Answer:
mountain ridges creating natural divides
Explanation:
Natural boundaries acting as controls for water flow and makes them move into oceans are typically mountain ridges. They are geographically called divides.
Water generally flows from regions of high elevations to flat lands and plains.
Oceans the final basin where water from lands flows into. Ocean basins are located at very low elevation and through this potential head, gravity allows all land water to flow ocean-ward.
Mountains are sources of inland water bodies and they control how these rivers flows. Therefore, they act as natural divides that guides rivers into basins.
Mozart is t most commonly associated w AUS
Answer:
Explanation:
Given
Parallel to: 
Passes through (-9,-4)
Required
Determine the line equation
First, we calculate the slope (m) of the said line
Make y the subject
Divide through by 3
An equation has the general form:
Where
So:
Because the required line is parallel to , then they have the same slope of
Next, is to calculate the line equation using:
Where
This gives:
Open bracket
Green since the color reflected is the one that your eyes pickup.
<u>Answer:</u>
<u>The Continental drift</u> is the displacement of continental masses relative to each other. This hypothesis was developed in 1912 by Alfred Wegener, who affirmed <u>that thousands of years ago there was a single and unique supercontinent, called </u><u>Pangea</u><u>, which later became separated.
</u>
His formulations were based mainly on the way in which the forms of the continents seem to fit on each side of the Atlantic Ocean, such as Africa and South America. He also took into account the distribution of certain fossils that coincided in continents far from each other.
<h2>
At first this approach was discarded by most of his colleagues, because <u>
his theory lacked a logical and geological explanation for its epoch. </u></h2><h2>
</h2>
He proposed that the continents move on another denser layer of the Earth that made up the ocean floor. But it was not until the 1960s, with the development of the theory of tectonic plates, that the movement of the continents could be adequately explained.
