DEGREE. 
' ‘ Angles 
oo Names of Stations, oS Diff. alae Error. 4 correéted for | Diftances. 
§ Brees ee Calculation. 
XVIII Hollan-hill oer 5 : ; oac 1 
XVIII. | ollan-hi! - ~ 44 43 32 — 44 4$ 3t 
Sutton-A fhfield - (13 49 "9 —0.53 113 si . 
rpit - 21 247 20.5 | —o.1 21 27 22 
180 oO 7 +0. ag 
Hollan-hill fom SsstoonA thfield . 38375.2 
Orp : . : 95975+3 
XIX. Bardon-hill - 42 58 59.5 | —0.69 42 58 59 
Hollan-hill - 74 52 38 —1.93 74 52 34 
Orpit - 62 8 25 =Si.61 62 8 24 
180 0 2 45 — 0.20 
Bardos-hill from {Onn lan-bil ° ° ipa 
- ~ r 13 5895.3 
XX. Caftle-ring - 55 32 44 —0.94 2 4 
Bardon-hill - 68 of 455 me 23 : 
Orpit - 56 3 ae —0.90 56 3 14 
180 O 3.5 85 | +0.65 
; : - - 153235.2 
Caftle-ring from {Bee a. hill - ° ee 
XXI1. Corley - 72 32 46.5 | —1.19 42 32 46 | 
Caftle-ring - 47 $4 42.25| —0.86 47 54 42 
Bardon-hill : 59 32 32.25] —0.94 59 32 32 
1180 Oo 1 | — ni —1.93 hoe 
ardon-nl - 10635763 
oney ae { Caitlesting ~ - 1235307 
XXIL. | Arbury-hill : 34 I4 33-5 | —0.98 | 34 14 33 
| Corley 107 20 14.25] —1.99 f , 107 20 14 
Bardon-hill - g8 25 13.25| —o.80 5 13 
0 0 1 | : oi 2.37 1 ae, P 
Arbury-hill F sardon-hi “. '1804.26.0 
rbury-hil from Corley : . rr745 7% 
Calculation of the Meridien aid between Dunnofe and Feet Miles. 
The bearings of certain fo from the parallels to the me- 
ridian of Dunnofe, by obfervations of the poie-ftar at Dun- 
rofe. 
Dunnofe and Butfer-hill 
Brill and Arbury-hill 
131,263.0 = 24.86 
0 
Dunnofe and Butfer-hill - 20 58 39 N.E. Arbury-hill and Bardon-bil a ea 4 me 86 
AEA ori - 34 20 17 N.E. Bardon-hill and Or 126.567.8 = ie 
ighclere an - 35 30 4o N.E. Orpit and Heathe rfed dp 15203 7 = 19.17 
Sea : i 7 - - 4.55 25 ae Heatherfedge and Beconsill: i 480.7 = 8.23 
ruil an rDbury- 44 - I2 30 17 IN-W. 
Arbury-hill and Bardon-hill 57 N.W. a6, 
don- 334 = 196.27, the 
Omies ye obdge 2 ; 9 ea diftance between Clifton ant ae to the me 
Heatherfed geand Bemon-hill 2 e 4 ; NE. ridian of Dunnofe, which may be taken for the true length 
e bearings, and 
Rrz2 
of the arc itfelf, as the di age of the al ftation from 
Thefe their refpeCiive fides, give the fol- the meridian of the latter is only 4779 fee 
lowing diftances on the meridian of Dunnofe. 
Bearings 
