A survey base station is established using a RTK-GPS receiver with mobile units to collect data points in and around the crater. Information will be used to monitor surface changes, deformation, erosion and aggradation inside the crater. This type of technology is precise to the centimeter. View to the south, toward Crater Glacier and the lava domes.
Images
![Precise surveying of Mount St. Helens crater with RTK-GPS technolog...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1207.jpg?itok=0s1M27gK)
A survey base station is established using a RTK-GPS receiver with mobile units to collect data points in and around the crater. Information will be used to monitor surface changes, deformation, erosion and aggradation inside the crater. This type of technology is precise to the centimeter. View to the south, toward Crater Glacier and the lava domes.
![Erosional channels lead away from the northern face of Crater Glaci...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1208.jpg?itok=0BTyLiwQ)
Crater Glacier, located inside the crater of Mount St. Helens, continues to move at an average rate of about 11 cm per day (4.3 inches). During warm weather months, meltwater creates erosional channels on the crater floor.
Crater Glacier, located inside the crater of Mount St. Helens, continues to move at an average rate of about 11 cm per day (4.3 inches). During warm weather months, meltwater creates erosional channels on the crater floor.
![The sound of summer: rockfall inside the crater of Mount St. Helen...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1209.jpg?itok=lAUGWtfl)
In summer, the crater of Mount St. Helens is filled with a near constant sound of rockfall from the steep 600 m high (about 2000 feet) crater walls. The falling rock kicks up ash and dust (pulverized rock) as it tumbles onto the crater floor. View of east crater wall.
In summer, the crater of Mount St. Helens is filled with a near constant sound of rockfall from the steep 600 m high (about 2000 feet) crater walls. The falling rock kicks up ash and dust (pulverized rock) as it tumbles onto the crater floor. View of east crater wall.
![Steam vent near 1980-1986 dome, in the crater of Mount St. Helens....](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1210.jpg?itok=mGLkG08N)
Steaming continues on the 1980-1986 dome. View to the south and the east arm of Crater Glacier.
Steaming continues on the 1980-1986 dome. View to the south and the east arm of Crater Glacier.
A fumerole near the 1980-86 dome keeps an open hole in the east arm of Crater Glacier. The hole is approximately 12 m (40 ft) in diameter, easily wide enough to hold a school bus and deep enough so you could not see the bus' top. View to the south.
A fumerole near the 1980-86 dome keeps an open hole in the east arm of Crater Glacier. The hole is approximately 12 m (40 ft) in diameter, easily wide enough to hold a school bus and deep enough so you could not see the bus' top. View to the south.
![Monitoring channel erosion and aggradation, Mount St. Helens (North...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1215.jpg?itok=hwrL9llZ)
Fieldwork includes direct observations of changes to streams and stream beds to determine how changes will affect the downstream transportation of sediments. Here, the braided North Fork Toutle (left) joins Carbonate Springs Creek (right). View to the east.
Fieldwork includes direct observations of changes to streams and stream beds to determine how changes will affect the downstream transportation of sediments. Here, the braided North Fork Toutle (left) joins Carbonate Springs Creek (right). View to the east.
![Ultraviolet spectrometer on roof of vehicle is driven beneath gas p...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img5058.jpg?itok=56VVvars)
The vehicle-based UV spectrometer is routinely driven beneath the summit and East Rift Zone gas plumes to measure sulfur dioxide gas emissions during typical trade-wind conditions.
The vehicle-based UV spectrometer is routinely driven beneath the summit and East Rift Zone gas plumes to measure sulfur dioxide gas emissions during typical trade-wind conditions.
![Earthen flow and Crater Glacier spill into upper Loowit Canyon, Mou...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1214.jpg?itok=qP99-dU3)
View of upper Loowit Canyon shows where Crater Glacier is spilling into the canyon (dark gray) and where an earth flow deposit (medium gray lobe inside canyon) occurred in early summer. View to the south.
View of upper Loowit Canyon shows where Crater Glacier is spilling into the canyon (dark gray) and where an earth flow deposit (medium gray lobe inside canyon) occurred in early summer. View to the south.
Visitors watching an eruption of Old Faithful Geyser from the Old Faithful Inn's balcony.
Visitors watching an eruption of Old Faithful Geyser from the Old Faithful Inn's balcony.
Mount Rainier is the backdrop for Eatonville, Washington.
Mount Rainier is the backdrop for Eatonville, Washington.
![Visitors stand on the observation deck at Johnston Ridge Observator...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1191.jpg?itok=coLP_p4l)
Visitors stand on the observation deck at Johnston Ridge Observatory at Mount St. Helens National Volcanic Monument.
Visitors stand on the observation deck at Johnston Ridge Observatory at Mount St. Helens National Volcanic Monument.
![Educators hiking at Mount Rainier with CVO and NPS staff during a t...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1188.jpg?itok=w59xZxYZ)
Educators hiking at Mount Rainier with CVO and NPS staff during a training at Mount Rainier, Washington.
Educators hiking at Mount Rainier with CVO and NPS staff during a training at Mount Rainier, Washington.
The Hawaii County Fire Department captured this image of Isaac Hale Park and boat ramp during their overflight of the area late this afternoon.
The Hawaii County Fire Department captured this image of Isaac Hale Park and boat ramp during their overflight of the area late this afternoon.
![The CVO Sediment Laboratory works closely with scientist in providi...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img1167.jpg?itok=yqClX9wC)
The CVO Sediment Laboratory works closely with scientist in providing authentic and reliable data to support their research.
The CVO Sediment Laboratory works closely with scientist in providing authentic and reliable data to support their research.
USGS scientists Jeff Cordova and Fletcher Brinkerhoff conducting LiDAR scans and a GPS survey within the burned area of the Yarnell.
USGS scientists Jeff Cordova and Fletcher Brinkerhoff conducting LiDAR scans and a GPS survey within the burned area of the Yarnell.
Burned area within the Yarnell Hill Fire near Yarnell Arizona.
Burned area within the Yarnell Hill Fire near Yarnell Arizona.
USGS scientists Jeff Cordova and Fletcher Brinkerhoff set up the LiDAR and GPS equipment to survey a burned watershed within the Yarnell Hill Fire.
USGS scientists Jeff Cordova and Fletcher Brinkerhoff set up the LiDAR and GPS equipment to survey a burned watershed within the Yarnell Hill Fire.
Center for the Study of Active Volcanoes (CSAV) students Javier Pacheco (Costa Rica) and Syegi Kunrat (Indonesia) participate in field studies at Mount St. Helens.
Center for the Study of Active Volcanoes (CSAV) students Javier Pacheco (Costa Rica) and Syegi Kunrat (Indonesia) participate in field studies at Mount St. Helens.
The ocean entry at Kupapa‘u Point remains active, with several lava steams entering the water creating a moderate plume.
The ocean entry at Kupapa‘u Point remains active, with several lava steams entering the water creating a moderate plume.
![Several birds take a closer view of the ocean entry. Narrow stream...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img2533_0.jpg?itok=Lv0ARP00)
Several birds take a closer view of the ocean entry. Narrow streams of lava were battered by the surf as they poured into the water.
Several birds take a closer view of the ocean entry. Narrow streams of lava were battered by the surf as they poured into the water.
![Practice is the key to protecting yourself during an earthquake...](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/vhp_img2907.gif?itok=fZLAjfWw)
Island residents are encouraged to practice "Drop! Cover! Hold on!" during the Great Hawaii ShakeOut drill at 10:17 a.m. on October 17, 2013. Taking these actions during an earthquake will greatly reduce your risk of injury or death. For more information, please visit http://shakeout.org/hawaii/.
Island residents are encouraged to practice "Drop! Cover! Hold on!" during the Great Hawaii ShakeOut drill at 10:17 a.m. on October 17, 2013. Taking these actions during an earthquake will greatly reduce your risk of injury or death. For more information, please visit http://shakeout.org/hawaii/.