1971-80 |
Musgrave Row |
TN |
Cup |
|
1 |
(Rigby 1991, 77). An unusual TN cup (Bidwell 1979, fig. 69.247). Thin sectioning shows abundant grains of quartz in two size grades. Also present are smaller fragments of sandstone, quartzite and mica. Since other examples of this form have been identified at Winchester and Chichester a continental source is likely. |
|
1971-80 |
Musgrave Row |
TN |
Cup |
|
1 |
(Rigby 1991, 77). An unusual TN cup (Bidwell 1979, fig. 69.247). Thin sectioning shows abundant grains of quartz in two size grades. Also present are smaller fragments of sandstone, quartzite and mica. Since other examples of this form have been identified at Winchester and Chichester a continental source is likely. |
|
1971-80 |
All contexts |
TN |
Cam 8 |
|
5 |
(Rigby 1991, 77) |
|
1971-80 |
All contexts |
TN |
Cam 8 |
|
5 |
(Rigby 1991, 77) |
|
1971-80 |
GS 41-48-16 |
TN |
Cam 8 |
716 |
1 |
(Rigby 1991, 76). |
|
1971-80 |
GS 41-48-16 |
TN |
Cam 8 |
716 |
1 |
(Rigby 1991, 76). |
|
1971-80 |
All contexts |
TN |
Cam 16 |
|
53 |
(Rigby 1991, 77) |
|
1971-80 |
All contexts |
TN |
Cam 16 |
|
53 |
(Rigby 1991, 77) |
|
1971-80 |
FH81 L1123 |
TN |
Cam 16 |
661 |
1 |
(Holbrook & Bidwell 1992, fig. 7.1). |
|
1971-80 |
FH81 L1123 |
TN |
Cam 16 |
661 |
1 |
(Holbrook & Bidwell 1992, fig. 7.1). |
|
1971-80 |
LCS 90 333 |
TN |
Cam 16 |
615 |
1 |
|
|
1971-80 |
LCS 90 333 |
TN |
Cam 16 |
615 |
1 |
|
|
1971-80 |
NP 83 115 |
TN |
Cam 16 |
660 |
1 |
|
|
1971-80 |
NP 83 115 |
TN |
Cam 16 |
660 |
1 |
|
|
1971-80 |
All contexts |
TN |
Cam 2 |
|
1 |
(Rigby 1991, 77) |
|
1971-80 |
All contexts |
TN |
Cam 2 |
|
1 |
(Rigby 1991, 77) |
|
1971-80 |
All contexts |
TN |
Cam 46 |
|
1 |
(Rigby 1991, 77) probably Cam. 46 |
|
1971-80 |
All contexts |
TN |
Cam 46 |
|
1 |
(Rigby 1991, 77) probably Cam. 46 |
|
1971-80 |
All contexts |
TN |
Cam 58 |
|
11 |
(Rigby 1991, 77) |
|
1971-80 |
All contexts |
TN |
Cam 58 |
|
11 |
(Rigby 1991, 77) |
|
1971-80 |
MM71 MVI+ DWMP 67 |
TN |
Cam 58 |
885 |
1 |
|
|
1971-80 |
MM71 MVI+ DWMP 67 |
TN |
Cam 58 |
885 |
1 |
|
|