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Question 3·Hard·Central Ideas and Details

Until recently, geologists gauged the pace of coastal erosion mainly by comparing maps and shoreline surveys recorded decades apart. The advent of high-resolution satellite imagery, however, allows scientists to trace shoreline changes annually, revealing variations that long-term averages hide. One study of Alaska’s north coast demonstrated that, while the coastline receded an average of two meters per year between 1950 and 2000, annual retreat rates during the 2010s oscillated between less than one meter and more than six meters. Such findings warn against assuming that the past half-century’s modest rate will persist. They also highlight the necessity of combining historical records with contemporary observations to obtain a fuller picture of how quickly—and unpredictably—the land is yielding to the sea.

Which choice best states the main idea of the passage?