The Panola weekly star. (Sardis, Miss.) 1882-18??, 1882-02-25

The selase n the isaamiie,
Tn fstautlie eqfeilihm tas, All Hhftfti.
W. Ffsth ihi aii 1i4slf ifHflhs tnff
uwnl fesulisl N ttfI KitF adesntfhbui N
Aftilo knHulpdse and much n lhls lbrisAtd
feanafhleai Information " N fnth : ptafu
'slJ nssim fnlufe a 10 aiatd pisd ffnuhi
lof : tHHllnuahte " etplmilNh In me- mmoia
Hsi0hs ~ iti NHiih thruah ne alpifeHi
\ luetfsf statements heretofore iueelte1 N
Safdlna the SnJhse n me- ioti ieA0hslie and
lalri mnsenepia N ~ Long eai his hefiHc
rlnilaiiluns. tofy ffth hsis ar revealed
shith sh0v haw me- meaasfness \ appnehi
faihef than real ue lung Hne thc hut W
Demonstrate The iaa ihit Wpnrtl Land Il N
q sep lintlied ettehi noHhetly lle hii
shown the inacfuuNy VI the theory " ile
late d. reierahn, The distinguished uef
man RedHfarhcf, thd Wfange Land
wn Tho eastern extremity ~ an kftilc
continent lIe hAs discovered he cs
la,cnte NJ vast polar ocean
nottheastwnrd from the New Siberian Islands
he has arsi discovered ai least two islands IN
the great ntean basin " the Avlle lule ~
sides ihe original discovery ~ these islands
he has proved, In his observation u lhlfd
island Al the notthcastwafd from New N
lcfia, tho verify " the claim hy ilcdcnttfom
and saunlkov IN lhO that land existed there
which had been seen lie has proved tho cs.
lsience of mighty cuten, sweeping alowly
around the earth ~ the north of Asia w.
rope, Greenland aud America, with great
banch dlvergng Fonthwesterly around The
eastern promoniorlcr of frans Joeci Land,
which Ia but an estenainno of Greenland hehas
proved that the temperature u the high lail
tuder he attaIncd below the Arctic rde Ia not
incompatible with good health aud compare
Tive comfort, vhen suitable food and shelter
are provided for cSplorcrA Ia
He has completely disprovcd the assumption
that q 'paleocryrtlc' sea, or area Of ancient
and unthawablc Ice, exlsts IN the high north;
for, while caught amid fragments o. foe ice
forming mn immense floating field, he driftcd
about In vast open, polar sea duripg consid
crably more than year and ahalfo time, aud
stil did not during that period aight the shores
OF the lonely ocean upon which he was swept
aud whelmed about In ley arms like waif IN
| the drcary abyss As the experience uf Wey-
nreeht and pa,er IN tho Tey,,hoir whllc
,,,',', s,,', 80.
uugn' W Nm' 'ce npo OH northwest 'al's
0f NOVA lembla and drifting about during
long months In the saa u Ffanz Josef Land,
proyed 10 those unaeouain,ed with the fact
ia, M. na,, ~ ,ho &C.,, w.. rnoxn 40 A.
as ~, ','' y, 'ne oVuA'' ~, NV" !" ~
n,Nsap'o ny Norsei'cn IN the iouf'ech'n'
nlteentb ard sixteenth centuries, that II was
4 sea lncr,istcd by Ice over but A part ~ II,
..,rface ana dny,y n ,.r, NJ m, r.a, .a n,
- s..''., ~. ..'..s...'. .y. -, -, '
ho's ueA'y W.. n"p"''a"' 'o'aRe y"
proved IKE conditions existing away at th'
north of New Siberia. Moreover, the Jean
uette expeditIon ha. nnnaren,Iv dc,ermlpef
n ,o ,s ,.., ,hs, ,,,.,, I. ~, va, ,,..., h,',,
"~p. 'A,' ''"' "'o'" 70 :" WY tfo"' wv
OF Ihnd 10 the extreme polar sea near Asia
and that climate conditions In the near yIcln
Ity of the Pole are more genial than furthe
,c,,h -
'Ys ..,, -
hie''e sh"fes iacihg ,ne hot,h 40 not pro
duce icebefgs 10 any considerable extent Tn
almost total absence Of icebergs In the whal
in, a.. ,,o.,h ~ u,l,.t,,,.. s,.t, a., a, Al,