The daily chieftain. [volume] (Vinita, Ind. Ter. [Okla.]) 1898-1902, 1898-11-09
RISE AND FALL OF LAND.
ton of Coast Lines In Differ
ent Countries.

A series of 30 marks were made in
1851 on the Baltic coast, from Tornea
to the Maze of Norway, and in 1854
these were examined by commission
of the Swedish Academy of Sciences.
By these observations it was estab-
lished that the movement of elevation
was contained in the north, and that
of depression at the southern extrem-
ity of the peninsula. About Kalmar
and Karlskrona no change of level
could be detected as having occurred
within recent years, but since l7o0 1T
was proved that the head of the Gulf of
Bothnia had risen at the rate OF l,l70
meters per century. This rate OF ele-
vation declines progressively toward
the south. It is not more than O.3o OF
a meter at the Maze, and it Is zero at
Bornholm. The mean elevation of the
Swedish coast is thus 1.6O meters per
century. From these and a host of
similar data, no doubt can exist re-
garding the rise of the Scandinavian
peninsula, and inferentially there was
a period when the Arctic ocean com
municated with the Baltic. The Jap
anese islands are also rising, and many
districts around the sea of Aral and
the Caspian are in similar plight, ac-
cording to evidence equally conclusive.
In more southern regions data equally
cogent are ready to our hand. Crete
has risen II feet above its ancient
level; the old Greek ports are high and
dry, and limestone rocks which the
sea never touches are to be found
pierced by species of shellfish which
bores into stone, though, it may be
added, so little can any law be formu-
lated regarding these areas OF eleva-
ton and subsistence that on the east
ern side of the island the ruins of sew
eral Greek towns may be seen under
the water. Marine shells far above the
highest tidal mark are found plentiful
ly along the shores of South America,
commencing at Terra del Fuego, and
along the west coast for distance of
at least 1000 miles, and in patches
probably as far north as the Isthmus
of Panama, these evidences of up
heaval being deposited at elevations
varying, according to Darwin, from
300 to 1900 feet over the sea level The
raised sea beaches, which are taken as
proofs of the rising of the land, are
found not only around the places al
ready noticed, but along the outer
coast of Norway, South America-at
Coquimbo, for example-and along
many parts of the shores of Great
Britain. At Brighton, for instance,
there is marked specimen of this in
the cliffs east of Kemp Town; while
Robert Chambers wrote an elaborate
work, mainly descriptive of those to be
traced along the Scottish coasts at all
heights up to 100 feet above the pres
ent sea level. Again. though belong
ing to the same class of proofs, the
elevation of the coast here is indicated
by caves, formed by the constant dash
of the waves, being found along the
coasts of Scotland, near Campbelltown
and Neill, in Cantire, for example, at
places far above the reach of the sea,
which laves the base of the cliff in
which they are excavated. In Natal
upheaval is still going on, and the east
ern coast of Africa is generally be-
lieved to be rising; Australia, on the
northeast if not on the whole of the
east coast, is rising. Until late peri
cd in the geological history of Tas-
mania, the site of Hobart Town was
covered by the sea, and in New Zea-
land. though there is an area of de-
preston on the extreme northwestern
point, the mass of the land is rising
Public Opinion.
THAT Sergt BUNKER IS certainIy 4
terror"
"What has he done now?"
"As soon as we got off at thE 6epes
he rushed up and kissed the thre
prettiest girls in the;erowd- az per
feet strangers"
What old they sa42''
.'They said: OBJ Geprges NiIsh k1s
you coming home ssain p : Cleveland