TOEFL全新真試題

          時間:2021-06-12 14:24:15 試題 我要投稿

          TOEFL全新真試題

            READING COMPREHENSION

          TOEFL全新真試題

            Questions 1-9

            The ocean bottom ------a region nearly 2.5 times greater than the total land area of the

            Earth ---- is a vast frontier that even today is largely unexplored and uncharted. Until

            about a century ago, the deep-ocean floor was completely inaccessible, hidden beneath

            waters averaging over 3,600 meters deep. Totally without light and subjected to intense

            pressures hundreds of times greater than at the Earth s surface, the deep-ocean bottom

            is a hostile environment to humans, in some ways as forbidding and remote as the void

            of outer space.

            Although researchers have taken samples of deep-ocean rocks and sediments for

            over a century, the first detailed global investigation of the ocean bottom did not

            actually start until 1968, with the beginning of the National Science Foundation s Deep

            Sea Drilling Project (DSDP).Using techniques first developed for the offshore oil and

            gas industry, the DSDP s drill ship, theGlomar Challenger, was able to maintain a

            steady position on the ocean s surface and drill in very deep waters, extracting samples

            of sediments and rock from the ocean floor.

            The Glomar Challenger completed 96 voyages in a 15-year research program that

            ended in November 1983. During this time, the vessel logged 600,000 kilometers and

            took almost 20,000 core samples of seabed sediments and rocks at 624 drilling sites

            around the world. The Glomar Challenger s core samples have allowed geologists

            to reconstruct what the planet looked like hundred of millions of years ago and to

            calculate what it will probably look like millions of years in the future. Today, largely

            on the strength of evidence gathered during the Glomar Challenger s voyages, nearly

            all earth scientists agree on the theories of plate tectonics and continental drift that

            explain many of the geological processes that shape

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