OH02f0001 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^plow A20 I705-I714JL.J !! bu A20 I708-I708JLW.J !! bu A21 I705-I714JL.J jl ts A21 I708-I708JLW.J jw ts A35 V825-V817CJC.J cjc v4 B11 I708-I708JLW.J jw surface soil layer approximately 10 cm deep. D01 I705-I714JL.J jl k1 D06 V908-V908CJC.J cjc 7847 @bottom D06 V908-V908CJC.J cjc 7857 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. F02 >co f0002 I712-I712JLW.J gb I01 V827-V827CJC.J cjc s20-OH2 I03 V827-V827CJC.J cjc h9m-OH2 K05 I708-I708JLW.J jw pale brown K06 I708-I708JLW.J jw 10YR6/3 K08 I708-I708JLW.J jw fine and dusty with considerable vegetative matter. O01 v0001 I705-I714JL.J jl O01 v0001a I705-I714JL.J jl O01 v0001b I705-I714JL.J jl O01 v0002 I707-I714JL.J jl O01 v0002a I707-I714JL.J jl O01 v0003 I707-I714JL.J jl O01 v0004 I707-I714JL.J jw O01 v0005 I713-I714JL.J jw O01 v0008 I714-I714JL.J jl O01 v0008a I714-I714JL.J jl O01 v0009 I714-I714JL.J jl O01 v0009a I714-I714JL.J jl O01 v0010 I714-I714JL.J jl O01 v0011 I714-I714JL.J jl O01 v0012 I714-I714JL.J jl O01 v0013 I714-I714JL.J jl O01 v0014 I714-I714JL.J jl O01 v0015 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0003 O03 V823-V817CJC.J cjc w0004 O03 V823-V817CJC.J cjc w0005 O03 V823-V817CJC.J cjc w0006 OH02f0002 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^plow A20 I705-I714JL.J !! of A20 I708-I708JLW.J !! of A21 I705-I714JL.J jl so A21 I708-I708JLW.J jw so A35 V825-V817CJC.J cjc v4 B11 I708-I708JLW.J jw soil immediately below surface soil, approximately 20 cm deep. C01 I705-I706JLW.J jw mKB examined the pottery, which contained one decorated sherd. Most of the sherds could tentatively be attributed to the third millennium. There is a third millennium cemetery to the south of where we are now digging, a third millennium house was partially excavated on the main tell, and Ninevite V sherds have been found in excavations for our own well and for a buried power cable. mKB reminds us that Urkesh was an early third millennium city. She showed examples of decorated bowls, large and small cups with pointed bases, and stands with cutouts or painted designs. D01 I705-I714JL.J jl k1 D06 I705-I714JL.J jl 0 @top D06 V908-V908CJC.J cjc 7827 @bottom D06 V908-V908CJC.J cjc 7847 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. F02 co f0003 I712-I712JLW.J gb I01 V827-V827CJC.J cjc s20-OH2 I03 V827-V827CJC.J cjc h9m-OH2 K05 I708-I708JLW.J jw dark yellowish brown K06 I708-I708JLW.J jw 10YR4/4 K08 I708-I708JLW.J jw compacted, but not easily penetrated by pick. Some laminations, perhaps as the result of plowing. O01 v0002 I707-I714JL.J jl O01 v0002a I707-I714JL.J jl O01 v0003 I707-I714JL.J jl O01 v0004 I707-I714JL.J jw O01 v0005 I713-I714JL.J jw O01 v0008 I714-I714JL.J jl O01 v0008a I714-I714JL.J jl O01 v0009 I714-I714JL.J jl O01 v0009a I714-I714JL.J jl O01 v0010 I714-I714JL.J jl O01 v0011 I714-I714JL.J jl O01 v0012 I714-I714JL.J jl O01 v0013 I714-I714JL.J jl O01 v0014 I714-I714JL.J jl O01 v0015 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0003 O03 V823-V817CJC.J cjc w0004 O03 V823-V817CJC.J cjc w0005 O03 V823-V817CJC.J cjc w0006 OH02f0003 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^plow A20 I705-I714JL.J !! of A20 I708-I708JLW.J !! of A21 I705-I714JL.J jl so A21 I708-I708JLW.J jw so A35 V825-V817CJC.J cjc v4 B11 I708-I708JLW.J jw soil immediately below soil f2. Uniform in color and texture. C01 I708-I708JLW.J jw almost impossible to differentiate f2 and f3 in baulk. f3 soil has vertical laminations and is similar to soil from south well (OP2k1f1) being excavated privately and monitored by us. D01 I705-I714JL.J jl k1 D06 I705-I714JL.J jl 35 @top D06 V908-V908CJC.J cjc 7757 @bottom D06 V908-V908CJC.J cjc 7827 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. F02 co f0004 I712-I712JLW.J gb F02 >co f0012 I716-I716JLW.J gb I01 V827-V827CJC.J cjc s20-OH2 I03 V827-V827CJC.J cjc h9m-OH2 K05 I708-I708JLW.J jw dark yellowish brown K06 I708-I708JLW.J jw 10YR4/4 K08 I708-I708JLW.J jw compacted and clumped more than f2, but the same color. O01 v0002 I707-I714JL.J jl O01 v0002a I707-I714JL.J jl O01 v0003 I707-I714JL.J jl O01 v0004 I707-I714JL.J jw O01 v0005 I713-I714JL.J jw O01 v0008 I714-I714JL.J jl O01 v0008a I714-I714JL.J jl O01 v0008c I714-I714JL.J jl O01 v0009 I714-I714JL.J jl O01 v0009a I714-I714JL.J jl O01 v0010 I714-I714JL.J jl O01 v0011 I714-I714JL.J jl O01 v0012 I714-I714JL.J jl O01 v0012a I714-I714JL.J jl O01 v0013 I714-I714JL.J jl O01 v0014 I714-I714JL.J jl O01 v0015 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0003 O03 V823-V817CJC.J cjc w0004 O03 V823-V817CJC.J cjc w0005 O03 V823-V817CJC.J cjc w0006 OH02f0004 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^accum A20 I709-I714JL.J !! bu A20 I711-I712JLW.J !! bu A21 I709-I714JL.J jl ac A21 I711-I712JLW.J jw ac A35 V825-V817CJC.J cjc v8 B11 I708-I707GB.J gb A very clear differentiation occurred between a heavy granular, and a soft greasy soil, with pockets of ash, and greater concentration of sherds. This look like some accumulation, though we do not have any boundaries (such as walls) that contain it. B11 I709-I709JLW.J gb a white band across k1 running NS in the middle of the locus gave the impression of being a wall. jW pointed out that it may be instead the differential color matching the line where excavations stopped yesterday. As a result, we do not assign a separate feature number to it. q9 contains sherds from this white band and east of it; q8 contains sherds from west of white band. B11 I711-I712JLW.J jw grayish brown hard-packed accumulation across entire locus. Powdery residue after scraping, but the surface is greasy when scraped, perhaps from the presence of organic material . Very clear dividing line between soil f3 and this feature, which seems to demarcate the lower limits of plowing. C02 I708-I707GB.J gb We will switch to small picks, and possibly we may have to sift as well, since the sealings are very small. If so, we will need to put up a tent. D01 I709-I714JL.J jl k1 D06 I709-I714JL.J jl 100 @top D06 V908-V908CJC.J cjc 7717 @bottom D06 V908-V908CJC.J cjc 7757 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. F02 co f0005 I712-I712JLW.J gb I01 V827-V827CJC.J cjc s610-OH2 I03 V827-V827CJC.J cjc h3u-OH2 K05 I711-I712JLW.J jw yellowish brown K06 I711-I712JLW.J jw 10YR5/4 M01 I708-I707GB.J gb The presence of some clay lumps is extraordinary: it clearly appears to be sealings suggests that they were dumped originally in this place: were they dumped from a single source "intra muros", or were they used and discarded here? O01 v0003 I707-I714JL.J jl O01 v0004 I707-I714JL.J jw O01 v0005 I713-I714JL.J jw O01 v0008 I714-I714JL.J jl O01 v0008a I714-I714JL.J jl O01 v0008c I714-I714JL.J jl O01 v0009 I714-I714JL.J jl O01 v0009a I714-I714JL.J jl O01 v0010 I714-I714JL.J jl O01 v0011 I714-I714JL.J jl O01 v0012 I714-I714JL.J jl O01 v0012a I714-I714JL.J jl O01 v0013 I714-I714JL.J jl O01 v0014 I714-I714JL.J jl O01 v0015 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0003 O03 V823-V817CJC.J cjc w0004 O03 V823-V817CJC.J cjc w0005 O03 V823-V817CJC.J cjc w0006 OH02f0005 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^accum A20 I709-I711JLW.J !! no ct A20 I709-I714JL.J !! bu A21 I709-I711JLW.J jw subfloor A21 I709-I714JL.J jl ac A35 V825-V817CJC.J cjc v8 B11 I709-I711JLW.J jw noticed a difference in soil texture as west half of k1 was scraped. Soil surface hard with small reddish pockets in tan base as compared with greasy uniform red-brown surface of accumulation of f4. First pick run yielding less pottery than in f4. Also, fewer charcoal pockets. B11 I711-I711JLW.J gb the decreasing number of sherds and inclusions may support the interpretation as a subfloor. C01 I711-I712JLW.J jw as excavation proceeds, subfloor material becoming moist and sticky. Several pieces of creamy-white plaster appearing along south baulk. C02 I711-I711JLW.J gb we go down 25cms within f5: I have alerted workmen to look for possible changes, so they woould stop before the 25 cms if necessary. D01 I709-I714JL.J jl k1 D06 I709-I714JL.J jl 130 @top D06 V908-V908CJC.J cjc 7677 @bottom D06 V908-V908CJC.J cjc 7717 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. F01 I711-I711JLW.J gb occasional lines, as if brick faces, but no clear homogeneous face as if for a wall, nor convincing mortar joins. F02 co f0008 I712-I712JLW.J gb F02 >co f0009 I712-I712JLW.J gb I01 V827-V827CJC.J cjc s611-OH2 I03 V827-V827CJC.J cjc h3u-OH2 K05 I709-I711JLW.J jw dark yellowish brown K05 I711-I711JLW.J gb reddish brown K05 I711-I712JLW.J jw dark brown K06 I709-I711JLW.J jw 10YR4/4 K06 I711-I712JLW.J jw 7.5YR4/4 K08 I711-I711JLW.J gb granular and scaly as if from mud brick M01 I711-I711JLW.J gb possible a subfloor; if so, it is strange that we should hav missed the floor surface, which one would expect to be strongly marked if such a good subfloor was made for it. A floor surface does not appear in the section either, but the distinction between accumulation on f4 and "subfloor" of f5 is very clear in the section. O01 v0004 I707-I714JL.J jw O01 v0005 I713-I714JL.J jw O01 v0008 I714-I714JL.J jl O01 v0008a I714-I714JL.J jl O01 v0008c I714-I714JL.J jl O01 v0009 I714-I714JL.J jl O01 v0009a I714-I714JL.J jl O01 v0010 I714-I714JL.J jl O01 v0011 I714-I714JL.J jl O01 v0012 I714-I714JL.J jl O01 v0012a I714-I714JL.J jl O01 v0013 I714-I714JL.J jl O01 v0014 I714-I714JL.J jl O01 v0015 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0003 O03 V823-V817CJC.J cjc w0004 O03 V823-V817CJC.J cjc w0005 O03 V823-V817CJC.J cjc w0006 O03 V823-V817CJC.J cjc w0007 OH02f0006 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A20 I710-I714JL.J !! of A20 I712-I712JLW.J !! of A21 I710-I714JL.J jw ho A21 I712-I712JLW.J jw ho B11 I712-I712JLW.J jw vertical hole from tap root of plant. Dark organic material in hole averaging 2-4 cm in diameter. Originally, I thought it was a post hole until I saw part of root. D01 I710-I714JL.J jw k1 D03 I720-I720JLWR.J jw 10 (91970 90141 - 7695) D06 I710-I714JL.J jw 0 @top D06 V908-V908CJC.J cjc 7695 D99 V908-V908CJC.J cjc There is only one elevation for this feature that was taken when the feature was relayed. F02 >cu f0004 I712-I712JLW.J gb F02 >cu f0005 I712-I712JLW.J gb F02 >in f0008 I712-I712JLW.J gb I01 V827-V827CJC.J cjc s30-OH2 I03 V827-V827CJC.J cjc h9m-OH2 OH02f0007 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A20 I710-I714JL.J !! of A20 I712-I712JLW.J !! of A21 I710-I714JL.J jw rh A21 I712-I712JLW.J jw rh B11 I712-I712JLW.J jw oblique hole about 50 cm long which began at a stone and rambled in a generally SW direction. Diameter about 5 cm. D01 I710-I714JL.J jw k1 D03 I720-I720JLWR.J jw 12 (91832 89928 - 7672) D06 I710-I714JL.J jw 0 @top D06 V908-V908CJC.J cjc 7672 D99 V908-V908CJC.J cjc There is only one elevation for this feature that was taken when the feature was relayed. F02 >in f0005 I712-I712JLW.J gb I01 V827-V827CJC.J cjc s30-OH2 I03 V827-V827CJC.J cjc h9m-OH2 OH02f0008 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^lam A20 I710-I714JL.J !! bu A20 I711-I712JLW.J !! no ct A21 I710-I714JL.J jw lm A21 I711-I712JLW.J gb laminations A35 V825-V817CJC.J cjc v14 B11 I712-I712JLW.J gb at the end of the day, beginning to see more inclusions, namely plaster chunks, charcoal lumps and whitish stones (one group of 4). Generally laminations are still showing up across the entire north half of k1. Relatively clear transition between f5 fill and f8 laminations in baulk. B11 I713-I714JLW.J jw scraped after first pick run. General conditions noted today by gB still apply. More charcoal flakes and more stones are evident. Stones are concentrated in NE corner and in region to south of pedistaled stones. Laminations present in all parts of N half of square. B11 I713-I714JLW.J jw scraped after second pick run. The consistency and texture of the laminations began to change, particularly in the western part. Soil became more powdery and took on a more reddish hue. Also somwhat drier. Laminations still clearly evident. B11 I713-I714JLW.J jw the pile of six stones seems to have been placed rather than randomly deposited. B11 I714-I714JLW.J gb inspected excavated area after final cleanup. f8 seems to consist of three more or less equal sections. f9 imbedded in f8 in the eastern third. The separation is still distinct, although the dimensions and orientaion are somewhat altered. In the eastern third, there is a dark area, not yet well defined, which resembles f10 in color and inclusions (eg. charcoal). The middle third is bounded by f11 on the north and contains a line of stones extending south to the unexcavated platform of f8 material in the south half of k1. It appears as if this center section may have bisected two areas of similar use, but it would take several more pick runs to test this hypothesis. The north face of the platform did not show these demarcations, nor did it show any evidence of horizontal separations that might have been associated with a floor. A significant amount of pottery, bone and two possible seal impressions were found in the west part, matching previous experiences. C01 I712-I712JLW.J jw soil in northeast quadrant beneath f5 continues to show clear evidence of laminations and moisture retention noted by GB on I711. Residue after scraping resembles chocolate shavings. Surface extremely greasy, making it difficult to cut with a trowel. C02 I712-I712JLW.J gb We consider f8 to extend across the entire North sector of k1, and continue digging across this sector, trying to rach a lower definition of these laminations. C02 I713-I714JLW.J gb we continue digging across northern half of k1, assuming uniformity of deposition (f8). The goal is to find som definition at the bottom which would provide an excellent stopping point for this operation (especially since as of tomorrow the workmen will be needed elsewhere - B6-B7). C02 I713-I714JLW.J jw we will pedistal the stones as we excavate, only in order to retain a point of reference. C04 I711-I712JLW.J gb I scraped after workmen did a careful cleaning. Soil flakes off very neatly, but shows neither a consistent slope nor strong compaction from above. It is very moist. C04 I712-I712JLW.J gb I inspected carefully the portion exposed (North half of k1) and concluded tht we have a uniform set of laminations across the part exposed. Material flakes off in fairly uniform, wide scales, which are rather soft and leave a fairly well-marked surface. However, neither does any portion of the surface extend very far, nor is there any indication of compaction. D01 I710-I714JL.J jw k1 D06 I710-I714JL.J jw 0 @top D06 V908-V908CJC.J cjc 7637 @bottom D06 V908-V908CJC.J cjc 7677 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. E01 I714-I714JLW.J gb the alignment of inclusiions was never clear while digging, except for patches of stones and sometimes the patches of gypsum flecks. But the sections show a clear horizontal alignment both E-W and N-S. There seems to be, however, a rise to the East, which was noted while excavating, and which shows clearly in N8. F02 co f0010 I715-I715JLW.J jw F02 >co f0011 I715-I715JLW.J jw H99 I711-I712JLW.J gb I assume this is the the result of water sitting within a bowl-like setting, hence giving evidence, in my estimation, of abandonment. Jim reminds me that laminations suggest containment; in this case this would possibly entail the presence of partially collapsed walls within which the settling of the water would have occurred. H99 I714-I714JLW.J gb U assume that the rise to the east is part of a general ridge which somehow delimits ane contains f5 (the subfloor). The western edge of this limit ought to be a structure hidden under the toplogical rise shown in v6. If so, the rise to the East of f8 represents some preexisting mass (a decomosed wall? a simple berm?) which retained water and dissolved itself into laminations. I01 V827-V827CJC.J cjc s630-OH2 I03 V827-V827CJC.J cjc h3p-OH2 K05 I711-I712JLW.J gb brown K05 I712-I712JLW.J jw dark brown K06 I712-I712JLW.J jw 7.5YR4/3 K08 I711-I712JLW.J gb thick flakes, very plastic, meaning that it congeals easily. K08 I713-I714JLW.J gb I picked, scraped and brushed the surface exposed in No. half of k1 (right after taking pictures for v5). The Eastern portion is harderand drier (and dryness does not seem to be a correlative of excavation times; in other words, there may be a real difference between E and W. Yet, it is not marked enough, nor is there any observable boundary between the two, to allow us to establish a new feeature(though it would match what was observed at a higher elevation between f9 and f8). In the West, the material is more granular and greasy, while in the East it remains scaly and flaky. M01 I713-I714JLW.J gb the general concentration of finds to the West suggests, perhaps, that we have the tail end of a deposit linked with a structure to the West, which is presumably hidden under the rise visible on the surface (see v6). M01 I714-I714JLW.J gb stones, laminations support outdoor area, possibly in front(E) of building. But no trash decomposing, since deposit is very clear. O01 v0005 I713-I714JL.J jw O01 v0005a I713-I714JL.J jw O01 v0005b I713-I714JL.J jw O01 v0007 I713-I714JL.J jw O01 v0008 I714-I714JL.J jl O01 v0008a I714-I714JL.J jl O01 v0008b I714-I714JL.J jl O01 v0008c I714-I714JL.J jl O01 v0009 I714-I714JL.J jl O01 v0009a I714-I714JL.J jl O01 v0010 I714-I714JL.J jl O01 v0010a I714-I714JL.J jl O01 v0011 I714-I714JL.J jl O01 v0011a I714-I714JL.J jl O01 v0012 I714-I714JL.J jl O01 v0012a I714-I714JL.J jl O01 v0013 I714-I714JL.J jl O01 v0014 I714-I714JL.J jl O01 v0015 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0003 O03 V823-V817CJC.J cjc w0004 O03 V823-V817CJC.J cjc w0005 O03 V823-V817CJC.J cjc w0006 O03 V823-V817CJC.J cjc w0007 OH02f0009 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^lam A20 I710-I714JL.J !! bu A20 I712-I712JLW.J !! bu A21 I710-I714JL.J jw ac A21 I712-I712JLW.J jw ac A35 V825-V817CJC.J cjc v12 B11 I712-I712JLW.J gb could not find any evidence of f9 in baulk between f5 and f8. I conclude that the small differences between f8 and f9 in my initial observations were caused by variations in retained moisture. B11 I712-I712JLW.J gb upon inspection, it does not differ signficantly from laminations f8. B11 I712-I712JLW.J jw accumulation below f5 in NW quadrant. Wetter and more greasy than f5 fill, with no inclusions of gray or red material. Drier than f8 laminations. Greasy surface, but scraping residue is powdery, compared with chocolate shaving residue of f8. Seems to be a clear demarcation between f8 and f9 down middle of square. D01 I710-I714JL.J jw k1 D06 I710-I714JL.J jw 0 @top D06 V908-V908CJC.J cjc 7667 @bottom D06 V908-V908CJC.J cjc 7677 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. F02 ov f0008 I712-I712JLW.J gb I01 V827-V827CJC.J cjc s630-OH2 I03 V827-V827CJC.J cjc h3p-OH2 K05 I712-I712JLW.J jw brown K06 I712-I712JLW.J jw 7.5YR5/4 O01 v0008 I714-I714JL.J jl O01 v0008a I714-I714JL.J jl O01 v0009 I714-I714JL.J jl O01 v0012 I714-I714JL.J jl O01 v0012a I714-I714JL.J jl O01 v0014 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0003 O03 V823-V817CJC.J cjc w0004 OH02f0010 File processed on 08-25-2016 - Source Files: ; Q8252038.E.E - Standards: ; A03 V817-V817CJC.J cjc ^collapse A20 I713-I714JL.J !! bu A20 I713-I714JLW.J !! no ct A21 I713-I714JL.J jw lm A21 I713-I714JLW.J jw lamination A35 V825-V817CJC.J cjc v14 B11 I713-I714JLW.J jw dark soil patch NE corner of k1. Patch is eliptical with long axis 110 cm running N-S. One end of the long side touches the east baulk. The short axis is 70 cm. One end of the short side touches the north baulk. Soil within is Munsell 7.5YR4/3, dark brown. Surrounding soil is Munsell 7.5YR4/6, strong brown. A few red streaks run more or less vertically through the feature. Some charcoal bits and fist-sized stones also inside. B11 I715-I715JLW.J jw see Sketch 5 for approximate location. D01 I713-I714JL.J jw k1 D06 I713-I714JL.J jw 0 @top D06 V908-V908CJC.J cjc 7642 @bottom D06 V908-V908CJC.J cjc 7647 @top D99 V908-V908CJC.J cjc The original elevations were measured from the surface down and appear in the record with these numbers. In 2011 cJC used the absolute elevation of m1869 which was located on the surface near OH2 to convert these measurements. F02 co f0004 I716-I716JLW.J gb I01 V827-V827CJC.J cjc s20-OH2 I03 V827-V827CJC.J cjc h9m-OH2 K05 I716-I716JLW.J gb reddish, but less so than f3. K05 I720-I721JLW.J jw light brown K06 I720-I721JLW.J jw 7.5YR6/4 K08 I716-I716JLW.J gb granular O01 v0008c I714-I714JL.J jl O01 v0010 I714-I714JL.J jl O01 v0012a I714-I714JL.J jl O01 v0013 I714-I714JL.J jl O03 V823-V817CJC.J cjc w0004 O03 V823-V817CJC.J cjc w0005 O23 I716-I716JLW.J gb C5407 taken by GB with hand camera to show scoring of f12 and rodent holes. Look SW at corner of Southern and Western baulks.