evaporation is when a mass of water is hit by sunlight and some of it turns to a vapor. In the atmosphere, that vapor cools and the water molecules fuse with other water molecules, forming clouds. (condensation) When the clouds become full, the water precipitates onto land or into the ocean in the form of rain, sleet, snow or hail (precipitation).
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If you're an edge it's multiple choice and it would be c
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think of the model as the data that you would put on a spreadsheet and the diagrams as the different types of charts that you can use to view and interpret that data, for instance, a pie chart or bar chart
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Options (B)
Explanation:
New Zealand is an island country, located adjacent to the great pacific ocean. Whereas, the country of Australia is located towards the north-western side of New Zealand, at a distance of about 2500 miles.
The capital of Australia is Canberra, and the capital of New Zealand is Wellington.
Most of the interior Australia is comprised of desert where there occurs little or no rainfall, whereas there occurs large mountains at the central portion of New Zealand and is mainly due to the presence of active plate margin.
There are about 600 large islands in New Zealand, and majority of its population lives in Aukland, which is located in the extreme northern side of the country.
Thus, the correct statement is option (B).
Answer:
Explanation:
Rivers have three sections or courses: the upper course, middle course and lower course. The upper course of a river typically sees much erosion of bedrock in order to achieve the equilibrium mentioned above.
The upper course is also at the highest altitude as this is where the headwaters of the river originate. Rivers in the upper course erode down vertically which often creates a steep channel profile in what becomes the river valley.
The middle course sees a river at a slightly lower altitude than the upper course, but is still maintains a sense of trying to acquire equilibrium in flow and shape. The discharge and velocity of the river still allows the water to erode the banks and chart a course of least resistance through lateral erosion.
The lower course is unique as this is the stage in which a river has reached sea level. Here we find features not found in the middle and upper courses like floodplains and river deltas that have been formed by the sediment deposits of rocks and dirt gathered from upstream.
