M peak of tekeiuite. 51 
morning, 74° j at six in the 
mornitfg 42<> ^ i at one, in the following 
<he bottom nc’.i^ Past four, 32®; at 
•>our and a half a*1 ^"P °“® 
Eone is diffirnU f sun-use, 33''. I'hc descent down the 
of w'c S f'-o™ the fall 
pumi “e. Haviiw an' themselves from the beds of 
sued our marcl dnf "u to the bottom, we pur- 
tosay.l™"' of tl'o lava, that is 
The ravines -ind r. having ascended its eastern, 
formidable ■ \he ‘’o tins stream of lava are deep and 
troublesome, often dafwerT” always painful and 
selves down from rorV r ' u" P^^oes weletour- 
'vliy there should be these ”o opinion 
fee of this lava : i„ >rregularities in the sur- 
the trough of the se- •, 1 V'^ mscmblcs what sailors tenri 
if the sea in a 510™/'] oompare it to nothing but 
sudden stationarv tl,e t.ad by some force become on a 
3ga'm approached I n retaining their swell. As wa 
valley, \L d™th nf , n steep 
tf less tlian oL hundi-ed'l' cannot 
the lava lyinff in hr i ^ hundred and fifty feet 
“irailar to the masses of " "Pon the other 
have tumbled down ^‘^ae and decay 
^■o-u. the scoria, or ^'P^ ' and, except 
they in no degree bear the calls “ the Fiery Surge, 
uf Iiqiud matter. ^ tuaiks of having rolled as a stream 
\Ve descended tlip 
almost at a run, and arrive ™’aT T^‘'^„"''th great rapidity 
han two hours. We then *" little more 
'ug the trade by which we had pb ° and follow- 
‘-eachetl, about fom o'c ock ?bi Pteceding day, 
iws^mable friend Mr. Barry ^ ‘Country-house of our 
oa-urivd' on the^24ih''of is any distinct account, 
fK‘shocksof ^^on twenty! 
■■ ' .St a great liu-ht w^, foft. On the 
'^ hiic mountains. Hem tt on Manja, towards the 
Were formed, which tlirp!^ ‘'Pened, and two volcanoes 
wf- ^''“oonsiderSle nm ^"^P^ to 
sUU couiinuS to be H combustible matter, 
'uea to be tlirown up, kindled above fifty 
u 2 ' 
