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Trees, What Trees? EarthCache

Hidden : 4/7/2009
Difficulty:
1.5 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

The Bisti/De-Na-Zin Wilderness Area was not always a barren high desert; it was on the edge of an ancient inland sea with a forest, swamp and rivers. It was thought that there were cypress-like conifers and other plants towering as high as 200 feet.

South of the Bisti/De-Na-Zin Wilderness Area a fossil forest has been found and was so named because of the number of in situ fossilized tree stumps and logs found there. The logs you see here were more than likely washed down from the fossil forest and deposited where they have set for millions of years.

Changes occurring in the earth’s climate during the Cretaceous period, left remains of plants and animals buried in the thick sediment of sandstone, mudstone, and shale of the Fruitland and Kirkland Formation.





Creation of Petrified Wood:

Once a tree has fallen and is quickly covered by mud it will retain its shape before the decay process begins. As the trees start to decay, due to the anaerobic environment, volcanic ash with high concentrations of silica and other minerals dissolved in the water seep into the cells of the tree. As the water evaporates the minerals replace the cells of the tree making it look like the original tree, however heavier. Petrified wood weighs about 150 pounds per cubic foot and is considered one of the harder minerals, being rated between 7 and 8 on the Moh’s Hardness Scale.


Colors of Petrified Wood:

The color of petrified wood does not come from the wood itself but from the minerals that were in the water and mud during the petrifaction process.

Copper – green/blue
Cobalt – green/blue
Chromium – green/black
Manganese – pink
Carbon – black
Iron Oxides – red, brown, yellow
Manganese Oxides – black
Silica – white, grey


The Bisti/De-Na-Zin Wilderness Area is open year round, however the temperatures can be extreme during the summer and the roads and area can be impassable during rains, as the ground can become slippery and leaves footprints that can take years to disappear.

There are no developed trails or signs and you are encouraged to discover the wonders of the wilderness. Exploring the many carved out enclaves leading from the washes allows the opportunity to experience solitude and a primitive type of recreation.

The area is closed to motorized vehicles and mechanical forms of transportation (mountain bikes included). Also prohibited are campfires, collecting fossils or petrified wood, climbing on delicate geologic features, traveling in groups of more than eight people, and trespassing on adjacent tribal lands.


Directions:

To reach the Bisti/De-Na-Zin Wilderness Area off NW 371, go south about 36 ½ miles from the San Juan River crossing in Farmington and take a left turn on to Road 7297 (not county maintained). Follow the gravel road for about 2 miles to the Bisti parking lot. From Crownpoint go north on NM 371 about 46 miles, just past the Don Gleason Bridge over the De-Na-Zin Wash to the turn.

Topographic Maps for this area include: Alamo Mesa West, Alamo Mesa East , Bisti Trading Post, and Tanner Lake.


Note: This Earthcache can be accomplished during the same trip as “Bisti Badlands” (GC1NBCX) , they are in the same general area.


Logging Requirements:

You will need to take a tape measure with you to answer one of the questions.


The above coordinates will take you to a piece of petrified wood more than a mile from the parking area. To log this Earthcache:

1. Post a picture of you/your group exploring the area. Please do not post any pictures of this piece of wood. (Optional)

E-mail me the answers to these questions:

2. What may have made this piece of petrified wood the color it is?
3. Can you count the growth rings on this piece of wood?
4. How long is this log and what is the diameter?
5. The study of fossilized plants is called what (a little internet searching will help)? (Optional as of January 1, 2011)

Be sure that you provide your e-mail address when you send the answers to the above questions so that I can respond to your answers faster. I will respond to all, as I feel it is an important part of owning an Earthcache.

Other waypoints:

Turn Off from NM 371: 36 13.918 108 16.282
Parking Area: 36 15.736 108 15.173


References:

Bisti/De-Na-Zin Wilderness, Bureau of Land Management Wilderness Area Northwest New Mexico Brochure

New Mexico Bureau of Geology & Mineral Resources, New Mexico Institute of Mining & Technology, http://geoinfo.nmt.edu/index.html

Petrified Wood: To Become Stoney, http://www.earlham.edu/~tinkeem/web/petwood.htm
Sullivan, Robert M. 2006. Ah-shi-sle-pah Wilderness Study Area (San Juan Basin, New Mexico): A paleontological (and historical) treasure and resource. New Mexico Museum of Natural History and Science Bulletin 34:169-174.

U. S. Department of the Interior Bureau of Land Management Recreation Guidelines and Information: http://www.nm.blm.gov/recreation/recreation_guidelines.htm

Wolberg, Donald L. and Bellis, Diane, Report of the regional historical, stratigraphic, and paleontological framework of the Late Cretaceous Fossil Forest locality near Split Lip Flats, San Juan County, New Mexico


This Earthcache was placed with permission of the
Bureau of Land Management
Farmington Field Office



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