Chapter 10: Problem 11
Explain how sediment liquefaction occurs in an earthquake and how it can cause damage. (F)
Chapter 10: Problem 11
Explain how sediment liquefaction occurs in an earthquake and how it can cause damage. (F)
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Get started for freeThe northeast-trending Ramapo fault crops out north of New York City. Precambrian gneiss forms the hills to the northwest of the fault, and Mesozoic sedimentary rock underlies the lowlands to the southeast. (You can see the fault on Google Earth by going to Latitude \(41^{\circ} 10^{\prime} 21.12^{\prime \prime} \mathrm{N}\), Longitude \(74^{\circ} 5^{\prime} 12.36^{\prime \prime}\) W. Where the fault crosses the Hudson River, there is an abrupt bend in the river. A nuclear power plant was built near this bend. Geologic studies suggest that the Ramapo fault first formed during the Precambrian, was reactivated during the Paleozoic, and was active again during Mesozoic rifting. Imagine that you are a geologist with the task of determining the seismic risk of the fault today. What evidence of present-day or past seismic activity could you look for? (B)
What types of structures are most prone to collapse in an earthquake? What types are most resistant to collapse? (I)
Compare normal, reverse, and strike-slip faults. (A)
Explain the differences among the scales used to describe the size of an earthquake. (E)
Is seismic risk greater in a town on the west coast of South (B) America or in one on the east coast? Explain your answer.
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