
Friday, April 23, 2010
Postcard Friendship Friday: Bryce Canyon

Friday, April 16, 2010
PFF: Zion National Park

Thursday, November 12, 2009
Geology of Nevada: Postcard Friendship Friday
I have already blogged about my Geology of Utah postcard (on July 3!), so it's time to move on to Nevada. Utah is to the east, Idaho to the north, California to the West. the large areas of orange to the north of Nevada are fairly young volcanic rocks that extend into Idaho. there are some orange blotches to the south too. Note the pink, purple and blue bands oriented north-south, with pale yellow in between. This is the Basin and range part of the North American continent.[The following information is from a remote sensing tutorial published by NASA.]
Major C.E. Dutton, an early explorer of the American West, described these mountains as they appeared on a map as resembling "an army of caterpillars crawling northward out of Mexico".
Hmm, I see what he's saying. Below is a color - coded relief map (relief: the ups and downs of the landscape) of NV.
The mountains are uplifted parts of older continental crust. This area was being pulled apart, slowly, and the pieces in-between sank lower. The valleys are filled with a lot of sediment that has eroded from the ranges and partially filled them up. This is what the area looks like from the air.
[End quoting]Some of these peaks are significant. Wheeler Peak in Great Basin National Park is about 13,000 ft (4000 m) tall. What little rain or snow there is falls on these peaks and so the heights are green with pine trees, even white with snow. It is quite different from the dry, hot, desert valleys in between!
There is a wonderful part of the East Humboldt Range where erosion had sculpted the ridges in amazing ways, and the ridge is so thin that there is a hole right through it! This, of course, is called the Hole-in-the-Wall (or Lizzie's Window), near Hole-in-the-Wall Mountain. Please see this website for hiking in the area. The photos are amazing, but copyrighted, so I am not going to reproduce them here.
Las Vegas is way to the south of the state. Many areas in the middle of the state are very sparsely populated. With renewed gold mining in some areas in the north, population has grown somewhat.
Much more detail from about.com: http://geology.about.com/library/bl/maps/blnevadamap.htm
Nevada Bureau of Mines and Geology: http://www.nbmg.unr.edu/
Viridian
Friday, July 3, 2009
Utah: Postcard Friendship Friday

On the left is a geological map of Utah. Each color represents different rock that is exposed at the surface, or near the surface, just covered by soil. Without an explanation the colors mean very little so there is a key in the upper right. Here, different colors represent rocks of different ages. Yes, there is standard color scheme! Yellows are most recent rocks, or sediments recently deposited by rivers. Greens and aqua are Mesozoic rocks (time of the dinosaurs). Blue, gray-blue to brown colors are the older rocks (Paleozoic). Igneous rocks of what ever age get their own bright colors: reds, pinks, magenta. They really liven up a geologic map!
The lower right contains a cross section, as if you cut through the ground, took half away, and saw what was inside. Older rocks are on the bottom, younger on the top, as you might expect.The geology under Utah leads to amazing landscapes. Utah is the home of Bryce and Zion, also Arches National Park and many others. In the north are beautiful mountains and wonderful ski areas.