Northern Wisconsin advertiser. [volume] (Wabeno, Wis.) 1898-1925, 1900-09-06
IOLD IS EARTH?
EN- THAT DEFIES THE SCI
1 ENTIFIc WORLD.
CINE LATE DISCUSSIONS
But They Are BY no Means Conclusive
HAny Time From 100000 to 9O,-
100000 Years May Mark This Age
- of the World Learned Folk at
Y Sea.


Every year or two the scientific
world is favored with new speculations
regarding the age of the earth by men
who are in some measure qualified to
express an opinion. Lord sKelvinfs
reiterated estimate, based on the sup
posed rate of the cooling of the globe
from molten mass. was between TO-
100000 and 20,000000> years. These
figures have been received with univer-
sal respect, but have not been univer-
sally accepted. The biologists declare
that five or ten times as long period
is needed to allow for the slow devel-
opment of man from the lowest fossil
forms of life hitherto discovered. And
the biologists, after trying to form an
idea of the rate at which sedimentary
rocks are laid down today, say that
the strata already in existence could
hardly have been deposited in anything
like 100000 900 years. Only last year
Sir Archibald Geih.e expressed dissat-
isfaction with Lord Kelvin's estimate
for this reason.
Within the last lew weeks two new
contributions to the discussion have
beer made public. Prof. Grove X. Gill
bert, the retiring president of the
American Association for the Advance
ment of Science, treated one phase of
the matter in an address on Rhythms
and Geologic Time, and Prof. Jolly of
the University of Dublin has been con-
Quoting some original Investigations, a
report of which has just been pub
lished The Washington expert ven
tured no opinion of his own on the age
of the earth, and offered no comment
on the estimates of others. He merely
considered the methods employed thus
far in reaching conclusions, and sug-
gested that possibly a closer study of
certain rhythms that have been OBJ
served by biologists migvt be service
able New ways of attacking the
problem may prove more advantageous
than the old ones, although Prof. Gill
bert recommends adhering to the latter
even while employing the former.
In many places in the earth's crust
the deposits betray more or less
symmetrical alteration. In the coal
regions, for instance, sandstone and
shale are situated one above the other
in a monotonous succession. Else
where rocks which are of sedimentary
origin are curiously banded with
streaks of different hue. Sometimes
these markings are thin as sheet of
paper, and sometimes they are much
thicker. But they always suggest
change of circumstances at compare
lively regular intervals. In Scandina-
via there are alternate deposits OF
foreign trees and Doggy moss, which
indicate that the earth's surface was
first covered with one and then the
other in systematic manner. The re-
cession and advance of glaciers, too,
have superimposed one stratum of
gravel upon another in some instances
II successive times. A somewhat SIM
liar qualification of the deposits at the
position that there were number of
subsidences there, in consequence of
the weight of accumulated material.
Some influences which are supposed
to have had a share in shaping the
earth's surface are distinctly more
periodical than others. Prof. Gilbert
referred, for instance, to the notion
that the retardation of the earth's
rotation from tidal forces might cause
an alteration between fiattening at
the poles and an approach to spheric-
ity. The resulting changes of level
would modify the condition of those
continental areas that would thus be
exposed at one time and submerged at
another No attempt has yet been
made, however, to use this standard
in estimating the time represented by
adjacent geological deposits.
The phenomenon of the procession OF
the equinoxes is completed in period
of 81 900 years. At one stage OF this
cycle the southern hemisphere has
hotter summers and colder winters
than the northern, and 10000 years
later the situation is reversed. 1t has
been suspected by Croll and others that
local climatology would be so altered
by this agency as to leave some inn
press on the geological record. Prof.
Gilbert views that theory with some
favor and hopes that evidence OF It's
dness will be sought by geologists.
atever else may be thought OF
PrS Joly's recently published paper,
M lacS-of defniteness can be imputed
- Il rsa principal mineral constltu-
emf Of the. sea is chloride OF sodium
prof Joly thinks that all Of the So
dunn in thafbody Of water came from
the rocks, and was washed in there a.
q comparatively >uniform rate, in con-
sequence of the action Of the weather
upon the land. The soundness OF ms
premises will doubtless be called il
question, but his RESULTS are interest
ing. After applying ahnumDer Of cor
rections to his figures, Nhe concludes
that between sO,Ooo,oOO and 10000. 90
years have elapsed sinces the surface
Of the globe was first subjected to tn
denuding action Of rain.