http://www.azgs.az.gov/MarcusLandslide_2008.shtml
The slide is a 500,000 year old rock slide that has has a length of about 2 km from scarp crown to deposit toe (see Google Earth image below) and a deposit volume of about 5.25 million cubic metres. The elevation difference is about 500 m.
Two minor criticisms from me, though:
- The site does not give the lat/long of its location, which makes looking at it on Google Earth rather more difficult than it ought to be. The location of the crown is: 33°40'47.27"N, 111°48'1.31"W. The deposit extends almost due east from this point;
- The site states that "Poised for collapse, a heavy rain, a bolt of lightning, or an earthquake could have spontaneously triggered". It is highly unlikely that lightning would trigger failure.
Douglass, J., Dorn, R.I. and Gootee, B.F., 2004. A large landslide on the urban fringe of metropolitan Phoenix, Arizona. Geomorphology, 65, 321-336. doi:10.1016/j.geomorph.2004.09.022
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