{"character_count": 2393, "word_count": 443, "ccnet_language_score": [0.8747000098228455], "ccnet_perplexity": [2090.699951171875], "fasttext_language": ["en"]}
TF,sm staH1sresi Tysye5 IL bs T7so SieiE.i.1


AFTER Il wing, for two hours, n5uIged my
eyes " th a view Of the n,erirr Of the cr2ter,
rhar Is. IL the contemplation Of ipedac,e, which
in its krd, and in The Preient age, i without a
parallel IN he world urned them to auoth
er fcrne, viii h IS hkewife uaeoua.led fer the
Tnut pli.ity the beauty, and the variety, Of the
otjeds it P eients.


H. fat, there Is perhaps, no elevated region
on the whole globe which offer, al one view, 70
ample an extent Of fea and and as the fun liz Of
E.na. The 6rlt Of the lub!ime Obi Cts which 1,
prelents is the immenlr MATS Of its own ccloItl
BODY. When in the country below il, near Ca
tanla, We raiie our eyes to this fovercgn Of the
mountains, we certainly iurvey il ~iCh admira-
ton, as it rlco maje.tically, and lifts its lofty
head above the clouds and with kidd Of ge-
ornetiic glance we cit mate its height from the
baie to the fummit bu; we only lcc it il pro-
fe. Very different IS the appearance il pre-
tents, viewed from is toV e:ing tOp. when The
whole Of its enormous bulk is lube9ed To the
eye. The hra part, and that ne4Teit the obier-
vcr, is the upper region, which, from the guam
tity Of fnows and ice bcneah which It i, buried
during the. greater part Of the year, may be
called The fTigio zone, but viii b, at that time,
was diveRed of this covering, AMI only exhibit
ed rough and craggy cliffs, here PlleI on each
other, and there lePerate, and rfng perpendc
ularly fearful to view and impofi0le to aicend.
Towards the middle Of this zone, an af5mbiage
Of fugitive clouds, irradilted by the fun, and
all in molten, increafed the wild variety Of the
fcene Lower down, appeared the middle re-
gion, which, from the mildnefs Of lis climate,
may merit he name of the temperate zone
Its numerous woods, interrupted in vario1s Pla-
ces, feem, like a torn garment, to diicover the
nudity of the mountain. Here ariie a multitude
Of other mountains, vhich, III any other htua-
ton, would appear Of gigantic Gze, but are but
pieRa;es compared to Esna. Thele have all or
i9insted from fery eruPtons. Laaly, the eye
confemplates,with admiration, the lower Iegion,
which, from lis violent hea-, may claim the ap-
pellation Of The torrid zone the mott ex,enGve
Of the three, adorned with elegant villas and
eaales, verdant hills and Aowery fields, and ter
minated by the ex;enive coaa, where, to the