214 Raleigh's Tyfoon of 1835. 
~ 
4. That the violence of the wind was apperenily greater with 
the Raleigh, than with the ea. Hayes. 
nt’ 
T 
aged track of Leva 
mass ls * 
a5 | is 
3 . cd 
- Supp 
5h ae Ua cede natehet 
‘6th 
4th |Aug. 
i 
— 
S aia ee oe : 
5 "Phat the gale was Serine ee an English schooner, 
Aug. 5th, in lat. 18° 2’ N. lon. 115° 50’ E.; but the Levant, arri- 
ving on the 7th, in her course through the ‘Chines sea, did not eu- 
counter the gale. 
6. That the fall and rise of the habbit at Macao, and with 
the Raleigh, and the strength and changes of wind with the latter, 
were such as are often exhibited near the centre of a hurricane ; 
and that the minimum depression of the barometer occurred about 
seventeen hours later at Macao, than with the Raleigh. 
These facts seem to establish the following conclusions: 
1. ‘That the Tyfoon advanced in a westerly direction. 
2. Negatively ;—that it did not pass through the China sea, from 
_N. E. to 8. W., nor on the opposite of this course. 
