Page 446 - Atlas of Creation Volume 1
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FOSSIL SPECIMENS DISCOVERED IN MOROCCO






                          A large number of fossils from different periods have been discovered in Morocco, well known for its

                     400-million-year old trilobite fossils. Excavations in the Atlas Mountains and various other areas have
                     revealed Morocco's rich fossil beds.
                          Most frequently encountered in Morocco are echinoid fossils. Echinoid, the general
                     name for sea urchins, is actually the name given to a broad range of invertebrate

                     marine organisms. There are more than 800 species of these creatures, which
                     generally live on the sea bed, and specimens dating back 450 million years
                     can be found. Echinoids have been in existence for nearly half a billion
                     years, with all their complex structures and flawless mechanisms,

                     which in fact deals another severe blow to the theory of
                     evolution. These creatures, with all their structures fully
                     developed, lived at a time when evolutionists claim that
                     life was supposedly very primitive. And many of them

                     are still alive today, with those exact same structures.
                     They have remained unchanged for hundreds of
                     millions of years and never undergone
                     evolution.













































                                                                                                                     The  Atlas Mountains, extending
                                                                                                                     about 2400 kilometers (1500 miles)
                                                                                                                     have rich fossil beds. The highest
                                                                                                                     peak is Jbel Toubkal, with an
                                                                                                                     elevation of 4167 meters (13665
                                                                                                                     feet). The  Atlas Mountains were
                                                                                                                     formed millions of years ago when
                                                                                                                     the continents of  America and
                                                                                                                     Africa collided. It is assumed that
                                                                                                                     the Appalachians in North America
                                                                                                                     was the result of a similar
                                                                                                                     geological movement.




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