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El Tablón (The Plank)

A cache by Isisfan Send Message to Owner Message this owner
Hidden : 02/10/2009
2 out of 5
1 out of 5

Size: Size: not chosen (not chosen)

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Geocache Description:

El Tablón (The Plank)

El Tablón (The Plank)

This Earthcache offers plenty of parking just off of 1-80 in Wyoming. There are many geological points of interest in this area. There is also an informational sign about 300 feet east of coordinates, which you can drive to.

As the Mesozoic Era ended 65 million years ago, the dinosaurs were dying out, and the Rocky Mountains were crumpling skyward. In concert with their rise, the forces of erosion began to work on these highlands and aprons of debris. Carried by wind and water, they spread out from their flanks. Throughout much of the Tertiary Period, the mountain summits barely poked above these vast plains of debris.

Then, in the Miocene Epoch (some 20 million years ago) a second, more general uplift of the Mountain West began, adding 5000 feet to elevations across the Colorado Plateau and Rocky Mountain Province. This uplift, which continued into the Pliocene, accelerated stream erosion throughout the region; the process was further enhanced by the cold, wet climate of the Pleistocene, as mountain glaciers carved deep canyons and massive amounts of meltwater carried away much of the erosional debris that had enveloped the mountains.

“The Gangplank” is a bridging grade between soft sedimentary rocks of the Plains and the hard granites of the Rockies, which here eroded down to less than 1,000 feet of additional climb above the plains surface. From the coordinates, the sedimentary rocks to the east (Late Miocene) are 10 million years old.

Recent History of El Tablón (The Plank)

When the transcontinental railroad was built n the 1860’s, Wyoming was the natural choice for crossing the Rockies. The railroad was built across Southern Wyoming, climbing west from Cheyenne on” the gangplank” of tertiary sediments that lapped onto the Laramie Range to the North, then across the Laramie Basin, crossing between the Snowy Range and Medicine Bow Mountains to the south.

"The Gangplank" is a wide, natural pass west of Cheyenne that offers a gradual climb between the watersheds of the North and South Platte Rivers. The Union Pacific line and Interstate 80 use this route today.

To log this cache, you must do the following:

A. Answer the questions in your own words, and to the best of your ability.

Bonus: B. Post a photo of yourself in the parking lot with the either the plains, the granite rocks, or the informational sign in the background. The pavement does not have to be included in your photo. ? You might also want to share any photos you take of the scenery, wildlife, or plant life in the area.

Photo not required, but answers are :)


1. The large granite rocks to the West of the coordinates are Pre-Cambrian in age. Estimate how old the rocks are in years (Example: Three million)

2. What does erosion mean?

Email your answers to:


Additional Hints (Decrypt)

Gur fvta fnlf vg nyy.

Decryption Key


(letter above equals below, and vice versa)

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