Saturday, July 30, 2016

Petrified Forest National Park



It was raining when we entered the Petrified Forest National Park in Arizona.  The Painted Desert is a part of this park.  We were a bit discouraged that the day was foggy and drizzly and were sure we were not to see it in the best light.  But, when we stopped in the Visitor Center and spoke with a knowledgeable employee, he surprised us with the news that we were there on the best day.  He explained that the multi-hued layers of Navaho sandstone, mudstone, siltstone and claystone, which had absorbed the moisture from the rain, would enhance its color.

He was right.  While at the Painted Desert Inn, the fog began to lift and the Painted Desert began reveal itself in vivid relief. 
Painted Desert Inn

Painted Desert, Arizona
 



1934 Survey Bench Mark

Another special point of interest in this park is the Blue Mesa where we enjoyed more spectacular views from several overlooks.






Petrified wood can be seen at Crystal Forest and Giant Logs Trail.
Petrified Wood



Petrified wood, like many rocks and stones, is comprised primarily of the mineral quartz.  Quartz or silicon dioxide, as it is called by chemists, is formed of molecules of two atoms of the element oxygen and one atom of the element silicon.  Although quartz is colorless in its purest form, petrified wood usually is not because it contains small amounts of other elements which produce a variety of colors.
When the Colorado land plate shifted upwards, it raised the elevation of this area and caused it to change from rain forest to an arid.  This shift in climate caused the forest to petrify.
For those of you who wish for a scientific explanation of petrification, the following is from Wikipedia: 
Petrified wood; literally "wood turned into stone" is the name given to a special type of fossilized remains of terrestrial vegetation. It is the result of a tree or tree-like plants having completely transitioned to stone by the process of permineralization. All the organic materials have been replaced with minerals (mostly a silicate, such as quartz), while retaining the original structure of the stem tissue. Unlike other types of fossils which are typically impressions or compressions, petrified wood is a three-dimensional representation of the original organic material. The petrifaction process occurs underground, when wood becomes buried under sediment or volcanic ash and is initially preserved due to a lack of oxygen which inhibits aerobic decomposition. Mineral-laden water flowing through the covering material deposits minerals in the plant's cells; as the plant's lignin and cellulose decay, a stone mold forms in its place. The organic matter needs to become petrified before it decomposes completely. A forest where such material has petrified becomes known as a petrified forest.

Polished Petrified Wood in the Petrified Forest Museum






Another gem in the Petrified Forest.

New Route 66 Exhibit and Pull-Out Along Petrified Forest National Park Road
Petrified Forest, AZ – "A new paved pull-out has been developed along the park road within Petrified Forest National Park,” stated Superintendent Lee Baiza. This new pull-out showcases a section of the old Route 66 trace that passes through the park. From the vantage point that the pull-out offers, visitors can view the roadbed and a line of historic telephone poles. The roadbed and telephone poles mark the path of the famous “Main Street of America” as it passed through Petrified Forest National Park. From Chicago to Los Angeles, this heavily traveled highway was not only a road. It stood as a symbol of opportunity, adventure, and discovery. Petrified Forest National Park is the only National Park that contains a section of the old highway.


In addition to the new pull-out, a 1932 Studebaker exhibit has been installed adjacent to the newly developed area. The car was donated to the National Park Service by Frank and Rhonda Dobell, owners of Arizona Automotive Service in Holbrook, Arizona.








Friday, July 1, 2016

White Sands National Monument

Traveled 425 miles today from Santa Rosa, NM to Chambers, AZ.  Cell service was spotty for a good part of Rte. 54.  Points of interest were Lincoln County - Billy The Kid Country and Carrizozo Malpais (Spanish for badlands).

We stopped in Carrizozo at a restroom, and according to G, Kirk learned to play the tuba!  Meanwhile, in the women's room the handicap stall was occupied, and the other stall was missing the door, but a large, black trash bag was available to use as a handy temporary curtain.  Joan was so kind as to hold the garbage bag up to shield me in the stall from the casual observer.

The Valley of Fires is located in Carrizozo in central NM.  The Little Black Peak is a volcano vent.  Lava flowed out of the earth in the Tularosa Valley covering many square miles of buckled, twisted basalt lava, part of an extensive flow up to 165 feet thick and over 45 miles long that originated from several nearby volcanoes.

 
Google Image
 
 
Lava Flow
 
 
We visited the White Sands National Monument at Alamogordo, NM.  The white dunes encompass ten acres at an elevation of 4,235 feet.  The sand dunes are gypsum. 
 




 
Joan and I rented sleds and climbed the dunes to "sand sled."  We waxed the bottom of the sleds for more speed, but it wasn't nearly as fast as snow sledding.