NORTH AMERICAN GRANITE LANDFORMS

The origin and age of granite landforms has long intrigued Geomorphologists. In order to estimate the rate at which these landforms change as a function of climate, particularly precipitation, we collected samples from three very different locations across the southern US including: the Alabama Hills of southern California (of John Wayne fame), the Llanno uplift of central Texas, and Stone Mountain in Georgia (of Olympic fame). We find that the granites in arid California are eroding mot slowly, on the order of a few meters per million years whereas the granites in Georgia are eroding more quickly, 5-10 m/My. Our initial data from the Stone Mountain area suggest it's been around a while. Erosion rates on the adjacent plain are 20m/My whereas the rock is eroding at about 7 m/My. Given this differential, the 220 m high Stone Mountain took upwards of 10 million years to obtain it current stature!

Llanno Uplift, Texas


ENCHANTED ROCK RISES ABOUT 100m ABOVE THE SURROUNDING PLANE


CHRISTINE MASSEY SITS ON A SHEET AT THE LOWER PART OF LITTLE ROCK

Alabama Hills, California




WEATHERD BOULDER FROM SIERRA NEVADA ON ALABAMA HILLS BEDROCK SURFACE


WEATHERED SURFACES OF THE ALABAMA HILLS


Georgia Piedmont



WEATHERING FEATURES ON STONE MOUNTAIN


THE TOP OF ARABIA MOUNTAIN APPEARS TO BE ERODING AT ABOUT 4 M/My




IT APPEARS THAT COSMOGENICALLY ESTIMATED MINIMUM MODEL RATES OF EROSION SCALE WELL WITH MEAN ANNUAL PRECIPITATION




For more information see


Bierman, P., Gillespie, A., Caffee, M. and Elmore, D. (1995). Estimating erosion rates and exposure ages with 36Cl produced by neutron activation. Geochimica et Cosmochimica Acta, 59, 3779-3798.

Bierman, P. (1994). Using in situ cosmogenic isotopes to estimate rates of landscape evolution: A review from the geomorphic perspective. Journal of Geophysical Research (special issue on Tectonics and Topography), 99, B-7, 13,885-13,896.


Research supported by PRIME, Purdue University; CAMS, Livermore National Laboratory; NSF, Geology and Paleontology. In collaboration with David Elmore (PRIME), Marc Caffee (LLNL), Alan Gillespie (UW), Milan Pavich (USGS)