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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