at the North Pole.
Sight of the
eshing
at an angle of
2. The earth rotates from west
cast
3. Biosphere is the narrow zone of contact between lithosphere, hydrosphere and
atmosphere.
4. The earth has an average temperature of 17°C
5. Atmospheicis the major
reservoir of carbon on the earth.
III. Long Answer Questions
1. Study the figure and answer the questions that follow:
What does the figure show
you about the earth?
(b) State briefly the Bedford Level Experiment. Pgrands
(c) The sun rises and sets at different times in different
places. What does the statement show about the
shape of the earthpPg9
(d) In what way is the earth's atmosphere beneficial to
mankind? 10
2. Provide reliable evidence to prove that the earth is spherical in shape.
3. Give the distinctive features of the earth as a unique planet.
4. Describe the role of each of the following in making earth a habitable planet.
(a) Atmosphere pg
Figure for Q1
pg7
912
(2
(c) Temperature
pgel
Project/Activity
noiect on Natural Creation and Destruction. State the conditions essential for the
Hy new species have evolved and of
Answers
Answer:
Q. thora short karke bhejo..............bagut lamba hay
Answer:
Mark me as brainliest pls
Explanation:
Carbon cycle
Carbon cycleThe carbon cycle is the biogeochemical cycle by which carbon is exchanged between the biosphere, geosphere, hydrosphere and atmosphere of the Earth.
Carbon cycleThe carbon cycle is the biogeochemical cycle by which carbon is exchanged between the biosphere, geosphere, hydrosphere and atmosphere of the Earth.The cycle is usually thought of as four major reservoirs of carbon interconnected by pathways of exchange.
Carbon cycleThe carbon cycle is the biogeochemical cycle by which carbon is exchanged between the biosphere, geosphere, hydrosphere and atmosphere of the Earth.The cycle is usually thought of as four major reservoirs of carbon interconnected by pathways of exchange.The reservoirs are the atmosphere, the terrestrial biosphere (which usually includes freshwater systems and non-living organic material, such as soil carbon), the oceans (which includes dissolved inorganic carbon and living and non-living marine biota), and the sediments (which includes fossil fuels).
Carbon cycleThe carbon cycle is the biogeochemical cycle by which carbon is exchanged between the biosphere, geosphere, hydrosphere and atmosphere of the Earth.The cycle is usually thought of as four major reservoirs of carbon interconnected by pathways of exchange.The reservoirs are the atmosphere, the terrestrial biosphere (which usually includes freshwater systems and non-living organic material, such as soil carbon), the oceans (which includes dissolved inorganic carbon and living and non-living marine biota), and the sediments (which includes fossil fuels).The annual movements of carbon, the carbon exchanges between reservoirs, occur because of various chemical, physical, geological, and biological processes.
Carbon cycleThe carbon cycle is the biogeochemical cycle by which carbon is exchanged between the biosphere, geosphere, hydrosphere and atmosphere of the Earth.The cycle is usually thought of as four major reservoirs of carbon interconnected by pathways of exchange.The reservoirs are the atmosphere, the terrestrial biosphere (which usually includes freshwater systems and non-living organic material, such as soil carbon), the oceans (which includes dissolved inorganic carbon and living and non-living marine biota), and the sediments (which includes fossil fuels).The annual movements of carbon, the carbon exchanges between reservoirs, occur because of various chemical, physical, geological, and biological processes.The ocean contains the largest active pool of carbon near the surface of the Earth, but the deep ocean part of this pool does not rapidly exchange with the atmosphere.
Carbon cycleThe carbon cycle is the biogeochemical cycle by which carbon is exchanged between the biosphere, geosphere, hydrosphere and atmosphere of the Earth.The cycle is usually thought of as four major reservoirs of carbon interconnected by pathways of exchange.The reservoirs are the atmosphere, the terrestrial biosphere (which usually includes freshwater systems and non-living organic material, such as soil carbon), the oceans (which includes dissolved inorganic carbon and living and non-living marine biota), and the sediments (which includes fossil fuels).The annual movements of carbon, the carbon exchanges between reservoirs, occur because of various chemical, physical, geological, and biological processes.The ocean contains the largest active pool of carbon near the surface of the Earth, but the deep ocean part of this pool does not rapidly exchange with the atmosphere.Note: The above text is excerpted from the Wikipedia article "Carbon cycle", which has been released under the GNU Free Documentation License.