Ocean Waves A wave is a periodic disturbance in space and time‚ possibly transferring energy to or through a space-time region. Have you ever ridden a wave in the ocean? Ocean waves travel on the surface of the water. You can see them and you can feel them. As you swim through the water‚ you can even make your own waves. The winds cause waves on the surface of the ocean (and on lakes). The wind transfers some of its energy to the water‚ through friction between the air molecules and the water molecules
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tsunami/earthquake and the 2010 Haiti earthquake. Disaster 1 – Japanese Tsunami and Earthquake On Friday the 11th of March 2011‚ a magnitude 9.0 Earthquake struck coastal waters‚ along a subduction zone‚ surrounding Japanese islands. At the time of the Earthquake‚ no one expected what was about to occur‚ one of the most devastating tsunamis to have ever hit Japan. Earthquakes are caused by forces deep within the Earth when two blocks of the earth suddenly slip past one another.
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|THE TEARDROP OF THE INDIAN OCEAN: | | | |It’s Most Valuable Cash Crop | |
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Relieving Chile and Haiti Many earthquakes strike different countries and very often‚ and they face efforts to rebuild the nation. Some countries do it better than others and some are more effective. But‚ this does not only apply to earthquakes but also to other natural disasters such as floods and droughts. In such situations‚ humanitarian and development aid rush in from different corners of the world and from the countries government. The aid that is received goes into the relief efforts of the
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examples of earthquakes‚ assess the extent to which attempts at prediction and mitigation may have influenced the impact of the hazard. An earthquake is the result of a sudden release of energy in the Earth’s crust that creates seismic waves. Earthquake is a major threat to the human and natural environments‚ in which people died‚ buildings collapsed and cities destroyed. Prediction and mitigation are usually conducted in order to reduce the impact of an earthquake on environment. Earthquake prediction
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legend of the Earthquake Once upon a time‚ it was a dark and ominous day and trouble was arising in the underworld. Shiva the goddess of death and destruction had finally finished her mighty plans to take back what was rightfully hers. her plan was to swoop in from behind the city of peace ‚ and raid the museum of everything sweet and sour and steel the orb of tranquillity. Though to her surprise when she arose from the cavern of raw meat‚ Their awaited Johnny Mon Soony and Snoop Dogg. The most
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Change Over Time: Indian Ocean The Indian Ocean trade began in 650 A.D. and lasted until 1750. When the Indian Ocean trade began it was very simple but over the years there were many changes. The desire to have more goods had increased and soon enough so did technology which made the Indian Ocean trade more efficient. The Indian Ocean trade was influenced by variation of many political power and it was the key-factor to the east-west exchange connecting non-neighboring countries and the spreading
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The Ocean Specific Purpose: To inform my audience about the ocean and the benefits the ocean has on us. Central Idea: We have not discovered a majority of the ocean and I wanted to share why we have not done that. To inform that the ocean is very valuable and that we need to spend more time on really discovering what is down there. Introduction I. The ocean covers more than 70% of the planet’s surface. II. 95% percent remains unexplored‚ and unseen by the human eye. III. Over one million
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Investigating Earthquakes – Japan Gurjit & Ashwin Preliminary questions: a. Why do earthquakes happen in this location? b. Does this location fall on any fault lines? c. What are they doing to prepare themselves? d. How often earthquakes happen in this location? e. The last earthquake? f. The strongest earthquake? g. What are the hazards of earthquakes in this area? h. How are the structures built in this area Investigation: i. Japan is located in an area where several continental
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AN EARTHQUAKE IN AUSTRALIA Australia has a relatively low rate of seismicity due to its location towards the centre of the Indo-Australian Tectonic Plate. Earthquake activity is much higher around the margins of the Indo-Australian Plate‚ for example In places such as Indonesia‚ Papua New Guinea and New Zealand. Nevertheless‚ many historic earthquakes have Occurred in Australia and Geosciences Australia’s database (QUAKES) contains information on tens of thousands Of historic earthquakes in the
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