Tuesday, January 26, 2016

Geology of the National Parks in Pictures - City of Rocks

The next up on my Tour of the Geology of the National Parks in pictures is:

Our last stop on this trip through Idaho was the City of Rocks National Reserve. As always, you can click on the pictures to enlarge the images. At the City of Rocks, it is possible to travel through the whole park in essentially one loop, however you must leave the park on the western edge to get between the northern and southern roads of the park. We decided to take the southern road first, following the available Automobile Tour, then loop around to the northern road to finish the park.

 It has been a long trip, so I ended up not getting out of the car for this one. But snapped the picture as I drove by regardless.

During our trip we followed the "Automobile Tour" and my wife had read about each of the stops along the way. This is Circle Creek Basin. The main part of the rocks are from a 28 million year old granitic dome named the Almo Pluton, which is the lighter colored granitic rocks. The darker brownish-gray rocks are the Green Creek Complex (a complex mainly consisting of granite, granitic gneiss, and schist), which is 2-3 billion years old and are some of the oldest rocks in North America.

Treasure rock, where we let our daughter get out for the first time to "go play on the rocks".

View of the most prominent feature of the park, the Twin Sisters and Pinnacle Pass (on the left half of the photo). This is the pass through which the California Trail followed. The left twin is made up of Green Creek Complex, and the right is Almo Pluton.

Side view of the Twin Sisters focusing on the Green Creek Complex sister in the foreground. The other twin is actually directly behind the formation with only the tip of it peaking over the center of the photo. The outcrop on the left half in the background is not one of the twins (I think).

Dike through the Almo Pluton.

This was the last picture before having to leave the park on the western edge to complete our loop on the northern road. You can see the natural jointing of the rocks in the background lining up with the eroded arch in the foreground. 

A rock formation lovingly called the Bread Loaves showing more jointing in the granitic pluton. This is the first formation after we came back into the park on our loop.

The northern part of the part had a lot more rock formations than the southern part and in general was much prettier. If you can only do part of the park, I recommend this part. 

Here is Window Arch, which is probably the best hike in the park. Especially for people with a 5 year old who can't walk that far.

The pathway up to Window Arch, through the Almo Pluton.

Some nice jointing in the Window Arch area.

Back along the road, on our way out looking into the City of Rocks, where it indeed looks like a bunch of "buildings" sticking up out of the ground.

Thursday, January 14, 2016

Drunk on Geology - Dubhe

The next up in our Drunk on Geology series is Dubhe Imperial Black IPA right here from Uinta Brewery out of Salt Lake City, UT. 

Dubhe was a word that I saw on the package and I had to Google it to determine if it was a geological word or not and what I found I was rather surprised about. It turns out that Dubhe is the end star of the Big Dipper (as highlighted on the package). 

From their website: 

"Named Utah's Centennial Star in 1996, Dubhe (pronounced Doo-bee) illuminates the front of the big dipper from 124 light years away. Dubhe, also known as Alpha Ursae Majoris, is a red giant that appears orange in color and has a mass 4x that of the sun."

The word dubhe, is an Arabic word meaning bear, which is fitting since the Big Dipper is small part of the larger Ursa Major (or the Great Bear). Dubhe is one of the two stars that point towards the North Star.