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ACKNOWLEDGMENTS

Liam Fiztgerald of Snowbird Ski Area for opinions on Provo
Canyon slidepaths.

Don Howlett of Alberta

Darwon Stoneman of Powderbirds Helicopters for timely ava-
lanche activity information.

Darce Trotter of Sundance Ski Area for avalanche control, his-
tory, weather data, etc.

UDOT Region Two Avalanche Forecasters

Utah Avalanche Forecast Center staff for information and opin-
ions.

Photograph Melanie Buck UDOT Media Production Specialist
Bridal Veil Falls Avalanche Path

"Snow Avalanches in Provo Canyon" Published in ISSW Pro-
ceedings 1994 by Kevin Griffith
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BV US6S Highlight
lines. Trees were broken on the north side of the highway
for a width of a 400 meters. Snow was deposited on the
uphill side of the highway in a debris pile 550 meters
wide with the toe of the deposition 180 meters beyond the
highway. The deepest part of the deposition was across
the Provo River from the slidepath on the county road. At
that point depth wasestimated to be 12 to 15 meters. There
were no reports of missing persons.
The events described above become less impressive
when compared to the fact that the Bridal Veil avalanche
was roughly thirty percent of the avalanche that released
around 1 A.M. January 31. Fracture propagationalong the
summit ridge of Cascade mountain connectedthree sepa-
rate drainages, Bridal Veil, Bunnell Fork, and Big Springs.
In addition to Bridal Veil, this massive slide ran the full
width of Bunnell Fork starting at3322 meters anddescend-
ing to 1920 meters. Fracture propagation continued hun-
dreds of meters into Big Springs, the drainage south of
Bunnells. The crown facethat connectedthese three drain-
ages wasover three kilometers wide andaveragedbetween
two and three meters deep. The total area involved was
approximately 530 hectares. The alphaangleof the Bridal
Veil portion of the slide was calculatedto be 26º 39'.
At the endof April theburiedrailroadcar wasstill under
avalanche debris. The roof started melting out at the end
of June and was halfway melted out by mid August. The
avalanchedebris on the county road had not melted when
this was written and the road was still closed. Several of
the conifir trees in the debris were approaching 300 years
in age. A conifir from a previous avalanche was over 300
years old.
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