Yellowstone National Park as an opportunity for deep continental drilling in thermal regions. [Abstract only]
Journal Article
·
· Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6019820
The Yellowstone caldera represnets the most intense magnatic and thermal anomaly within the conterminous United States. Voluminous rhyolite ash flows, accompanied by formation of huge calderas, occurred approximately 2.0, 1.3, and 0.6 My B.P. Although the last lava flow was about 70,000 B.P., much evidence suggests that magma may still be present at relatively shallow depth. The evidence from gravity and magnetic lows, magnetotelluric soundings, seismic wave velocities, maximum depths of earthquake foci, significant recent uplift of the caldera floor, and exceptionally high heat flux suggest that magmatic temperatures may be attained 5 to 10 km beneath much of the caldera. Most of the hot-spring and geyser activity occurs within the caldera and along a fault zone that trends north from the caldera rim through Norris Geyser Basin and Mammoth Hot Springs. The thermal waters and gases have been extensively sampled and analyzed over a period of 100 years. The chemical, isotopic, and hydrologic data obtained from natural discharges and from shallow wells drilled in thermal areas, enable formulation of models of the hydrothermal system. No previous intermediate-depth drilling has been conducted at Yellowstone to help select the best location for a deep drill hole, and because Yellowstone is a National Park, no commercial drilling will be available for add-on experiments. Also, a deep drill hole in Yellowstone would have to be sited with great regard to environmental and ecological considerations. Nevertheless, the large amount of existing data is sufficient to formulate testable models. The Yellowstone thermal anomaly is so extensive and scientifically interesting that almost any suitable drilling site there may be superior to the best drilling site in any other silicic caldera complex in the United States.
- Research Organization:
- Geological Survey, Menlo Park, CA
- OSTI ID:
- 6019820
- Journal Information:
- Geol. Soc. Am., Abstr. Programs; (United States), Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Vol. 15:5; ISSN GAAPB
- Country of Publication:
- United States
- Language:
- English
Similar Records
The geology and remarkable thermal activity of Norris Geyser Basin, Yellowstone National Park, Wyoming
Geology and remarkable thermal activity of Norris Geyser Basin, Yellowstone National Park, Wyoming
The boron isotope systematics of the Yellowstone National Park (Wyoming) hydrothermal system: A reconnaissance
Book
·
Thu Dec 31 23:00:00 EST 1987
·
OSTI ID:6533237
Geology and remarkable thermal activity of Norris Geyser Basin, Yellowstone National Park, Wyoming
Journal Article
·
Thu Dec 31 23:00:00 EST 1987
· U.S. Geol. Surv., Prof. Pap.; (United States)
·
OSTI ID:5362456
The boron isotope systematics of the Yellowstone National Park (Wyoming) hydrothermal system: A reconnaissance
Journal Article
·
Mon Oct 01 00:00:00 EDT 1990
· Geochimica et Cosmochimica Acta; (USA)
·
OSTI ID:6026682
Related Subjects
15 GEOTHERMAL ENERGY
150303* -- Geothermal Exploration & Exploration Technology-- Exploratory Drilling & Well Logging
150901 -- Geothermal Engineering-- Drilling Technology & Well Hardware
CALDERAS
DRILLING
GEOLOGIC MODELS
GEOPHYSICAL SURVEYS
LAVA
MAGMA
PUBLIC LANDS
SURVEYS
YELLOWSTONE NATIONAL PARK
150303* -- Geothermal Exploration & Exploration Technology-- Exploratory Drilling & Well Logging
150901 -- Geothermal Engineering-- Drilling Technology & Well Hardware
CALDERAS
DRILLING
GEOLOGIC MODELS
GEOPHYSICAL SURVEYS
LAVA
MAGMA
PUBLIC LANDS
SURVEYS
YELLOWSTONE NATIONAL PARK