In a river, erosion dominates at the cutbank. a. true
A cut bank, otherwise called a stream precipice or waterway cut bluff, is the external bank of a bend or wander in a water channel (stream), which is persistently going through erosion.
Cut banks are found in overflow along developed or wandering streams, they are situated outwardly of a stream twist, known as a wander, inverse the sneak off slant within the curve.
They are molded similar as a little precipice, and are shaped by the disintegration of soil as the stream slams into the waterway bank. Instead of a point bar, which is an area of statement, a cut bank is an area of erosion.
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The Crust and Lithosphere (which are almost synonymous) are not typically divided into two distinctive layers, so we can reject them.
The correct answer is is the core: (b). The inner core is solid and it's made of iron and nickel. The outer layer is liquid and this is the reason for the differentiation of the two parts.
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The geography of the United States is very different from one place to another, and it is due to the sheer size of the country, as well as all the geological activities that influenced it.
So if travel from state to state, different types of landscapes will appear, from semi arid and arid places in the west, across high mountains with dry plateaus as you move towards east, then vast lowlands through the central part of the country, and then smaller elongated mountains and hills, and at the end lowlands alongside the eastern coast of the country.
