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spring 04 / 17:1 - Grand Canyon River Guides

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own sources of error. Because the offsets in the flows on<br />

either side of the canyon are about the same, this<br />

strongly suggests that the Prospect Dam and Toroweap<br />

lava flows should also be about the same age. We draw<br />

this conclusion despite the uncertainties in the age<br />

dating.<br />

The take-home message from all of this is that every<br />

age reported in scientific literature, as well as every<br />

dating technique used to produce these ages, have their<br />

own uncertainties and sources of error. No age is, in fact,<br />

“set in stone,” but by using a variety of dating techniques<br />

to date the same lava flows or deposits, geologists<br />

produce ages that begin to converge on a “true age” of<br />

the lava flows or deposits. So, when people ask you “how<br />

old is the <strong>Grand</strong> <strong>Canyon</strong>” or “how long did it take to<br />

form”, gently explain to them that science has helped<br />

constrain the age of the big ditch to five to six million<br />

years old, depending upon whether you believe in<br />

creation science or not, but that the really interesting<br />

thing is that the age of the canyon beneath Toroweap<br />

Point is much younger than previously believed. Our<br />

work, combined with other researchers, suggests that this<br />

part of the canyon formed less than a million years ago<br />

and the river at Lava Falls arrived within 100 feet of its<br />

current depth about 500,000 years ago. By anyone’s idea<br />

of speed, that’s fast downcutting.<br />

Kaufmann, D., O’Brien, G., Mead, J.I., Bright, J., and<br />

Umhoefer, P., 2002. Late Quaternary <strong>spring</strong>-fed deposits in<br />

the eastern <strong>Grand</strong> <strong>Canyon</strong> and their implications for deep<br />

lava-dammed lakes, Quaternary Research, v. 58, p. 329-340.<br />

Lucchitta, I., G.H. Curtis, M.E. Davis, S.W. Davis, and B.<br />

Turrin, Cyclic aggradation and downcutting, fluvial<br />

response to volcanic activity, and calibration of soilcarbonate<br />

stages in the western <strong>Grand</strong> <strong>Canyon</strong>, Arizona,<br />

Quaternary Research, v. 53, 23-33, 2000.<br />

McIntosh, W.C., Peters, L., Karlstrom, K.E., and Pederson, J.L.,<br />

2002. New 40Ar-39Ar dates on basalts in <strong>Grand</strong> <strong>Canyon</strong>:<br />

Constraints on rates of Quaternary river incision and slip on<br />

the Toroweap fault and implications for lava dams: Geological<br />

Society of America Abstracts with. Programs, Rocky<br />

Mountain Section.<br />

McKee, E.D. and Hamblin, W.K., and Damon, P.E., 1968. K-<br />

Ar age of lava dams in <strong>Grand</strong> <strong>Canyon</strong>. Geol. Soc. Amer.<br />

Bull. 79: 133-136.<br />

Pederson, J., Karlstrom, K., Sharp, W., and McIntosh, W.,<br />

2002. Differential incision of the <strong>Grand</strong> <strong>Canyon</strong> related to<br />

Quaternary faulting – Constraints from U-series and Ar/Ar<br />

dating. Geology, v. 30, p. 739-742.<br />

Webb, R.H., Melis, T.S., Griffiths, P.G., Elliott, J.G., Cerling,<br />

T.E., Poreda, R.J., Wise, T.W., and Pizzuto, J., 1999, Lava<br />

Falls Rapid in <strong>Grand</strong> <strong>Canyon</strong>: Effects of Late Holocene<br />

debris flows on the Colorado <strong>River</strong>. U. S. Geol. Surv. Prof.<br />

Paper 1591, 90 pp. + map.<br />

Cassie Fenton & Bob Webb<br />

References:<br />

Dalrymple, G.B., and Hamblin, W.K., 1998. K-Ar ages of Pleistocene<br />

lava dams in the <strong>Grand</strong> <strong>Canyon</strong> in Arizona.<br />

Proceedings of the National Academy of Sciences, v. 95, p.<br />

9,744-9,749.<br />

Damon, P.E., Laughlin, A.W., and Percious, J.K., 1967. The<br />

problem of excess Argon-40 in volcanic rocks, in Proc.<br />

Symp. Rad. Dating and Methods of Low-Level Counting,<br />

Monaco 2-10 March, 1967: International Atomic Energy<br />

Agency: 24 p.<br />

Fenton, C.R., Poreda, R.J., Nash, B.P., Webb, R.H., and<br />

Cerling, T.E., Geochemical discrimination of five Pleistocene<br />

lava-dam outburst-flood deposits, western <strong>Grand</strong><br />

<strong>Canyon</strong>, AZ, Journal of Geology, v. 112, p. 91-110.<br />

Fenton, C.R., Webb, R.H., Pearthree, P.A., Cerling, T.E., and<br />

Poreda, R.J., 2001. Displacement rates on the Toroweap and<br />

Hurricane faults: Implications for Quaternary downcutting<br />

in <strong>Grand</strong> <strong>Canyon</strong>. Geology 29: 1,035-1,038.<br />

Hamblin, W.K., 1994, Late Cenozoic lava dams in the western<br />

<strong>Grand</strong> <strong>Canyon</strong>, 135 pp., Geological Society of America<br />

Memoir 183, 139 pp.<br />

Huntoon, P.W., 1977, Holocene faulting in the western <strong>Grand</strong><br />

<strong>Canyon</strong>, Arizona, Geological Society of America Bulletin,<br />

v. 88, p. 1619–1622.<br />

Jackson, G.W., 1990, Tectonic geomorphology of the Toroweap<br />

fault, western <strong>Grand</strong> <strong>Canyon</strong>, Arizona: Implications for<br />

transgression of faulting on the Colorado Plateau. Arizona<br />

Geological Survey Open-File Report 90-4, p. 1–66.<br />

page 10<br />

grand canyon river guides

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