In general, earthquake intensity is greatest in areas underlain by sediment.
When two earthen blocks abruptly slide past one another, it causes an earthquake. Fault or fault plane refers to the area where they slide. An earthquake's severity is quantified by its intensity, which is a number (written as a Roman numeral), which includes consequences on people, structures, and the earth's surface.
There are many different scales, for earthquake measurement but the Rossi-Forel scale and the Modified Mercalli scale are the two that are most frequently used in the US. The amount of soft soil that can be penetrated by seismic waves increases with the depth of the sediment layer above the bedrock. Greater wave size and amplification result from soft soil. To put it simply, the softer and thicker the soil, the higher the shaking or wave amplification.
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Answer:
This is because of isostatic adjustment.
Explanation:
The mountains of the Himalayas keep growing because of the isostatic adjustment. it allows for a gravitational balance in the Himalayan mountain region, which causes tectonic plates to float below these mountains. This fluctuation occurs in the densest part of the asthenosphere. This density, together with the force of gravity, causes an increase in the height of the tectonic plate that sinks more and more. As the tectonic plate sinks, inversely, this plate rises, when its weight decreases, and it is this rise that causes the mountain to grow.
Answer:
B. Great Plains.
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Again there isn’t a map but Olympia is the capitol of Washington state
Answer:
try to find a live feed of space
Explanation:
