Page 40 - Atlas of Creation Volume 1
P. 40

Where Are Fossils Mostly Discovered?


                          Fossils are widely dispersed just

                     about everywhere on Earth. Almost no
                     fossils are encountered in some types of
                     rock, but large numbers are found in
                     others. Geologists have divided rock

                     types into three main groups:
                          1. Igneous
                          2. Sedimentary
                          3. Metamorphic
                          The  igneous       category includes

                     granite or basalt-type rocks formed by
                     the cooling of magma present in the
                     depths of the Earth, or else emitted by

                     volcanoes in the form of molten lava.
                     Sedimentary rocks form when sand, silt,
                     mud, and other small particles or
                                                                                               The world's oldest rocks are in Greenland,
                     substances carried in water are                                           between 3.9 and 3.8 billion years old.

                     deposited on top of one another.
                     Metamorphic rocks are igneous or sedimentary ones that have undergone structural changes due to high
                     temperature and pressure deep in the Earth.
                                                        Few fossils are generally encountered in igneous seams. The rare examples

                                                   discovered are fossils that have resulted when a plant or animal gets trapped
                                                   inside molten lava. Very few fossils can survive the high temperatures and
                                                   pressures that transform sedimentary strata into metamorphic rock. Almost all
                                                   fossils are found in sedimentary seams or deposits.

                                                        Nearly all sedimentary rocks are formed by substances carried by wind or
                                                   water or else from the erosion of still other rocks. Some forms, such as coal, are
                                                   made of plant or animal remains. Clastic is the name given to sedimentary rock
                                                   formed by minute particles or grains. Sandstone and schist are examples of

                                                   such rocks. If there has been dissolution in the substances transported, then
                                                   due either to chemical solution or vaporization, "organic" sedimentary beds
                                                   form. Examples of such rocks are limestone and dolomite. In general,
                                                   sedimentary rock seams are a mixture of clastic and organic seams. Fossils are

             The age of rocks are determined by    usually seen in shales, schists, sandstone and limestone formed from calcium
             the researches made on the decay      carbonate.
             of radioactive minerals.

                          How Are Fossils Found and Extracted?


                          The tools used to collect fossils are simple ones such as those used by geologists:
                     hammers, trowels, various cutting implements, compasses, brushes and sieves.

                          Fossils sometimes appear on the surface when eroded out of the soft
                                       rock strata around them. In such cases, it is sufficient to
                                          clean the fossils with a brush. However, fossil
                                           collecting is not usually that easy. The rocks inside
                                           which they are concealed are generally very hard,

                                           and it can take hours to extract a fossil from its rocky
                                           matrix. First, it is important to determine from what
                                          point the rock should be broken. Fracture lines are





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