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Spheres of the Earth
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There are four
interconnected spheres
on Earth:
• biosphere
• geosphere
• hydrosphere
• atmosphere
Matter cycles and energy
flows through these four
spheres.
Spheres of the Earth
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Spheres of the Earth
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BiosphereHydrosphere
AtmosphereGeosphere
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The biosphere represents all
living components on Earth.
Components include:
all plants (e.g. trees, flowers and
grasses)
all animals (e.g. birds, mammals
and fish)
all fungi (e.g. mushrooms and
molds)
other examples
The biosphere can be
described as the total sum of
all ecosystems.
Biosphere
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The geosphere represents all
solid land and interior
components of Earth.
Components include:
all types of rock and
minerals
Earth’s mantle
other examples
The geosphere can be
described as the Earth
beneath our feet.
Geosphere
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The hydrosphere
represents all water
components of Earth.
Components include:
saltwater bodies (examples)
freshwater bodies
(examples)
The hydrosphere can
be described as the
total mass of all water
found on Earth.
Hydrosphere
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The atmosphere represents all gaseous components surrounding Earth’s surface; it’s retained on Earth’s surface via gravity.
Components include:
oxygen gas (O2)
nitrogen gas (N2)
other examples
The atmosphere protects life on Earth by absorbing UV radiation from the sun, maintaining temperatures and warming Earth’s surface.
Atmosphere
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Interconnectedness
• All four spheres are highly interconnected.
dependent and internally connected to one another
examples
• When one of the four spheres is positively
or negatively affected, the other three are
also affected.
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Energy flow
• Energy flows freely through the
four spheres.
• All of Earth’s energy comes from the sun.
• Energy cannot be created nor destroyed; it
can be transformed and recycled.
• Energy can be stored in different spheres
for long periods of time.
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Energy flow
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Matter cycles
• Different forms of matter continually cycle through the four spheres.
• Matter cannot be created or destroyed; it can be transformed and recycled.
• Carbon can move through many different forms:
as glucose (C6H12O6) in organic matter
as methane (CH4) in decaying matter
as carbon dioxide (CO2) in the atmosphere
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Matter cycles
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