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fossil soil वाक्य

"fossil soil" हिंदी मेंfossil soil in a sentence
उदाहरण वाक्यमोबाइल
  • There are also occasional cemented claystone deposits, as well as numerous paleosols ( fossil soils ).
  • Without protection in anoxic sediments, amber would gradually disintegrate; it is never found buried in fossil soils.
  • Most fossil soils before the development of terrestrial vegetation in the Silurian are entisols, showing no distinct soil horizons.
  • Oligocene fossil soils of well drained woodlands ( red bands ) and swamps ( black spots ) in the Painted Hills, Oregon
  • The loess, loess-derived sediments and the many intercalating fossil soils overlying the " Rocourt soil complex " and the " scrapers.
  • Geological features such as geodes, chemical nodules, impressions of raindrops, and paleosols ( fossil soils ) are commonly found in this formation as well.
  • The horizons of fossil soils typically are sharply defined only in the top layers, unless some of the parent material has not been obliterated by soil formation.
  • Despite the difficulties of identification mentioned earlier, this makes paleopedology ( the study of fossil soils ) potentially very useful to understanding the ecological relationships in past ecosystems.
  • In north-central China, blankets of loess that were deposited during glacial periods alternate with paleosols ( fossil soils ) that formed during warmer and wetter interglacials.
  • The kinds of horizons in fossil soils are, though, generally the same as those found in present-day soils, allowing easy classification in modern taxonomy of all but the oldest soils.
  • Their northern limit ( except fossil soils ) is very sharply defined in North America by the limits of maximum glaciation during the Pleistocene, because ultisols typically take hundreds of thousands of years to form far longer than the length of an interglacial period today.
  • With the exception of some exceedingly old soils which have a clayey, grey-green horizon that is quite unlike any present soil and clearly formed in the absence of O 2, most fossil soils can be classified into one of the twelve orders recognised by this system.

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