Cf. Waythomas et al., A CATASTROPHIC FLOOD CAUSED BY DRAINAGE OF A CALDERA LAKE AT ANIAKCHAK VOLCANO, ALASKA, AND IMPLICATIONS FOR VOLCANIC HAZARDS ASSESSMENT, Geological Society of America bulletin, 108(7), 1996, pp. 861-871
Aniakchak caldera, located on the Alaska Peninsula of southwest Alaska
, formerly contained a large lake (estimated volume 3.7 x 10(9) m(3))
that rapidly drained as a result of failure of the caldera rim sometim
e after ca, 3400 yr B.P. The peak discharge of the resulting flood was
estimated using three methods: (1) flow-competence equations, (2) ste
p-backwater modeling, and (3) a dam-break model, The results of the da
m-break model indicate that the peak discharge at the breach in the ca
ldera rim was at least 7.7 x 10(4) m(3) s(-1), and the maximum possibl
e discharge was approximate to 1.1 x 10(6) m(3) s(-1). Flow-competence
estimates of discharge, based on the largest boulders transported by
the flood, indicate that the peak discharge values, which were a few k
ilometers downstream of the breach, ranged from 6.4 x 10(5) to 4.8 x 1
0(6) m(3) s(-1), Similar but less variable results were obtained by st
ep-backwater modeling. Finally, discharge estimates based on regressio
n equations relating peak discharge to the volume and depth of the imp
ounded water, although limited by constraining assumptions, provide re
sults within the range of values determined by the other methods, The
discovery and documentation of a flood, caused by the failure of the c
aldera rim at Aniakchak caldera, underscore the significance and assoc
iated hydrologic hazards of potential large floods at other lake-fille
d calderas.