Answer:
Climactic plot structure is when the story begins at the height of the story, meaning the climax and then progresses to tell the events before the climax and the aftermath of the climax.
Explanation:
Climactic plot structure is different from other plot structures as it begins right from the exact moment of the climax. It is also known as "<em>en media res</em>" in literary terms. It literally means, "<em>in the middle of</em>", meaning the story starts at the middle of the story. This type of plot structure requires a background story of the 'how' and 'why' of the beginning of the story. It then comes to the climax, i.e. the start of the story line, and then proceeded to give a solution or ending of the plot. Examples of such type of narrative plot structures will include "The Odyssey" by Homer, "Divine Comedy" by Dante or the movies "Slumdog Millionaire", "Thor" or even "Gandhi" and "Forest Gump". The starting of the plot shows the event that is the climax, which then moves on to explain or show how or why that happened, then moves to the future scenes, the concluding plot of the story.
Explanation:
Methods of Desalination
At least three principle methods of desalination exist: thermal, electrical, and pressure. The oldest method, thermal distillation, has been around for thousands of years. In thermal distillation, the water is boiled and then the steam is collected, leaving the salt behind. However, the vaporization phase change requires significant amounts of energy. More modern methods of distillation make use of various techniques such as low-pressure vessels to reduce the boiling temperature of the water and thus reduce the amount of energy required to desalinate.
A second major type of desalination utilizes electric current to separate the water and salt. Typically, electric current will be used to drive ions across a selectively permeable membrane, carrying the dissociated salt ions with it. A key characteristic of this method is that the energy requirement depends on how much salt is initially present in the water. Consequently, it is suitable for water with initial salt concentrations but too energy intensive for sea water. [3]
A third principle method of desalination is reverse osmosis, in which pressure is used to drive water through a selectively permeable membrane, leaving the salt behind. [3] Similarly to electrically-driven separation, the amount of energy required for desalination depends on the initial salt content of the water. Again, this renders reverse osmosis unsuitable for sea water purification.
Atlantic Ocean, United states (below), Pacific Ocean (both oceans are on either side of Canada), and Alaska.
The closest layer of the atmosphere is called the Troposphere which extends up to about 7.5 miles into the atmosphere. The next layer is called the Stratosphere which extends from approximately 7.5 miles to 21.1 miles into the atmosphere. The next layer is called the Mesosphere which extends from from 21 miles to 49.7 miles up and the final level is the Thermosphere goes from 49.7 miles up to 195.6 miles into the atmosphere.
To form a fragmentary sedimentary rock, the fragments must be naturally compacted and cemented together.
Sedimentary rocks are made of sedimentary fragment and weathering from other rocks. Sedimentary rocks form at the Earth's surface, so they are easy to locate and study. An example of a Fragmentary Sedimentary rocks is shale.