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Red Canyon Hoodoos EarthCache

Hidden : 5/15/2008
Difficulty:
1.5 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

A great quick stop at a new Visitors Center to learn a little geology about Red Canyon. You do not need to pay an entrance fee, and is available 24/7, year round.

Welcome to Red Canyon!


Photo courtesy of Wikimedia Commons

Red Canyon is a smaller version Bryce Canyon National Park, but the rock formations and geology that formed each landscape are the same. Here and at Bryce Canyon you will see many rock formations called Hoodoos.

Hoodoos are tall thin spires of rock that protrude from the bottom of arid basins and badlands. They are composed of soft sedimentary rock and are topped by a piece of harder, less easily-eroded stone that protects the column from the elements. They are mainly located in the desert in dry, hot areas. 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. (Geology purists do note that only a tall formation should be called a hoodoo; any other shape is called a 'hoodoo rock'.)

In addition to Red Canyon and other areas of the Colorado Plateau, hoodoos are commonly found in the Badlands regions of the Northern Great Plains (all in North America). 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. WED Enterprises (now Walt Disney Imagineering) notably based the design of the Disneyland version of the popular Big Thunder Mountain Railroad around a series of hoodoos, although these were constructed out of steel and concrete.

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. Minerals deposited within different rock types cause hoodoos to have different colors throughout their height. (adapted from Wikipedia)

To log this visit, please email the answers that can be found on the information plaque at the coordinates for the following questions:

  1. Oxygen reacted with what type of deposits to turn the sediments that form these rocks red?
  2. Where did the oxygen come from?
  3. Extra Credit: The hoodoos are composed of limestone. What test could you do to determine if a rock sample could be limestone or not?
    1. Scratch test
    2. Acid test
    3. Color test

Additional Hints (Decrypt)

Fvta vf ba gur fbhgujrfg fvqr bs gur ivfvgbef pragre, abegu raq. TCF fvtany znl whzc n ovg fvapr lbh jvyy or orarngu gur bireunat bs gur ohvyqvat.

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)