UPDATE - On June 20, NASA's Earth Observatory web site showed before and after pictures from space of the Colbran, CO landslide. They are excellent views of the area and you can look at the images here. As mentioned briefly below, there curiously is a gas well located at the head of the slide. No one seems to be talking about this. Anyway, I mention the NASA site for two reasons, to see the before and after shots but also to highlight that on that site there is a link to my posting. It is the highlighted text in paragraph 3, telling readers to check out "these diagrams." Glad to know the folks at NASA EO are watching Earthly-Musings!
The landslide appears to have let loose beneath Sugarloaf Peak at an elevation of 9,400 feet. It "toes out" at about 7,400 feet (yep - landslides have toes). The map coordinates are N39.19078° W107.85518°. A view of the topography of this area can be viewed on Topoquest here. The road and aqueduct that were disrupted can also be seen on the map. Thanks to Chuck L. for this information.
It appears from Google Earth images that a previous slide had occurred on this slope. This slide is in the geologic past but most of the slides likely were active in the late Pleistocene Period, during the last Ice Age when conditions were much wetter here. There is some chatter on the web about the influence that fracking may have had on this, however it is apparent that slippage has occurred here long before fracking. Time will tell if this was a contributing cause or not.
The earth movement appears to be of a distinctive type called a Toreva landslide. These were first described in 1937 and named after the small Hopi Indian village of Toreva. The original article that describes these features can be accessed here. It makes for fascinating reading. See a complete treatment of Toreva blocks on Conor Watkins and J. David Rogers web site here.
The slide likely originated in the Green River and/or Wasatch formations, two of the younger rock units of the northern Colorado Plateau. These deposits are around 55 to 50 million years old and record deposition in ancient lakes and rivers. Here is a map to show the ancient setting of the deposit.
|Image from "Ancient Landscapes of the Colorado Plateau" by Ron Blakey and Wayne Ranney|
The landslide mass is approximately two miles long and 3/4's of mile wide near the top, thinning to about 1/2 mile wide in the middle. It covers about 700 acres. Jonathan White of the Colorado School of Mines was quoted on May 27 that a concern is that water is accumulating on top of the back-rotated block near the head scarp of the slide. This ponded water could further destabilize the huge mass of rock that has already slipped about 100 feet down.
Dan M. of Washington also sent me some really good geologic information on this particular area. You can access a USGS report on landslide studies of Grand Mesa here. Within the report are these two diagrams, showing how these features develop.
|From Baum and Odum, 1996|
|From Baum and Odum, 1996|