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sediments at the edges of the continents and on the ocean ground, then lakes characterize an interruption to the smooth stream of the system.Glacier ice gives a singular document of brief-time period change, which is discussed in the part of this chapter coping with cyclical change. On an extended time scale, windblown dust in sediments from the deep Atlantic signifies that the Sahara first grew to become an enormous desert about 10-million-years in the past,

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