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    1. TOEFL全新真試題

      時(shí)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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