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USGS/Cascades Volcano Observatory, Vancouver, Washington

Volcano Observatories -
Taking the Pulse of Active Volcanoes


-- Excerpt from: Wright and Pierson, 1992,
Living With Volcanoes: The U. S. Geological Survey's Volcano Hazards Program: USGS Circular 1073, 57p.
To study active volcanism, the Volcano Hazards Program depends principally on the research and monitoring conducted at three permanent installations: the Hawaiian, Cascades, and Alaska Volcano Observatories*. Each observatory provides continuous and periodic monitoring of the seismicity, other geophysical changes, ground movements, gas chemistry, and hydrologic conditions and activity between and during eruptions. They also provide a detailed record of eruptions in progress. These observations serve to characterize eruptive behavior, identify the nature of precursory activity leading to eruption, define the processes by which different types of deposits are emplaced, and specify the hazards that could be unleashed by each kind of eruption. From direct observation of precursory signs, it is possible to anticipate eruptions. Underlying all observatory operations is an ongoing program of fundamental research in volcanic processes, supplemented by collaborative studies conducted at other USGS centers. Such research typically includes direct interpretation of the monitoring and eruption data, and it leads to formulation of conceptual models that can be tested by theoretical or laboratory simulations of volcanic systems.

The Hawaiian Volcano Observatory (HVO)

HVO is the U. S. Geological Survey's oldest such facility, founded in 1912 by Thomas A. Jaggar and run continuously by the USGS since 1948 (Heliker and others, 1986). It is located on the summit of Kilauea, one of the most active volcanoes in the world, on the Island of Hawaii. With the frequent eruptions at Kilauea and nearby Mauna Loa, HVO is a training ground for most of the volcanologists at the USGS. Many volcano-monitoring techniques used worldwide were originally developed at HVO, which is a testing ground for new techniques and instruments. The existence of HVO gave the USGS the unique capability of responding to activity at other U.S. volcanoes. When Mount St. Helens reawakened in March 1980, the USGS was well prepared to respond to the crisis. Scientists who had previously deciphered the volcanic history of Mount St. Helens, together with HVO alumni, quickly assembled to monitor the seismic activity and steam explosions. All worked together with the many agencies and public officials who were anxious to know when and if a large eruption was going to occur and what hazards it might create. Guided by USGS information, public officials designated zones of restricted access, and the loss of life from the May 18th eruption was thereby minimized, even though the timing of this event could not be precisely predicted.

Cascades Volcano Observatory (CVO)

After the devastating explosive eruption in 1980, the Cascades Volcano Observatory (CVO), in Vancouver, Washington, was founded and staffed with hydrologists, geologists, geochemists, and geophysicists (Brantley and Topinka, 1984). The observatory quickly broke new ground in its study of the ongoing eruption cycle at Mount St. Helens. In mapping and interpreting the origin of the deposits of the May 18 eruption, scientists had the unique advantage of direct observation of the landslides, eruption, and volcanic debris flows. Monitoring the growth of the lava dome in the crater of Mount St. Helens resulted in accurate predictions, 1 to 3 days in advance, of 16 out of 17 dome-building eruptions-an unprecedented feat in the young science of volcanology.

Alaska Volcano Observatory (AVO)

In 1988, the USGS added a third volcano observatory, the Alaska Volcano Observatory (AVO), in Anchorage and Fairbanks, Alaska, to expand and coordinate existing monitoring of the many active volcanoes along the Alaska Peninsula and in the Aleutian Islands. Many international flightpaths lie directly over Alaska, and the frequent eruptions of these volcanoes pose a serious hazard to aircraft far downwind. Study of Alaskan eruptions also provides more frequent opportunities to study volcanic activity similar to that of the less frequently active Cascade Range volcanoes.

Long Valley Observatory (LVO)*

In May 1980, just 1 week after the eruption at Mount St. Helens, a strong earthquake swarm occurred at Long Valley, California, site of a huge eruption of silicic magma about 700,000 years ago. The most recent volcanic activity in the area resulted in the formation of lava domes 550 years ago, accompanied by phreatic explosions that blanketed much of eastern California and western Nevada with volcanic ash (Bailey and others, 1976; Miller, 1985). Following the 1980 earthquakes, the USGS began monitoring Long Valley by setting up an observatory-like project operated from the USGS center in Menlo Park, California. Studies conducted since 1980 have documented almost 2 feet of uplift of the ground within the Long Valley Caldera and have accurately located earthquakes occurring as swarms in and around the caldera, the most recent of which took place in 1990 and 1991. The work at Long Valley is designed to monitor and interpret the current unrest and to make forecasts of any activity that might occur. Thus, the Long Valley project effectively constitutes a fourth volcano observatory in function and responsibilities, if not in name. The largest possible volcanic event at Long Valley, a catastrophic explosive eruption associated with renewed caldera collapse, is also the most difficult to forecast because of the long time interval between such eruptions and the absence of historically documented large caldera-forming eruptions anywhere in the world.

Yellowstone Volcano Observatory (YVO)*

The Yellowstone Volcano Observatory is the most recent U.S. volcano observatory. To strengthen the long-term monitoring of volcanic and earthquake unrest in the Yellowstone National Park region, on 14 May 2001 the U.S. Geological Survey (USGS), Yellowstone National Park, and University of Utah entered into an agreement to establish the Yellowstone Volcano Observatory (YVO). The goal of the observatory is to improve the existing collaborative study and monitoring of active geologic processes and hazards of the Yellowstone Plateau volcanic field and its caldera. The Observatory is supported by the U.S. Geological Survey, University of Utah, and the Yellowstone National Park. The park was the world's first National Park. It contains the largest and most diverse collection of natural thermal features in the world.


* Long Valley Observatory established as permanent observatory since this report was written. The Yellowstone Volcano Observatory was established in 2001. Information about the Yellowstone Volcano Observatory courtesy Volcano Hazards Program Website, 2002, and Yellowstone Volcano Observatory Website, 2002


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06/17/02, Lyn Topinka