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       Michael A. Stecker 
      
      masmd@sbcglobal.net 
       
       
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      Bryce Canyon National 
      Park 
      Introduction 
      Bryce Canyon National Park in southwestern Utah is named for a series of 
      horseshoe-shaped amphitheaters carved from the eastern edge of the 
      Paunsaugunt Plateau. Colorful red, brown, pink and white cliffs and spires 
      called hoodoos are the parks most prominent and aesthetically appealing 
      features.  
       
      Geology 
      During the Cretaceous Period (starting about 144 million years ago) a 
      great inland seaway extended over much of south central and western USA 
      into the area now occupied by Bryce Canyon. Over a 60 million year period 
      it depositing sediments that eventually became the sedimentary rocks of 
      the region -- the brown and gray marine rocks now exposed at the park's 
      lowest elevations and across the Paria Valley. Then, in the Tertiary 
      Period (66 - 40 million years ago) highlands to the west eroded into 
      shallow, broad basins. Iron-rich calcific sediments were deposited in the 
      beds of a series of lakes and streams. These became the reddish rocks of 
      the Claron Formation from which the hoodoos (pillar of rock, usually of 
      fantastic shape) are carved. About ten million years ago forces within the 
      Earth erupted creating the massive uplifts of the Aquarius and Paunsaugunt 
      plateaus. Rock layers on the Aquarius now tower 2,000 feet above the same 
      layers of the Paunsaugunt. Consequently, older Cretaceous layers now 
      rested side by side with younger Tertiary layers across fault lines. 
      Ancient rivers then carved the tops and exposed edges of these blocks, 
      removing some layers and sculpting intricate formations in others. The 
      Paria Valley was created and later widened between the plateaus. 
       
      History 
      The Paiute indians are the indigenous people of the Bryce Canyon region. 
      The first Euro-Americans to explore the area were Capt. Clarence E. Dutton 
      and John Wesley Powell in the 1870s. Many of today's place names come from 
      this time. Other names like Paunsaugunt (home of the beavers), Paria 
      (muddy water), Panguitch (water or fish) and Yovimpa (point of pines) were 
      derived from the Paiute language. The Paiutes were soon displaced by 
      emissaries of the LDS Church (Mormons). Prime among them was Ebenezer 
      Bryce for whom the canyon was named. In 1923 President Warren G. Harding 
      proclaimed part of the area as Bryce Canyon National Monument under the 
      Powell (now Dixie) National Forest. In 1924 legislation was passed to 
      establish the area as Utah National Park. In 1928 its name was changed to 
      Bryce Canyon National Park 
  
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