(1)
The geology of the Earth's surface is dominated by the particular
properties of
water.
Present on Earth in solid, liquid, and gaseous states, water is
exceptionally
reactive.
It dissolves, transports, and precipitates many chemical compounds and is
constantly
modifying the face of the Earth.
(5)
Evaporated from the oceans, water vapor forms clouds, some of which are
transported
by wind over the continents. Condensation from the clouds provides the
essential
agent of continental erosion: rain. Precipitated onto the ground, the water
trickles
down to form brooks, streams, and rivers, constituting what is called the
hydrographic
network. This immense polarized network channels the water toward a
(10)
single receptacle: an ocean. Gravity dominates this entire step in the
cycle because
water
tends to minimize its potential energy by running from high altitudes
toward the
reference
point that is sea level.
The
rate at which a molecule of water passes though the cycle is not random but
is
a
measure of the relative size of the various reservoirs. If we define
residence time as
(15)
the average time for a water molecule to pass through one of the three
reservoirs atmosphere, continent, and ocean-we see that the times are very
different. A water
molecule
stays, on average, eleven days in the atmosphere, one hundred years on a
continent
and forty thousand years in the ocean. This last figure shows the
importance
of
the ocean as the principal reservoir of the hydrosphere but also the
rapidity of water
(20)
transport on the continents.
A
vast chemical separation process takes places during the flow of water over
the
continents.
Soluble ions such as calcium, sodium, potassium, and some magnesium are
dissolved
and transported. Insoluble ions such as aluminum, iron, and silicon stay
where
they are and form the thin, fertile skin of soil on which vegetation can
grow.
(25)
Sometimes soils are destroyed and transported mechanically during flooding.
The
erosion
of the continents thus results from two closely linked and interdependent
processes,
chemical erosion and mechanical erosion. Their respective interactions and
efficiency
depend on different factors.
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