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Horizontal displacement vectors for GPS stations at Mount St. Helen...
Horizontal displacement vectors at Mount St. Helens (2008-2014)
Horizontal displacement vectors at Mount St. Helens (2008-2014)
Horizontal displacement vectors at Mount St. Helens (2008-2014)

Map of horizontal displacement vectors for Global Positioning System (GPS) stations in and around Mount St. Helens. Blue arrows show the direction and magnitude of horizontal movement, as measured at the GPS station from 2008-2014. The total horizontal displacement is indicated in millimeters (mm) and inches (in).

Map of horizontal displacement vectors for Global Positioning System (GPS) stations in and around Mount St. Helens. Blue arrows show the direction and magnitude of horizontal movement, as measured at the GPS station from 2008-2014. The total horizontal displacement is indicated in millimeters (mm) and inches (in).

Water-tube tiltmeter installed in 1956 in an underground vault near...
Water-tube tiltmeter installed in 1956 in an underground vault near...
Water-tube tiltmeter installed in 1956 in an underground vault near...
Water-tube tiltmeter installed in 1956 in an underground vault near...

The Uwekahuna WT (water-tube) instrument is still measured today, providing one of the longest records of deformation for any volcano. The tiltmeter is read by looking into the portal on each pot and adjusting the sight until two pins appear to touch.

The Uwekahuna WT (water-tube) instrument is still measured today, providing one of the longest records of deformation for any volcano. The tiltmeter is read by looking into the portal on each pot and adjusting the sight until two pins appear to touch.

Water-tube tiltmeter "pot" installed in 1956 in an underground vaul...
Water-tube tiltmeter "pot" installed in 1956 in an underground vaul...
Water-tube tiltmeter "pot" installed in 1956 in an underground vaul...
Water-tube tiltmeter "pot" installed in 1956 in an underground vaul...

The Uwīkahuna WT (water-tube) instrument is still measured today, providing one of the longest records of deformation for any volcano. The tiltmeter is read by looking into the portal on each pot and adjusting the sight until two pins appear to touch.

The Uwīkahuna WT (water-tube) instrument is still measured today, providing one of the longest records of deformation for any volcano. The tiltmeter is read by looking into the portal on each pot and adjusting the sight until two pins appear to touch.

Big Pine Volcanic Field, California, from southwest cinder cone, wi...
Big Pine Volcanic Field, CA, from SW cinder cone
Big Pine Volcanic Field, CA, from SW cinder cone
Big Pine Volcanic Field, CA, from SW cinder cone

Big Pine Volcanic Field, California, from southwest cinder cone, with US Route 395 and Owens River in view

Coconut grove and campground on the southern shoreline of Kīlauea V...
Coconut grove and campground on the southern shoreline of Kīlauea a...
Coconut grove and campground on the southern shoreline of Kīlauea a...
Coconut grove and campground on the southern shoreline of Kīlauea a...

Coconut grove and campground on the southern shoreline of Kīlauea Volcano at Halapē before 1975 magnitude 7.7 earthquake. Halapē was a popular hiking destination in Hawai‘i Volcanoes National Park.

Landslides in the Western Columbia Gorge, Skamania County, Washingt...
Landslides in the Western Columbia Gorge, Skamania County, WA, Scie...
Landslides in the Western Columbia Gorge, Skamania County, WA, Scie...
Landslides in the Western Columbia Gorge, Skamania County, WA, Scie...

Recent light detection and ranging (lidar) imagery has allowed us to identify and map a large number of previously unrecognized landslides, or slides, in heavily forested terrain in the western Columbia Gorge, Skamania County, Washington, and it has revealed that the few previously recognized areas of instability are actually composites of multiple smaller landslide

Recent light detection and ranging (lidar) imagery has allowed us to identify and map a large number of previously unrecognized landslides, or slides, in heavily forested terrain in the western Columbia Gorge, Skamania County, Washington, and it has revealed that the few previously recognized areas of instability are actually composites of multiple smaller landslide

Seismic hazard for the State of Hawaii based on past earthquakes an...
Seismic hazard for the State of Hawaii based on past earthquakes an...
Seismic hazard for the State of Hawaii based on past earthquakes an...
Seismic hazard for the State of Hawaii based on past earthquakes an...

Seismic hazard across the State of Hawaii, with high seismic hazards depicted with warm colors (red-orange) and relatively low seismic hazards depicted with cool colors (green). Engineers use these types of maps to prescribe building codes known as Seismic Design Codes (SDC) and create earthquake resistant structures.

Seismic hazard across the State of Hawaii, with high seismic hazards depicted with warm colors (red-orange) and relatively low seismic hazards depicted with cool colors (green). Engineers use these types of maps to prescribe building codes known as Seismic Design Codes (SDC) and create earthquake resistant structures.

The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...
The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...
The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...
The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...

Vectors indicate Pacific Plate motion relative to presumed fixed mantle hot spot in millimeters per year. Gray lines indicate fracture zones. Isochrons along the Emperor Seamounts chain show the age of volcanism in millions of years. Ocean floor ages from imagery available on EarthByte.

Vectors indicate Pacific Plate motion relative to presumed fixed mantle hot spot in millimeters per year. Gray lines indicate fracture zones. Isochrons along the Emperor Seamounts chain show the age of volcanism in millions of years. Ocean floor ages from imagery available on EarthByte.

Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...
Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...
Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...
Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...

Mount Adams elevation is 3,745 m (12, 286 ft). Mount St. Helens was the smallest of five major volcanic peaks in Washington State.

South Sister northwest flank. Right shoulder at skyline is thin she...
South Sister NW flank. Right shoulder at skyline is thin sheet of m...
South Sister NW flank. Right shoulder at skyline is thin sheet of m...
South Sister NW flank. Right shoulder at skyline is thin sheet of m...

South Sister northwest flank. Right shoulder at skyline is thin sheet of mafic material from 22ka summit eruption. Red cinders in headwall cirques are layered with dipping lava flows.

South Sister northwest flank. Right shoulder at skyline is thin sheet of mafic material from 22ka summit eruption. Red cinders in headwall cirques are layered with dipping lava flows.

USGS-CVO building sign, Vancouver, Washington....
USGS-CVO building sign, Vancouver, WA.
USGS-CVO building sign, Vancouver, WA.
Geologic Map of the Washougal Quadrangle, Clark County, Washington ...
Geologic Map of Washougal Quadrangle
Geologic Map of Washougal Quadrangle
Geologic Map of Washougal Quadrangle

Geologic Map of the Washougal Quadrangle, Clark County, Washington and Multnomah County, Oregon (Scientific Investigation Map 3257).

Geologic Map of the Washougal Quadrangle, Clark County, Washington and Multnomah County, Oregon (Scientific Investigation Map 3257).

Postshield eruption are the fourth stage of a Hawaiian volcano's ev...
Postshield eruption are the fourth stage of a Hawaiian volcano's ev...
Postshield eruption are the fourth stage of a Hawaiian volcano's ev...
Postshield eruption are the fourth stage of a Hawaiian volcano's ev...

Postshield eruption are the fourth stage of a Hawaiian volcano's evolution. A cap of evolved magma erupts to cover the surface of the volcano. Not all volcanoes have evidence for this phase.

Postshield eruption are the fourth stage of a Hawaiian volcano's evolution. A cap of evolved magma erupts to cover the surface of the volcano. Not all volcanoes have evidence for this phase.

Rejuvenated stage volcanism occurs after the volcano has moved away...
Rejuvenated stage volcanism occurs after the volcano has moved away...
Rejuvenated stage volcanism occurs after the volcano has moved away...
Rejuvenated stage volcanism occurs after the volcano has moved away...

Rejuvenated stage volcanism occurs after the volcano has moved away from the mantle hot spot. Eruptions occur in sporadic locations and may be interspersed with long periods of erosion.

Rejuvenated stage volcanism occurs after the volcano has moved away from the mantle hot spot. Eruptions occur in sporadic locations and may be interspersed with long periods of erosion.

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