Since 2009 the U.S. Geological Survey has systematically monitored hydrothermal behavior at selected Cascade Range volcanoes in order to define baseline hydrothermal and geochemical conditions. Gas and water data have been collected at 25 monitoring sites on ten of the highest-risk volcanoes in the Cascade Range. These sites include summit-fumarole groups and springs/streams that show clear evidence of magmatic influence in the form of high 3He/4He ratios and (or) large fluxes of magmatic CO2 or heat. The monitoring data are intended to (1) be suitable for comparison with other continuous geophysical monitoring data and (2) provide baseline data that will be useful during future episodes of volcanic unrest in the Cascade Range. Site records...
Monitoring Yellowstone National Park’s hydrothermal systems and establishing hydrothermal baselines ...
This paper focuses on the role that hydrothermal systems may play in caldera unrest. Changes in the ...
Four groups of thermal springs with temperatures from 50 to 80 °C are located on the S–SW–W slopes o...
Since 2009 the U.S. Geological Survey has systematically monitored hydrothermal behavior at selected...
Fumarolic areas may be sensitive to volcanic unrest. However, limited data make interpretation of ...
Quaternary-age volcanic peaks of Mt. Lassen, Mt. Shasta, and Medicine Lake Volcano preferentially re...
Closer monitoring of hydrogeochemical changes in the Cascade volcanic arc has been in effect since 2...
Graduation date: 2007The basaltic landscapes of the Oregon High Cascades form a natural laboratory f...
This paper focuses on the role that hydrothermal systems may play in caldera unrest. Changes in the ...
The Twin Falls - Banbury area is one of many Known Geothermal Resource Areas located along the perip...
International audienceAt the hydrothermal stage, volcanoes are affected by internal and external pro...
Data collected on several occasions between 1983 and 1985 as part of a hydrologic monitoring program...
Persistently active volcanoes present short and long term variation in their magmatic, hydrothermal,...
Four groups of thermal springs with temperatures from 50 to 80 °C are located on the S–SW–W slopes o...
The Nevado del Ruiz volcano is considered one of the most active volcanoes in Colombia, which can po...
Monitoring Yellowstone National Park’s hydrothermal systems and establishing hydrothermal baselines ...
This paper focuses on the role that hydrothermal systems may play in caldera unrest. Changes in the ...
Four groups of thermal springs with temperatures from 50 to 80 °C are located on the S–SW–W slopes o...
Since 2009 the U.S. Geological Survey has systematically monitored hydrothermal behavior at selected...
Fumarolic areas may be sensitive to volcanic unrest. However, limited data make interpretation of ...
Quaternary-age volcanic peaks of Mt. Lassen, Mt. Shasta, and Medicine Lake Volcano preferentially re...
Closer monitoring of hydrogeochemical changes in the Cascade volcanic arc has been in effect since 2...
Graduation date: 2007The basaltic landscapes of the Oregon High Cascades form a natural laboratory f...
This paper focuses on the role that hydrothermal systems may play in caldera unrest. Changes in the ...
The Twin Falls - Banbury area is one of many Known Geothermal Resource Areas located along the perip...
International audienceAt the hydrothermal stage, volcanoes are affected by internal and external pro...
Data collected on several occasions between 1983 and 1985 as part of a hydrologic monitoring program...
Persistently active volcanoes present short and long term variation in their magmatic, hydrothermal,...
Four groups of thermal springs with temperatures from 50 to 80 °C are located on the S–SW–W slopes o...
The Nevado del Ruiz volcano is considered one of the most active volcanoes in Colombia, which can po...
Monitoring Yellowstone National Park’s hydrothermal systems and establishing hydrothermal baselines ...
This paper focuses on the role that hydrothermal systems may play in caldera unrest. Changes in the ...
Four groups of thermal springs with temperatures from 50 to 80 °C are located on the S–SW–W slopes o...