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What's hot as lava, cold as snow, and larger than the state
of Rhode Island?
Yellowstone National Park! Spanning parts of Wyoming and Montana, Yellowstone
contains more than half the world's geysers and thermal activity, a landscape
that varies between high peaks and its own Grand Canyon,
and weather that can span all four seasons in one day.
In CR4's Animal Science blog,
I've written about my experiences observing the park's wildlife, which includes
bison, bears, elk, and wolves. Here, in the first installment of a four-part series,
Techno Tourist will guide you through geysers like the well-known Old Faithful,
as well as Yellowstone's less famous (but
perhaps more spectacular) thermal features. After wrapping up our visit to these
thermal areas, Techno Tourist will explore the Grand Canyon of Yellowstone and
visit Grand Teton National Park, Yellowstone's southern neighbor.
What are Thermal Features?
The term "thermal feature" sounds like a television special,
but it's actually a hole in the Earth's crust where hot water, steam (geysers),
and gases and vapors (fumaroles) can escape. Included in the list is the iconic
Old Faithful , which (because of its age) is
not so faithful anymore. When I visited Yellowstone, Old
Faithful was predicted to go off at 5:15 PM; it could be ten
minutes early or late. At 5:25, we were finally sprayed with mist as the wind
pushed the geyser's steam toward the crowd.
While geysers can be either intermittent (like Old Faithful) or continuous (like one of its neighbors),
fumaroles emit mixtures of steam and gas and are commonly called steam vents. Fumaroles
often release hydrogen sulfide, which oxidizes to sulfuric acid and sulfur. This
explains the horrible smell that wafts from and lingers around most of the
thermal features in the park. Some fumaroles smell worse than others, but all
of the areas with thermal activity have at least a hint of sulfur in the air.
Another big attraction in the thermal areas is the hot springs, or heated
pools of water. Heat from deep under the
Earth circulates near the water table and warms the springs. The pools are created as the water inches its
way up through cracks in the Earth's crust.
Temperatures average about 180 degrees Fahrenheit, but can reach over
400 degrees! There are, however, a few
pools in the park that are "cool" enough to take a dip in.
Editor's Note: Part 2 of this four-part series will run next
week, right here in TechnoTourist's Engineering Expeditions.
Resources:
http://www.usgs.gov/science/science.php?term=1149&type=feature
http://pubs.usgs.gov/gip/volc/geysers.html
http://www.yellowstoneparknet.com/roads_routes/mammoth_to_norris_geyser_basin.php
http://dsc.discovery.com/convergence/supervolcano/under/under.html
http://www.yellowstoneparknet.com/geothermal_features/hot_springs.php
http://whyfiles.org/022critters/hot_bact.html
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