Paper No. 7
Presentation Time: 3:10 PM


MITCHELL, Thomas M.1, SMITH, Steven A.F.2, ANDERS, Mark H.3, DI TORO, Giulio4 and CAVALLO, Andrea2, (1)Department of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, United Kingdom, (2)Istituto Nazionale di Geofisica e Vulcanologia (INGV), Via di Vigna Murata 605, Rome, 00143, Italy, (3)Department of Earth and Environmental Sciences, Lamont Doherty Earth Observatory of Columbia University, Palisades, NY 10964, (4)Dipartimento di Geoscienze, University of Padova, via G. Gradenigo, 6, Padova, 35131, Italy,

The Heart Mountain landslide of northwest Wyoming is the largest known terrestrial landslide on Earth. During its emplacement more than 2,000 km3 of Paleozoic sedimentary and Eocene volcanic rocks slid >45 km on a basal detachment surface dipping 2°, leading to 100 years of debate regarding the emplacement mechanisms. Recently, emplacement by catastrophic sliding has been favored, but experimental evidence in support of this is lacking. Here we show in friction experiments on carbonate rocks taken from the landslide that at slip velocities of several meters per second CO2 starts to degas due to thermal decomposition after only a few hundred microns of slip. This is associated with the formation of vesicular degassing rims in dolomite clasts and a crystalline calcite cement, microstructures that closely resemble those in the basal slip zone of the natural landslide. Our experimental results are consistent with an emplacement mechanism whereby catastrophic slip was aided by carbonate decomposition and release of CO2, allowing the huge upper plate rock mass to slide over a ‘cushion’ of pressurized material.