not think it was necessary to excavate the baulk in small sections. 

f 57
df bf
lc k3
ds Brickfall layer seen in western section of k3. It has clearly articulated red and gray bricks. It was discovered during a cleaning operation. This feature was only exposed, not excavated. It covers a thick layer of ash (f58). 
sg After k3 had been finished being excavated during the 2008 season gB wanted to cut back k3 by one meter from inside k200. As this was considered a cleaning operation of the trench no features were assigned. In the study season of 2010 it became necessary to refer to the brickfall and ash seen in this section and so feature numbers were assigned. As these features were only identified in the cleaning of the section they have only been exposed, not excavated.  
tc co f58
A35 v29

f 44
tc co f57

f 58
df ly
ad ash
lc k3
ds Thick ash layer seen in western section of k3. It has a yellowish tint in some places. It ranges from 20-50cm in thickness. It slopes from the south to the north. This feature was only exposed, not excavated. 
sg After k3 had been finished being excavated during the 2008 season gB wanted to cut back k3 by one meter from inside k200. As this was considered a cleaning operation of the trench no features were assigned. In the study season of 2010 it became necessary to refer to the brickfall and ash seen in this section and so feature numbers were assigned. These features were identified in section and have not been excavated. 
A35 v29

.ri cJC
.rd U818

v 37
ds This view shows the west section of k3 after it had been cut back and cleaned. Both brickfall and ash were very clearly articulated. Features were assigned to the brickfall and ash seen in this section although these features were only exposed, not excavated. These features are now f57 and f58. 

v 37a
ds This view shows the southwest corner of k3 after it had been cut back and cleaned.  Both brickfall and ash were very clearly articulated. Features were assigned to the brickfall and ash seen in this section although these features were only exposed, not excavated. These features are now f57 and f58.