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María Jesús Campos
learningfromgeography.wikispaces.com
The Earth’s Surface
To  make investigations
easier the surface of the
Earth has been divided
up into four
interconnected spheres:
       Lithosphere
       Hydrosphere
       Atmosphere
       Biosphere
HYDROSPHERE

   It comes from the
    ancient Greek
    “hydro” which means
    water and “sphaira”
    which means sphere.

   It refers to water on,
    under and over the
    surface of the Earth.
   There is always the
    same amount of
    water on Earth.
   Water appears in
    different states
    (liquid, gas or solid
    form).
   Water continually
    move between the
    atmosphere, the
    oceans and the
    continents.
   This continual movement is called the
    water cycle:
       Evaporation: water evaporates into the
        atmosphere, where it cools.
       Condensation: As it get cooler on the
        atmosphere, it condenses and forms clouds.
       Precipitation: when clouds cannot absorb
        any more water there is precipitation in the
        form of rain, snow or hail. Some
        precipitation falls on the land flowing into
        lakes and rivers, other water filters into the
        ground becoming groundwater.
       Transportation: water in rivers or
        groundwater is transported to the oceans
        and seas again and the water cycle begins
        again.
   Saltwater: 97% of
    the Earth’s water is
    saltwater located
    mainly in the
    oceans and seas.
   Freshwater: 3% is
    fresh water located
    on continents and
    islands (river,
    lakes, groundwater,
    water vapour…)
   Oceans: vast masses        Groundwater:
    of saltwater that           rainwater that
    separate the                infiltrates rocks and
    continents.                 soil into the Earth’s
   Seas: oceanic waters        surface.
    that are close to          Aquifers: stores of
    continents and not as       groundwater that
    deep as oceans.             accumulate
                                underground on top
   Rivers: continuously        of impermeable
    flowing currents of         layers of rock.
    water that flow into
    seas, lakes and other      Wells: holes that
    rivers.                     men do into the
                                Earth’s surface to
   Tributary: a river          bring underground
    that flows into             water to the surface.
    another river.
   Glaciers: huge mass of ice, formed from
    compacted snow, slowly flowing over a land
    mass.
   Ice caps: huge mass of ice and snow that
    permanently cover the poles of the Earth.
   Lakes: large bodies of water that
    accumulate in inland basins. They receive
    water from rivers, precipitation and
    groundwater.
   There are 3 stages in the course of a river:
       Upper Course: from the river’s source down the
        mountains water flows rapidly eroding rocks.
       Middle course: water flows less rapidly depositing
        sediments.
       Lower course: the river reaches its mouth into a lake,
        another river or a sea. Water flows slowly depositing
        sediments.
   The flow is the amount of water in a river. It depends
    on:
       The amount of rainfall.
       The type of soil
   Water is essential for
    life. Humans can only
    drink fresh water that
    needs to be purified.
   As most fresh water is
    trapped in ice and
    glaciers there is not
    much water for
    human consumption
    left.
   So we need to recycle
    water to assure our
    lifelihood.
   Although water is found in
    a considerable amount in
    temperate and tropical
    regions where there is a lot
    of precipitation there is an
    uneven distribution of
    water on the Earth.
   Floods: the inundation of
    land that is normally dry
    through the overflowing of
    a body of water
   Droughts: a long period of
    scanty or low rainfall that
    normally affects growing or
    living conditions.
Developed by María Jesús Campos
Chusteacher
Wikiteacher

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Hydrosphere

  • 2. The Earth’s Surface To make investigations easier the surface of the Earth has been divided up into four interconnected spheres:  Lithosphere  Hydrosphere  Atmosphere  Biosphere
  • 3. HYDROSPHERE  It comes from the ancient Greek “hydro” which means water and “sphaira” which means sphere.  It refers to water on, under and over the surface of the Earth.
  • 4. There is always the same amount of water on Earth.  Water appears in different states (liquid, gas or solid form).  Water continually move between the atmosphere, the oceans and the continents.
  • 5. This continual movement is called the water cycle:  Evaporation: water evaporates into the atmosphere, where it cools.  Condensation: As it get cooler on the atmosphere, it condenses and forms clouds.  Precipitation: when clouds cannot absorb any more water there is precipitation in the form of rain, snow or hail. Some precipitation falls on the land flowing into lakes and rivers, other water filters into the ground becoming groundwater.  Transportation: water in rivers or groundwater is transported to the oceans and seas again and the water cycle begins again.
  • 6.
  • 7.
  • 8. Saltwater: 97% of the Earth’s water is saltwater located mainly in the oceans and seas.  Freshwater: 3% is fresh water located on continents and islands (river, lakes, groundwater, water vapour…)
  • 9.
  • 10. Oceans: vast masses  Groundwater: of saltwater that rainwater that separate the infiltrates rocks and continents. soil into the Earth’s  Seas: oceanic waters surface. that are close to  Aquifers: stores of continents and not as groundwater that deep as oceans. accumulate underground on top  Rivers: continuously of impermeable flowing currents of layers of rock. water that flow into seas, lakes and other  Wells: holes that rivers. men do into the Earth’s surface to  Tributary: a river bring underground that flows into water to the surface. another river.
  • 11.
  • 12. Glaciers: huge mass of ice, formed from compacted snow, slowly flowing over a land mass.  Ice caps: huge mass of ice and snow that permanently cover the poles of the Earth.  Lakes: large bodies of water that accumulate in inland basins. They receive water from rivers, precipitation and groundwater.
  • 13.
  • 14. There are 3 stages in the course of a river:  Upper Course: from the river’s source down the mountains water flows rapidly eroding rocks.  Middle course: water flows less rapidly depositing sediments.  Lower course: the river reaches its mouth into a lake, another river or a sea. Water flows slowly depositing sediments.  The flow is the amount of water in a river. It depends on:  The amount of rainfall.  The type of soil
  • 15.
  • 16. Water is essential for life. Humans can only drink fresh water that needs to be purified.  As most fresh water is trapped in ice and glaciers there is not much water for human consumption left.  So we need to recycle water to assure our lifelihood.
  • 17. Although water is found in a considerable amount in temperate and tropical regions where there is a lot of precipitation there is an uneven distribution of water on the Earth.  Floods: the inundation of land that is normally dry through the overflowing of a body of water  Droughts: a long period of scanty or low rainfall that normally affects growing or living conditions.
  • 18.
  • 19. Developed by María Jesús Campos Chusteacher Wikiteacher