This first installment was written by me while traveling in Egypt, where I received word that US Highway 89 had been closed indefinitely due to a "geologic event". The Google Earth images really showed that this particular area is prone to geologic slumping. Enjoy!
(Note: I have removed dead links from the original story).
I am taking time out from my "Around the World" trip and writing from Luxor, Egypt where I visited King Tut's tomb today. Many friends, colleagues and one very special wife have written to me to share news of a giant slump that has closed State Highway 89 between Flagstaff and Page, Arizona. The Arizona Department of Transportation (ADOT) is calling this a "geologic event", one that occurred on the morning of February 20 (local Arizona time). ADOT has already produced an informative and image-rich video describing in engineering terms what happened to the road and what it might take to fix it (thanks to John P. for providing this link to me).
I can give an informal geological assessment of the rock failure as I travel that road often and am familiar with the geologic setting of that portion of the highway. It is one of the most scenic roads in all the state of Arizona.
View to the south of the Echo Cliffs (photo taken in winter, 2010). The older slump is also visible in the foreground and is a part of the recent slump area.
Great view of slump material which is common on this slope. The slump was caused by cohesion failure in the Triassic Chinle Formation. Anyone who travels Highway 89 north of Cameron will know the havoc that this shale and mudstone lithology creates in the bed of that highway. Motorists often "enjoy" a free massage since the clays and shales swell when wet, then contract as they dry.
The Chinle Formation exposed north of Cameron Arizona, displaying the soft nature of the shale, claystone and mudstone bedding. Photo taken on October 17, 2009.
Chuck LaRue of Flagstaff sent me this Google image of Highway 89 and the ancient slump is quite obvious from this vantage. Note how the white colored Navajo Sandstone clearly has slumped downslope just above the highway in this view. Note that road construction in the late 1950's curved around the westward protrusion of the slump material.
Same image with lines highlighting the prehistoric slump area. The solid red line shows where the rocks broke away from, the dashed yellow line is the top of the slump block. This mass of rock slid downslope about 250 to 300 feet. The age of slumping is unknown to me.
A 'Halfway Around The World' Assessment - As I can believe, ADOT geo-engineers are on site evaluating options. Some rumors suggest that the highway may closed up to one year. The bed failure of the highway necessitates a tedious detour around the slump to State Highway 98, making a trip from Flagstaff to Page some 50 miles farther. Some brave travelers may try the unpaved Coppermine Road but likely just once if they do (the road is quite bumpy). I am sure that one viable option is to quickly pave the Coppermine Road. Some have also said that maybe the "slump route" may be abandoned. Not likely.The road is too scenic and too direct for that and engineers rarely say, "We give up" these days. Look for a massive stabilization project on this slope, very similar to that undertaken on the Mesa Verde approach road in southwestern Colorado. (There huge portions of the Cretaceous Mancos Shale have often slipped, yet the National Park Service has completed very expensive and a well-engineered solution there. ADOT will do the same here, hopefully that will be landscape interpretive friendly, and we will be able to one day travel this great road again. However, this slope will also one day again slide downhill as it has for at least the last several hundred thousand years.
I can see why it's so popular. Great interpretations and combined use of photos and Google Earth. Nice!
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