The Morris County chronicle. [volume] (Morristown, N.J.) 1877-1915, 1901-11-22
! EAR OF THE EARTH.
oW THE FACE or OUR GLOBE is
CONTINUALLY CHANGING.


tie Influence.
The atmosphere plays Its part in geo
7gicaI operations. Its corroding pow
y backed1by rain and wind, helps to
ecay and disintegrate those rocks
Thich are exposed to its influence. Rain
ompletes the work thus begun. Wind
lows dust, sand and volcanic ashes
,ver large tracts of earth--in fact,
over the whole Of it.
1t is only of late years that geolo-
lists have discovered that fine vol
anic dust is carried over the whole of
he earth'5 surface anu plays a very
Important part in the deep sea depos-
is. On deserts and nearly rainless re-
sions blown sand will wear away the
hardest rocks by beating against
them. Some sandstone formations APP
pear to have been piled up by winds.
Winds cause ocean currents, waves
and storms. The great denuding
power of the sea is largely due to the
atmosphere. Some parts of the Eng
Iish coasts are being rapidly washed
away. Plants and animals have their
distribution considerably affected py
winds and ocean currents. Again,
whether living in water or on land,
animals live on the oxygen supplied
from the atmosphere, and land plants
absorb carbonic acid from the same
source.
Rain acts in two ways: ~ chemic-
ally by dissolving certain substances,
such as lime. out of the rocks, and ~
mechanically by wearing down their
surfaces as it flows over them. Any
old building-a ruined castle or cathe-
dral, for instances a wealth
cred" surface resulting from the ac-
ton of rain and wind. In sandstone
structures the details of carving are
often lost, and ON old tombstones the
lettering can hardly be deciphered.
Springs are due to rainwater collecting
in rocks and rising to the surface.
Rivers are fed by rains and springs.
A river is very powerful geological
agent. In the hardest rocks rivers
gradually carve out a valley or gorge.
This is accomplished partly by chemic.
ally dissolving certain mineral sub
stances, but chiefly by mechanical
erosion, the stones, sand and mud
wearing away the bed of a stream as
they run and tumble over it.
The finest examples of river action
are the famous canyons of Colorado,
which in some places are gorges 1900
or even 6,O00 feet deep, with vertical
sides. But, as already pointed out,
rivers have constructive action quite
as important as their destructive ac-
ton. By bringing down their burden
of sediment into lakes, estuaries and
seas they build up great piles of rock
and SOW the dust of continents to
be-,
Glaciers are rivers of ice fed by the
eternal SHOWS" of high mountain
ranges such as the Alps. They wear
out their own valleys as rivers do;
they transport mud, sand and stones to
great distances, in some cases sending
them sealed up in icebergs to float far
out TO sea and on melting deposit their
burdens on the sea floor. OFF the coast
of Newfoundland northern icebergs
are depositing a great mass of "gla-
cial drift
The sea is great denuding agent;
but its work is more constructive than
destructive. 1t is the workshop where
nearly all the stratified rocks have
been accumulated and ranged in layers
or strata. The rivers and ocean cur
rents continually bring in fresh sup
plies of debris even for hundreds of
miles.
Man, compared with the lower ami
mails, produces but little effect as ge-
illogical agent. Still the human race
has considerably modified the distribu-
ton of plants by cutting down forests
and by cultivating certain plants to
supply food. 50 with animals Ger
tain useful species have been cultivat-
ed and enormously increased at the
expense of others which prove useless
or harmful
But plants and animals have had,
and still have, far more influence geo
logically Coal seams are made up of
vegetable remains of former periods.
Forests have an important influence
on climate and on animal as well as
plant life. In the comparatively I'M
known world of the ocean marine
plants doubtless have important func-
TONS
Marine animals accomplish a vast
amount OF geological constructive
work. Great deposits thousands Of
feet thick owe their existence to small
ealcareous creatures living in the sea.
Coral reefs afford the most familiar
Illustration
The force known as heat is of great
Importance. The earth is hotter below
the surface and probably has d very
high temperature toward its center.
In some places not very, far below it's
surface it contains highly heated rock.
which occasionally flows over the sur
face during volcanic eruptions. In
other places we find hot springs in con-
nection with volcanic action
Heat exercises powerful influence
on rocks deeply buried below the
earth's surface, chiefly by means of
heated water and steam. In this way
rocks have been very much altered
or "metamorphosed." The crystalline
schists have thus been brought to their
present state by series of chemical
changes due to heat, and there is no
doubt that they were once ordinary
deposits OF clay, sand, etc. Hutchin-
sons Autobiography Of the Earth"
Ann r,,,1a4av Cn.,,,,onx-