The coordinates of these endpoints can help us find the length and the midpoint, or the point that is halfway between the two endpoints, of the line segment. We can calculate the length of a line segment by using the Distance Formula, and we can calculate the midpoint of a line segment by using the Midpoint Formula.
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Much of Utah used to be covered by a prehistoric body of water called <u>Lake</u> <u>Bonneville</u>. Evidences of this include fossils of trilobites and fish in Utah's mountains.
Sedimentary rocks are comprised of sediments (small bits and pieces of weathered rock), and the reason sedimentary rock formations are usually layered is because they were formed underwater. The pressure of the water compacts the rocks, and as new sediments arrive in the water, it is compacted on top of the previous compressed rock, creating layers.
Since we know that much of Utah used to be a lake, the best explanation for this sedimentary rock limestone is that A. Western Utah used to be under water (an ocean or inland sea).
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Answer:
It's not linear because if any step of the method fails, you need to return to the beginning (for example, a false hypothesis)
Answer:
Explanation:
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Weathering is the breaking down of rocks, soil and minerals. Erosion is the process of being gradually worn away by natural agents such as wind and water.
Some rocks may be generally weaker which causes them to break down quicker than rocks that are stronger.
