Item Number JLGt020
- Matte print on photographic paper
- 10-3/4" X 13-3/4" actual photo size
- 1-3/4" soft white matte (all around)
- 2-3/4" rustic/finished pine wood frame (all around)
- 19-3/4" X 22-1/2" finished size
- Shipping weight = 6lbs.
- Price = $150.00 (Includes shipping!)
- To purchase, call: (518) 915-4949
Or, send an e-mail to: jeff@jlgardnerphotography.com

I made the trip to Bryce Canyon the same weekend I toured and photographed Zion. I couldn't have asked for better weather and seeing these places in "off season" (not as many tourists) really made this adventure even more of a treat!

Here's something about Bryce Canyon from the National Park's website (http://www.nps.gov/brca/naturescience/index.htm): "Bryce Canyon National Park is a scientist's laboratory and a child's playground. Because Bryce transcends 2000 feet (650 m) of elevation, the park exists in three distinct climatic zones: spruce/fir forest, Ponderosa Pine forest, and Pinyon Pine/juniper forest. This diversity of habitat provides for high biodiversity. Here at Bryce, you can enjoy over 100 species of birds, dozens of mammals, and more than a thousand plant species."

"It is the uniqueness of the rocks that caused Bryce Canyon to be designated as a national park. These famous spires, called "hoodoos," are formed when ice and rainwater wear away the weak limestone that makes up the Claron Formation. However, the hoodoos' geologic story is also closely tied to the rest of the Grand Staircase region and the Cedar and Black Mountains volcanic complex. In short, Bryce has enough fascinating geology to fill a textbook."

And here's something about Bryce's mysterious "hoodoos": "Hoodoos are tall skinny spires of rock that protrude from the bottom of arid basins and "broken" lands. Hoodoos are most commonly found in the High Plateaus region of the Colorado Plateau and in the Badlands regions of the Northern Great Plains. While hoodoos are scattered throughout these areas, nowhere in the world are they as abundant as in the northern section of Bryce Canyon National Park. In common usage, the difference between Hoodoos and pinnacles or spires is that hoodoos have a variable thickness often described as having a "totem pole-shaped body." A spire, on the other hand, has a smoother profile or uniform thickness that tapers from the ground upward."

"At Bryce Canyon, hoodoos range in size from that of an average human to heights exceeding a 10-story building. Formed in sedimentary rock, hoodoo shapes are affected by the erosional patterns of alternating hard and softer rock layers. The name given to the rock layer that forms hoodoos at Bryce Canyon is the Claron Formation. This layer has several rock types including siltstones and mudstones but is predominatly limestone. Thirty to 40 million years ago this rock was "born" in an ancient lake that covered much of Western Utah. Minerals deposited within different rock types cause hoodoos to have different colors throughout their height."