Fall and Spring are my favorite times of the year. It’s hoodie weather and not so hot that I can be outside and not be covered in a permanent layer of sweat. 

Photo/Oladimeji Odunsi on Unsplash.com
Photo/Oladimeji Odunsi on Unsplash.com
Photo/Oladimeji Odunsi on Unsplash.com

This turned out to be the best time to visit Cedar Breaks since it wasn’t very busy even though there was a lot of traffic in Cedar Canyon. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

The Fall colors on the way to Cedar Breaks became more vivid the higher in elevation I climbed.  

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

While at Cedar Breaks the wind was chilly and it even started to snow a little bit. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

The information for the following bit of this piece comes from the Cedar Breaks pamphlet I picked up at the Cedar Breaks visitor’s center. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

The 6,155 acres that makeup Cedar Breaks was designated a national monument in 1933 by President Franklin D. Roosevelt. However, the creation of Cedar Breaks has been millions of years in the making. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

90 million years ago Cedar Breaks was bordered to the east by an ancient sea. As the mountains of what would become Cedar Breaks aged, they shed sediments carried to the ancient sea by rivers and streams. As the sea drained, it exposed rock formations created by compressed layers of sediments. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

Moving ahead 60 million years, Lake Claron was created after the sea retreated east and a low-lying area filled with fresh water. The sediments that drained from the new mountains to the west went to the bottom of Lake Claron along with organic matter that helped create the brilliant kaleidoscope of colors that can be seen in the canyons of Cedar Breaks. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

Moving forward again, this time 20 million years ago, volcanic ash, molten rock, and earthquakes created the Brian Head Formation. For about the last 10 million years, earthquakes continuously lowered the landscape to the west, leaving Cedar Breaks at the highest elevation point of the Grand Staircase. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

Now, Cedar Breaks lies at the western edge of the Colorado Plateau’s Grand Staircase, which is higher, cooler, and wetter than the points to the east. Because of its location, Cedar Breaks supports species that thrive in high-elevation conditions including coyote mint, deer, elk, and pika. 

Photo/Deirdre Denali Rosenberg on Unsplash.com
Photo/Deirdre Denali Rosenberg on Unsplash.com
Photo/Deirdre Denali Rosenberg on Unsplash.com
Photo/Meredith Fontana on Unsplash.com
Photo/Meredith Fontana on Unsplash.com
Photo/Meredith Fontana on Unsplash.com

Speaking of pika, I became a pika parent after leaving the visitor’s center and adopting a pika I’ve named Perry. 

Photo/Andrea Wright
Photo/Andrea Wright
Photo/Andrea Wright

Get more information on Cedar Breaks National Monument at the link here.

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