132 
DEG 
DEL 
Tranf. 
AbricD. f 
— — - Account of the horn of a large deer found in 
the heart of an oak - Clark 
XLI235 
! 
VIII 847 1 
- An account of two extraordinary deers horns, 
found under ground in different parts of York- 
fhire - - Know It on 
XLIV 124 
| 
X601 
Degree. Letter concerning a place in New York 
for meafuring a degree of latitude Alexander 
XLI 38 3 
f' 
i 
] 
— Propofai of a method for meafuring degrees of 
longitude upon parallels of the equator AUtchell 
LVI 1 19 
j 
Letter containing a fhort account of the mea- 
furement of three degrees of latitude under 
the meridian of Vienna - Liefganig 
LVIII 15 
-- Introduction to the following obfervations made 
by Ch. Mafon and Jer. Dixon, for determin- 
ing the length of a degree of latitude in the 
provinces of Maryland and Pennfylvania, in! 
North America - Mafielyne 
• — 270 
Obfervations, &c. Mafon and Dixon 
— 274 j 
Length of a degree of latitude in the provinces 
of Maryland and Pennfylvania, deduced from 
the obfervations of Meff. Mafon and Dixon 
- - Mafkeiyne 
— 323 
• 
■ * Kepler’s method of computing the moon’s pa- 
rallaxes in folar eclipfes, dernonftrated and ex- 
tended to all degrees of the moon’s latitude ; 
as alfo to the aligning the moon’s correfpon- 
dent apparent diameter : together with a con- 
cife application of this form of calculation to 
thofe eclipfes - - Pemberton 
LXI437 
Delgovicia. Extrad of a letter concerning the fi- 
tuation of the antient town Delgovitia 
- - Knowlton 
XLIV 100 
XI 1245 
A differtation on the fituation of the antient 
Roman ftation of Delgovitia in Yorkfhire 
- Burton 
— 541 
— 1246 
Delirium. Account of one who had no ear to mu- 
lic naturally, Tinging feveral tunes when in a 
delirium - - Doddridge 
— 596 
X 1084 
Cafe of the efficacy of bark in the delirium of a 
fever - - Munckley 
L 609 
Deluge. Some confiderations about thecaufe of the 
univerfal deluge - Halley 
XXXIII 118 
VI 2 I 
Some further thoughts on the fame Halley 
— 123 
4 
An extraCl of a philofophical account of a new 
opinion concerning the origin of petrefaCtions 
found in the earth, which has hitherto been 
afcribec 
