Four Spheres of Earth
Four Spheres of Earth
Lithosphere
The lithosphere is the solid, rocky crust covering entire planet. This crust is
inorganic and is composed of minerals. It covers the entire surface of the
earth. The lithosphere is also called as geosphere.
Hydrosphere
The hydrosphere is composed of all of the water on or near the earth. This
includes the oceans, rivers, lakes and even the moisture in the air. Ninety
seven percent of the earth’s water is in the oceans. The remaining three
percent is fresh water; three quarter of the fresh water is solid and exists in
ice sheets.
Biosphere
The biosphere is made up of the parts of
Earth where life exists. The biosphere extends from the deepest root systems of
trees, to the dark environment of ocean trenches, to lush rain forests and high
mountains. The biosphere has existed for
about 3.5 billion years.
Atmosphere
The
atmosphere is the body of air which surrounds our planet. This gaseous envelope
is most dense at sea level and rapidly decreases with increasing altitude. It
is an important geological agent. It acts as a thermal blanket, captures heat
and supply snow and rain water.
The air of our planet is about
78% nitrogen and about 21% oxygen; the small amount remaining is composed of
carbon dioxide and other gases such as neon, helium, krypton, xenon, water
vapors, dust particles and hydrocarbons etc.
Earth’s cycles and spheres are
interconnected. All four spheres can be and often are present in a single
location. The importance of soil as a natural body derives in large part from
its role as an interface between above four spheres of earth.
The interface where the worlds of
rock (lithosphere), air (atmosphere), water (hydrosphere) and life (biosphere)
meet is termed as Pedosphere or soil.
For instance, a piece of soil
will of course have mineral material from the lithosphere. Additionally, there
will be elements of the hydrosphere present as moisture within the soil, the
biosphere as insects and plants even the atmosphere as pocket of air between
soil pieces.