Welcome!

This summer I am taking on the country with Harvey (My family's rv), my family, and dog Timber. And of course, my camera (an Olympus Pen-Ep3) and many, many, many books. Join us on this adventure through my pictures and writings.


Sunday, July 29, 2012

Zion and Snow Canyon (Snow Canyon State Park Post)

After a breakfast at Jacob Lake Inn (Dad wanted more cookies to replace the ones Timber ate.), Mom and I stopped in the Kaibab National Forest Visitor Center, and I found this little Kaibab Squirrel.  I named him Jake for the Jacob Lake.   
Meet Jake!
We headed off to Zion National Park, but didn't stay long, because it was crowded and to reach most places you would have to ride the shuttle.  It was almost 100 degrees, and the shuttle wasn't air-conditioned, and we didn't want to leave poor Timber alone even if the generator was running.  


Checkerboard Mesa - a Navajo Sandstone geological feature within the park.  The horizontal lines represent wind deposited sand that later was glued together by calcite and iron-oxide forming the sandstone.  The vertical lines are less common, as they are actually small cracks within the rock.  They represent stress and erosion on the rock's surface most likely from expanding and contracting water when it freezes then thaws.   


If you can see the two black holes in the rock, those are ventilation shafts in a tunnel we drove through!  




When we reached Snow Canyon, the thermometer told us it was about 105 degrees fahrenheit.  We decided it was too hot to explore the canyon tonight.  We stopped and found a campsite.

Don't be fooled, Snow Canyon is anything but cold!  It was named for its explorers, Lorenzo and Erastus Snow.    
An interesting patch of lava-rocks.  


This rock has the same cracks as Checkerboard Mesa in Zion.  

Until Later,
Amy

Saturday, July 28, 2012

More Hoodoos and Grand Holes (Grand Canyon North Rim Post)

Sorry yet again for the lack of posts over the past few days.  No, I haven't been slacking off, I just haven't had much phone service, so the air card hasn't worked.  

Anyway, we woke up and before the heat, and began our hike.  We walked down into the canyon on a trail laden with switchbacks.  As we were descending, we saw these hoodoos.   



Close to the bottom of the canyon, by looking up hikers would see this towering over them.  We wondered how it was staying up, as it looked like it would fall on our heads.  

Natural Bridge of Bryce Canyon.  



The hoodoos during our ascent.  
We left Bryce Canyon and worked our way to the North Rim of the Grand Canyon.  That wasn't before a stop to the Jacob Lake Inn to sample their famous Cookies!

And they were delicious!  This one is a Lemon Raspberry, and my favorite out of the cookies I got.  

On the lookout for the Kaibab Squirrel!
        The Kaibab Squirrel (Sciurus aberti kaibabensis) is the most distinct member of the tassel eared squirrels. They are also an excellent example of evolution due to geographical isolation.  They only live in the Kaibab Plateau in the Ponderosa Pine forests surrounding the North Rim of the Grand Canyon.  These squirrels are easily recognized by their tufted ears, dark gray bodies with a black belly and russet stripe down its back, and white tails.  The tufts on their ears grow as they age.  (My dad wanted to see a really old Kaibab squirrel.) The Kaibab Squirrel doesn't hibernate, so their unique coloring helps them camouflage with all the seasons.
         The Kaibab Squirrel's closest relative would be the Abert's Squirrel, which lives in the South Rim of the Grand Canyon, along with other Ponderosa Pine forests in the Rocky Mountains from the United States to Mexico.  At the time of the last ice-age, many Abert's Squirrels dispersed throughout the Grand Canyon area.  As the climate rose, the Ponderosa Pines, and the squirrels that depended on them moved to the higher Kaibab Plateau.  These became the descendants of the modern Kaibab Squirrel,  and as the climate cooled, the Abert's Squirrels moved back to their niches in the South Rim area.

Miles and Miles of Meadow!

The Grand Canyon was created due to erosion by the Colorado River, and the 5 exposed rock layers tell geologists something about many different time periods.  It has supported human life for 10,000 years, with evidence from Paleo-hunters, to ancestral Puebloans or Anasazi.  

Although the North and South Rims of the Grand Canyon are 10 miles apart as the crow flies or 215 miles by road, however, the North Rim averages about 1,000 feet higher and 10 degrees cooler than the South Rim. However, more tourists visit the South Rim.  Some people consider the North Rim prettier than the South Rim.  



In recreation of a picture Dad took on his trip out west 31 years , where he dangled his feet 2,000 feet down into Dead Horse Point. (They added a fence, so he couldn't recreate it there.)  He has gotten more cautious at 50, because he only dangled them onto the lower edge.  









We stopped at Cape Royal Point, and we reached it just before sunset.  The lighting and haze cast beautiful views across the canyon.  

Again, Uncle Chris, don't worry, I didn't look at the sun directly!


After we reached the RV, Dad and I walked Timber down to a picnic area and an area called the Wedding Point.  It was the perfect place to watch the sunset.

We decided we wanted to get Mom and Karen, and on our way back to get them, Mom pointed this out to me.

We went back to our spot at the Wedding Point, as it was the best place to watch the sunset.








Timber looks happy!