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Contents contributed and discussions participated by keanu Dickinson

keanu Dickinson

Stop the Clock - Conservation International - 0 views

    • keanu Dickinson
       
      i cant beileve a speices die every 20 min
keanu Dickinson

Wildlife of Sydney - Fact File - Humpback Whale - 0 views

    • keanu Dickinson
       
      the HUMPback whale is a delecate whale from what iv read /heard
keanu Dickinson

Wildlife of Sydney - Fact File - Southern Right Whale - 0 views

    • keanu Dickinson
       
      I wonder why they call it the right whale
keanu Dickinson

Wildlife of Sydney - Fact File - Long-nosed Bandicoot - 0 views

    • keanu Dickinson
       
      Are these animals related to possums in any way? PS. crash bandicoot looks nothing like this xD
keanu Dickinson

Wildlife of Sydney - Fact File - Sugar Glider - 0 views

    • keanu Dickinson
       
      this animal dosent seem harmful or disturbing in any way actually it looks peaceful.
keanu Dickinson

Endangered Animals Links - 0 views

    • keanu Dickinson
       
      these animals are our friend
keanu Dickinson

Deal struck to protect the Congo gorillas - 0 views

    • keanu Dickinson
       
      i hear people fly contries to contries just to kill an animlal to they cAN GET MONEY
keanu Dickinson

Endangered Species - 0 views

    • keanu Dickinson
       
      i think its somthing in the water that makes them wash up.
keanu Dickinson

Beavers and Sea Eagles returning to England - 0 views

    • keanu Dickinson
       
      i know beavers may be warm but don kill em =P
keanu Dickinson

Endangered Species Information Network - 0 views

    • keanu Dickinson
       
      i thought there were only endangerd speices in other contries besides the USA.man how i was wrong
keanu Dickinson

Extinct Birds - 0 views

    • keanu Dickinson
       
      Would u kill a human?thought so. dont kill and animal
keanu Dickinson

Endangerd Species-The Rhinoceros - 0 views

    • keanu Dickinson
       
      STOP KILLING ANIMALS
keanu Dickinson

WWF - Great Apes - Losing their homes, losing their lives - 0 views

    • keanu Dickinson
       
      I seriously dont know what to say
keanu Dickinson

WWF - Polar Bear - WWF: A Leader in Polar Bear Conservation - 0 views

    • keanu Dickinson
       
      Antartica is melting away its hard enough for every animals there how it is but now poeple are helping them die.
  • With 20-25,000 polar bears living in the wild, the species is not currently endangered, but its future is far from certain.
keanu Dickinson

WWF - Rhinos - Very few rhinos now survive outside protected areas - 0 views

    • keanu Dickinson
       
      A great solution to stop these people from KILLING animals is stop buying their items.
keanu Dickinson

WWF - Marine Turtles - Three of the seven existing species of marine turtle are critica... - 0 views

    • keanu Dickinson
       
      What did the turtles do to YOU?
  • Many offspring, few survivors
keanu Dickinson

Bagheera: Endangered Species and Endangered Animal Online Education Resource - 0 views

shared by keanu Dickinson on 04 Dec 08 - Cached
    • keanu Dickinson
       
      I hate people who kill animals to help them live on. What is i shot u and sold ur skin?
keanu Dickinson

WWF - Tigers - Overview - 0 views

    • keanu Dickinson
       
      I cant belive that people would kill animals for money or coats.
keanu Dickinson

Blue Sky - Why is the Sky Blue? - 0 views

  • end of the spectrum are the reds and oranges. These gradually shade into yellow, green, blue, indigo and violet. The colors have different wavelengths, frequencies, and energies. Violet has the shortest wavelength in the visible spectrum. That means it has the highest frequency and energy. Red has the longest wavelength, and lowest frequency and energy. LIGHT IN THE AIR Light travels through space in a straight line as long as nothing disturbs it. As light moves through the atmosphere, it continues to go straight until it bumps into a bit of dust or a gas molecule. Then what happens to the light depends on its wave length and the size of the thing it hits. Dust particles and water droplets are much larger than the wavelength of visible light. When light hits these large particles, it gets reflected, or bounced off, in different directions. The different colors of light are all reflected by the particle in the same way. The reflected light appears white because it still contains all of the same colors. Gas molecules are smaller than the wavelength of visible light. If light bumps into them, it acts differently. When light hits a gas molecule, some of it may get absorbed. After awhile, the molecule radiates (releases, or gives off) the light in a different direction. The color that is radiated is the same color that was absorbed. The different colors of light are affected differently. All of the co
  • d after Lord John Rayleigh, an English physicist, who first described it in the 1870's.) WHY IS THE SKY BLUE? The blue color of the sky is due to Rayleigh scattering. As light moves through the atmosphere, most of the longer wavelengths pass straight through. Little of the red, orange and yellow light is affected by t
  • As you look closer to the horizon, the sky appears much paler in color. To reach you, the scattered blue light must pass through more air. Some of it gets scattered away again in other directions. Less blue light reaches your eyes. The color of the sky near the horizon appears paler or white.
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  • THE BLACK SKY AND WHITE SUN On Earth, the sun appears yellow. If you were out in space, or on the moon, the sun would look white. In space, there is no atmosphere to scatter the sun's light. On Earth, some of the shorter wavelength light (the blues and violets) are removed from the direct rays of the sun by scattering. The remaining colors together appear yellow. Also, out in space, the sky looks dark and black, instead of blue. This is because there is no atmosphere. There is no scattered light to reach your eyes. WHY IS THE SUNSET RED? As the sun begins to set, the light must travel farther through the atmosphere before it gets to you. More of the light is reflected and scattered. As less reaches you directly, the sun appears less
  • The sky around the setting sun may take on many colors. The most spectacular shows occur when the air contains many small particles of dust or water. These particles reflect light in all directions. Then, as some of the light heads towards you, different amounts of the shorter wavelength colors are scattered out. You see the longer wavelengths, and the sky appears red, pink or orange.
  • RE ABOUT:THE ATMOSPHERE WHAT IS THE ATMOSPHERE? The atmosphere is the mixture of gases and other materials that surround the Earth in a thin, mostly transparent shell. It is held in place by the Earth's gravity. The main components are nitrogen (78.09%), oxygen (20.95%), argon (0.93%), and carbon dioxide (0.03%). The atmosphere also contains small amounts, or traces, of water (in local concentrations ranging from 0% to 4%), solid particles, neon, helium, methane, krypton, hydrogen, xenon and ozone. The study of the atmosphere is called meteorology. Life on Earth would not be possible without the atmosphere.
  • d increases with increasing altitude. The increase is caused by the absorption of UV radiation by the oxygen and ozone. · The temperature increase with altitude results in a layering effect. It creates a global "inversion layer", and reduces vertical convection. Mesosphere - Extends out to about 100 km (65 miles) · Temperature decreases rapidly with increasing altitude. Thermosphere - Extends out to about 400 km ( 250 miles)
  • hes the Earth, 30% is reflected back into space by clouds and the Earth's surface. The atmosphere absorbs 19%. Only 51% is absorbed by the Earth's surface. We are not normally aware of it but air does have weight. The column of air above us exerts pressure on us. This pressure at sea level is defined as one atmosphere. Other equivalent measurements you may hear used are 1,013 millibars, 760 mm Hg (mercury), 29.92 inches of Hg, or 14.7 pounds/square inch (psi). Atmospheric pressure decreases rapidly with height. Pressure drops by a factor of 10 for every 16 km (10 miles) increase in altitude. This means that the pressure is 1 atmosphere at sea level, but 0.1 atmosphere at 16 km and only 0.01 atmosphere at 32 km. The density of the lower atmosphere is about 1 kg/cubic meter (1 oz./cubic foot). There are approximately 300 billion billion (3 x 10**20, or a 3 followed by 20 zeros) molecules per cubic inch (16.4 cubic ce
  • ers). At ground level, each molecule is moving at about 1600 km/hr (1000 miles/hr), and collides with other molecules 5 billion times per second. The density of air also decreases rapidly with altitude. At 3 km (2 miles) air density has decreased by 30%. People who normally live closer to sea level experience temporary breathing difficulties when traveling to these altitudes. The highest permanent human settlements are at about 4 km (3 miles). LAYERS OF THE ATMOSPHERE The atmosphere is divided into layers based on temperature, composition and electrical properties. These layers are approximate and the boundaries vary, depending on the seasons and latitude. (The boundaries also depend on which "authority" is defining them.) LAYERS BASED ON COMPOSITION Homosphere
  • LAYERS BASED ON TEMPERATURE Troposphere - Height depends on the seasons and latitude. It extends from ground level up to about 16 km (10 miles) at the equator, and to 9 km (5 miles) at the North and South Poles. · The prefix "tropo" means change. Changing conditions in the Troposphere result in our weather. · Temperature decreases with increasing altitude. Warm air rises, then cools and falls back to Earth. This process is called convection, and results in huge movements of air. Winds in this layer are mostly vertical. · Contains more air molecules than
  • · The air is very thin. · The prefix "strato" is related to layers, or stratification. · The bottom of this layer is calm. Jet planes often fly in the lower Stratosphere to avoid bad weather in the Troposphere. · The upper part of the Stratosphere holds the high winds known as the jet streams. These blow horizontally at speeds up to 480 km/hour (300 miles/hour) · Contains the "ozone layer" located
  • gen we need to breath. But it also serves other important functions. It moderates the planet's temperature, reducing the extremes that occur on airless worlds. For example, temperatures on the moon range from 120 °C (about 250 °F) in the day to -170 °C (about -275 °F) at night. The atmosphere
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