Mid- Atlantic ridge is a part of
constructive plate boundary or divergent plate boundary. This linear feature
lies in the midst of a two tectonic plates that are apart from each other.
Active divergent plate boundaries usually take place in the middle of oceanic
plates then become mid-oceanic ridges. In fact that a Mid- Atlantic Ridge is
mainly an underwater feature, some of its segments have an altitude that
extends above sea level. Its boundary is situated along Atlantic Ocean's bottom
and areas of the world's longest mountain range.
Answer:
$509
Explanation:
First, we find the lump sum to pay under the bank terms. The interest rate is 0.5% monthly, which is equivalent to 6.2% annually.
The formula is:
Where:
- P = Present value
- i = interest rate
- n = number of compounding periods of the interest rate
- X = lump sum we need to find
Now, we simply plug the amounts into the formula:
Next, we find the value of the lump sum under the company's preferred terms:
Finally, we susbtract the two figures to find the difference:
Glaciers carry soil from one place to another. This means that a lot of the fertile soil used mainly for that one area could have been taken away and effected negatively because the fertile soil on the bottom isn't as good as the one on the top, which has been dragged away by glaciers. However, it can take soil to environments where soil is needed, helping it.
(So sorry but the same questions get the same answers lol)
The correct answer is - True.
The transform boundaries of the tectonic plates are boundaries where two tectonic plates are sliding against each other. As they do that, they do create geological activity around the boundary, and earthquakes are a common occurrence. Another trademark of these boundaries are the faults, that stretch for several km in a linear manner, usually parallel to the boundary itself. Most of these faults are located in the ocean basins and they are connecting the offsets of the mid-ocean ridges, but they can also be found on land, like it is the case in California.
