Bill Evans, PhD (Former Employee)
Science and Products
Filter Total Items: 110
Geochemistry of natural gas manifestions from the Upper Tiber Valley (central Italy) Geochemistry of natural gas manifestions from the Upper Tiber Valley (central Italy)
Six natural gas manifestions from the upper Tiber Valley at Caprese Michelangela and Pieve S. Stefano (Arezzo) and at Umbertide (Pertugia) localities have been analysed for major, minor, trace gas compositions, as well as for ??13C in CO2 and CH4, ??15N in N2 and 3He/4He isotopic ratios. All gas emissions are CO2-rich (???94%), with N2 contents of 4-5%. Those from Caprese and Pieve S...
Authors
O. Vaselli, F. Tassi, A. Minissale, B. Capaccioni, G. Macro, William Evans
Multiple source components in gas manifestations from north-central Italy Multiple source components in gas manifestations from north-central Italy
Gas manifestations in north-central Italy consist of CO2-rich gases with minor N2-rich emissions and discharge either along with thermal springs or into cold and stagnant waters. 'Cold' gases are prevalently CO2-dominated (> 90%) while gases related to the thermal waters have variable composition: from CO2 > 99.5% to N2 > 90%. The variable composition of 'thermal' gases is caused by...
Authors
A. Minissale, William Evans, G. Magro, O. Vaselli
Mantle fluids in the San Andreas fault system, California Mantle fluids in the San Andreas fault system, California
Fluids associated with the San Andreas and companion faults n central and south-central California have high 3He/4He ratios. The lack of correlation between helium isotopes and fluid chemistry or local geology requires that fluids enter the fault system from the mantle. Mantle fluids passing through the ductile lower crust must enter the brittle fault zone at or near lithostatic...
Authors
B. Kennedy, Y.K. Kharaka, William Evans, A. Ellwood, D.J. DePaolo, J. Thordsen, G. Ambats, Robert Mariner
Knowledge of the fount and the cause of disaster Knowledge of the fount and the cause of disaster
No abstract available.
Authors
William Evans
Invisible CO2 gas killing trees at Mammoth Mountain, California Invisible CO2 gas killing trees at Mammoth Mountain, California
Since 1980, scientists have monitored geologic unrest in Long Valley Caldera and at adjacent Mammoth Mountain, California. After a persistent swarm of earthquakes beneath Mammoth Mountain in 1989, earth scientists discovered that large volumes of carbon dioxide (CO2) gas were seeping from beneath this volcano. This gas is killing trees on the mountain and also can be a danger to people...
Authors
Michael Sorey, Christopher Farrar, William Evans, David Hill, Roy Bailey, James Hendley, Peter Stauffer
Chemical and isotopic characteristics of fluids along the cameroon volcanic line, cameroon Chemical and isotopic characteristics of fluids along the cameroon volcanic line, cameroon
Results of the chemical and isotopic analysis of the water and gases discharged from volcanic crater lakes and soda springs located along the Cameroon Volcanic Line were used to characterize and infer their genetic relationships. Variations in the solute compositions of the waters indicate the dominant influence of silicate hydrolysis. Na+ (40-95%) constitutes the major cation in the...
Authors
G.Z. Tanyileke, M. Kusakabe, William Evans
Spatial radon anomalies on active faults in California Spatial radon anomalies on active faults in California
Radon emanation has been observed to be anomalously high along active faults in many parts of the world. We tested this relationship by conducting and repeating soil air radon surveys with a portable radon meter across several faults in California. The results confirm the existence of fault-associated radon anomalies, which show characteristic features that may be related to fault...
Authors
C.-Y. King, B.-S. King, William Evans, W. Zhang
Forest-killing diffuse CO2 emission at Mammoth Mountain as a sign of magmatic unrest Forest-killing diffuse CO2 emission at Mammoth Mountain as a sign of magmatic unrest
Mammoth Mountain, in the western United States, is a large dacitic volcano with a long history of volcanism that began 200 kyr ago and produced phreatic eruptions as recently as 500 ± 200 yr BP. Seismicity, ground deformation and changes in fumarole gas composition suggested an episode of shallow dyke intrusion in 1989–90. Areas of dying forest and incidents of near asphyxia in confined...
Authors
C. Farrar, M.L. Sorey, William Evans, J. F. Howle, B.D. Kerr, B. Kennedy, C.-Y. King, J. Southon
Degassing of Lake Nyos Degassing of Lake Nyos
No abstract available.
Authors
George Kling, William Evans, Michele L. Tuttle, Gregory Tanyileke
Chemical, isotopic, and dissolved gas compositions of the hot springs of the Owyhee Uplands, Malheur County, Oregon Chemical, isotopic, and dissolved gas compositions of the hot springs of the Owyhee Uplands, Malheur County, Oregon
Hot springs along the Owyhee River in southeastern Oregon between Three Forks and Lake Owyhee could be part of a north flowing regional system or a series of small separate geothermal systems Heat for the waters could be from a very young (Holocene) volcanic activity (basalt flows) of the Owyhee Uplands or the regional heat flow. The springs discharge warm to hot, dilute, slightly...
Authors
Robert Mariner, H.W. Young, William Evans
Six years of change in Lake Nyos, Cameroon, yield clues to the past and cautions for the future Six years of change in Lake Nyos, Cameroon, yield clues to the past and cautions for the future
The catastrophic release of gas from Lake Nyos, Cameroon, in 1986 caused substantial but incomplete mixing of the stratified water column. The post-release evolution of water-column structure has been monitored through April 1992. Changes began immediately after the event as rainfall and inflow brought dilute fluid into the surface layer. Inflow and surface mixing have gradually deepened...
Authors
William Evans, L. White, M. Tuttle, G.W. Kling, G. Tanyileke, R. Michel
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 110
Geochemistry of natural gas manifestions from the Upper Tiber Valley (central Italy) Geochemistry of natural gas manifestions from the Upper Tiber Valley (central Italy)
Six natural gas manifestions from the upper Tiber Valley at Caprese Michelangela and Pieve S. Stefano (Arezzo) and at Umbertide (Pertugia) localities have been analysed for major, minor, trace gas compositions, as well as for ??13C in CO2 and CH4, ??15N in N2 and 3He/4He isotopic ratios. All gas emissions are CO2-rich (???94%), with N2 contents of 4-5%. Those from Caprese and Pieve S...
Authors
O. Vaselli, F. Tassi, A. Minissale, B. Capaccioni, G. Macro, William Evans
Multiple source components in gas manifestations from north-central Italy Multiple source components in gas manifestations from north-central Italy
Gas manifestations in north-central Italy consist of CO2-rich gases with minor N2-rich emissions and discharge either along with thermal springs or into cold and stagnant waters. 'Cold' gases are prevalently CO2-dominated (> 90%) while gases related to the thermal waters have variable composition: from CO2 > 99.5% to N2 > 90%. The variable composition of 'thermal' gases is caused by...
Authors
A. Minissale, William Evans, G. Magro, O. Vaselli
Mantle fluids in the San Andreas fault system, California Mantle fluids in the San Andreas fault system, California
Fluids associated with the San Andreas and companion faults n central and south-central California have high 3He/4He ratios. The lack of correlation between helium isotopes and fluid chemistry or local geology requires that fluids enter the fault system from the mantle. Mantle fluids passing through the ductile lower crust must enter the brittle fault zone at or near lithostatic...
Authors
B. Kennedy, Y.K. Kharaka, William Evans, A. Ellwood, D.J. DePaolo, J. Thordsen, G. Ambats, Robert Mariner
Knowledge of the fount and the cause of disaster Knowledge of the fount and the cause of disaster
No abstract available.
Authors
William Evans
Invisible CO2 gas killing trees at Mammoth Mountain, California Invisible CO2 gas killing trees at Mammoth Mountain, California
Since 1980, scientists have monitored geologic unrest in Long Valley Caldera and at adjacent Mammoth Mountain, California. After a persistent swarm of earthquakes beneath Mammoth Mountain in 1989, earth scientists discovered that large volumes of carbon dioxide (CO2) gas were seeping from beneath this volcano. This gas is killing trees on the mountain and also can be a danger to people...
Authors
Michael Sorey, Christopher Farrar, William Evans, David Hill, Roy Bailey, James Hendley, Peter Stauffer
Chemical and isotopic characteristics of fluids along the cameroon volcanic line, cameroon Chemical and isotopic characteristics of fluids along the cameroon volcanic line, cameroon
Results of the chemical and isotopic analysis of the water and gases discharged from volcanic crater lakes and soda springs located along the Cameroon Volcanic Line were used to characterize and infer their genetic relationships. Variations in the solute compositions of the waters indicate the dominant influence of silicate hydrolysis. Na+ (40-95%) constitutes the major cation in the...
Authors
G.Z. Tanyileke, M. Kusakabe, William Evans
Spatial radon anomalies on active faults in California Spatial radon anomalies on active faults in California
Radon emanation has been observed to be anomalously high along active faults in many parts of the world. We tested this relationship by conducting and repeating soil air radon surveys with a portable radon meter across several faults in California. The results confirm the existence of fault-associated radon anomalies, which show characteristic features that may be related to fault...
Authors
C.-Y. King, B.-S. King, William Evans, W. Zhang
Forest-killing diffuse CO2 emission at Mammoth Mountain as a sign of magmatic unrest Forest-killing diffuse CO2 emission at Mammoth Mountain as a sign of magmatic unrest
Mammoth Mountain, in the western United States, is a large dacitic volcano with a long history of volcanism that began 200 kyr ago and produced phreatic eruptions as recently as 500 ± 200 yr BP. Seismicity, ground deformation and changes in fumarole gas composition suggested an episode of shallow dyke intrusion in 1989–90. Areas of dying forest and incidents of near asphyxia in confined...
Authors
C. Farrar, M.L. Sorey, William Evans, J. F. Howle, B.D. Kerr, B. Kennedy, C.-Y. King, J. Southon
Degassing of Lake Nyos Degassing of Lake Nyos
No abstract available.
Authors
George Kling, William Evans, Michele L. Tuttle, Gregory Tanyileke
Chemical, isotopic, and dissolved gas compositions of the hot springs of the Owyhee Uplands, Malheur County, Oregon Chemical, isotopic, and dissolved gas compositions of the hot springs of the Owyhee Uplands, Malheur County, Oregon
Hot springs along the Owyhee River in southeastern Oregon between Three Forks and Lake Owyhee could be part of a north flowing regional system or a series of small separate geothermal systems Heat for the waters could be from a very young (Holocene) volcanic activity (basalt flows) of the Owyhee Uplands or the regional heat flow. The springs discharge warm to hot, dilute, slightly...
Authors
Robert Mariner, H.W. Young, William Evans
Six years of change in Lake Nyos, Cameroon, yield clues to the past and cautions for the future Six years of change in Lake Nyos, Cameroon, yield clues to the past and cautions for the future
The catastrophic release of gas from Lake Nyos, Cameroon, in 1986 caused substantial but incomplete mixing of the stratified water column. The post-release evolution of water-column structure has been monitored through April 1992. Changes began immediately after the event as rainfall and inflow brought dilute fluid into the surface layer. Inflow and surface mixing have gradually deepened...
Authors
William Evans, L. White, M. Tuttle, G.W. Kling, G. Tanyileke, R. Michel
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.