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Big
Rock Candy Mountain -
a colorful reminder of Utah's volcanic past
by Carl Ege
Oh the buzzin’ of the bees
In the cigarette trees
Near the soda water fountain
At the lemonade springs
Where the bluebird sings
On the big rock candy mountain
You may recognize this chorus from the folk song, “Big Rock
Candy Mountain,” attributed to Harry “Haywire Mac”
McClintock and made famous in a 1950s recording by Burl Ives.
View of Big Rock Candy Mountain from the north.
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Shortly after the release of the song in 1928, some local residents,
as a joke, placed a sign at the base of a colorful mountain in Utah
naming it “Big Rock Candy Mountain.” They also placed
a sign next to a nearby spring proclaiming it 'Lemonade Springs.'
These names stuck, and the mythical Big Rock Candy Mountain of the
song became perhaps one of the most recognized geologic sites in
west-central Utah.
Geologic Information: Located a few miles north of Marysvale
in Piute County, Big Rock Candy Mountain consists of altered volcanic
rock in various shades of yellow, orange, red, and white.
Closer view of Big Rock Candy Mountain.
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Approximately 22 to 35 million years ago, a cluster of stratovolcanoes
(volcanoes similar to Mount St. Helens) erupted, depositing large
volumes of lava and ash. Known as the Bullion Canyon Volcanics,
these volcanic rocks are more than 3,000 feet thick.
Approximately 21 million years ago, at least six magma bodies
intruded the overlying Bullion Canyon Volcanics. Through a complex
chemical process involving hydrogen sulfide, steam, ground water,
and oxygen, the original volcanic rock was partially altered or
totally replaced. The vivid colors that one sees at Big Rock Candy
Mountain are the direct result of this mineralization.
The yellow, orange, and red colors are from the presence of iron
minerals, such as jarosite, hematite, and pyrite. The white color
is due to the presence of alunite and kaolinite, minerals rich in
potassium.
Over
the past 15 million years, erosion has removed the distinct shapes
of the former volcanoes, and within the past several million years
has exposed the altered volcanic rocks in Marysvale Canyon along
the Sevier River.
How to get there: From Salt Lake City, travel south on I-
15 to I-70 (exit 132). Turn left (east) onto I-70 and travel 22.4
miles to exit 23. Turn right (south) onto U.S. Highway 89 for 7.6
miles to view Big Rock Candy Mountain from a distance. If you want
a closer view, travel an additional 0.6 miles to the Big Rock Candy
Mountain Resort. Please respect private property when at the resort.
Geosights article, Survey Notes,
v. 35 no. 3, August 2003
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