An outcrop composed of six tsunami deposits on the inland side of the lowland backing Stardust Bay over 0.5 miles from the sea. Brown soils developed into the top of each sand sheet and black tephra (air fall volcanic ash) layers between two of the sand deposits aided correlation of the six sand sheets across the study area.
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Images related to natural hazards.
An outcrop composed of six tsunami deposits on the inland side of the lowland backing Stardust Bay over 0.5 miles from the sea. Brown soils developed into the top of each sand sheet and black tephra (air fall volcanic ash) layers between two of the sand deposits aided correlation of the six sand sheets across the study area.
USGS Scientists Engaged in Field Work on the Aleutian Islands
USGS Scientists Engaged in Field Work on the Aleutian IslandsThree geologists scramble down a hillside on Sedanka Island that overlooks Stardust Bay. The geologists documented driftlogs stranded at elevations up to 60 ft above sea level and over 0.5 mile inland.
USGS Scientists Engaged in Field Work on the Aleutian Islands
USGS Scientists Engaged in Field Work on the Aleutian IslandsThree geologists scramble down a hillside on Sedanka Island that overlooks Stardust Bay. The geologists documented driftlogs stranded at elevations up to 60 ft above sea level and over 0.5 mile inland.
USGS Scientist Taking Notes in the Field, near Prehistoric Drift Log
USGS Scientist Taking Notes in the Field, near Prehistoric Drift LogGeologist takes field notes to document the discovery of a 30-foot long driftlog stranded more than 0.5 mi inland at Stardust Bay on the remote Alaskan island of Sedanka. The log, stranded at an elevation of more than 60 feet above sea level, was carried inland and deposited in 1957 by a large tsunami generated by the magnitude 8.6 Andreanof Islands earthquake.
USGS Scientist Taking Notes in the Field, near Prehistoric Drift Log
USGS Scientist Taking Notes in the Field, near Prehistoric Drift LogGeologist takes field notes to document the discovery of a 30-foot long driftlog stranded more than 0.5 mi inland at Stardust Bay on the remote Alaskan island of Sedanka. The log, stranded at an elevation of more than 60 feet above sea level, was carried inland and deposited in 1957 by a large tsunami generated by the magnitude 8.6 Andreanof Islands earthquake.
USGS scientist Thierry Work takes a sample from diseased coral at Tunnels Reef on the north shore of Kauai, Hawaii
USGS scientist Thierry Work takes a sample from diseased coral at Tunnels Reef on the north shore of Kauai, Hawaii
220 kV transmission lines running adjacent to Tongariro Volcano, Ne...
220 kV transmission lines running adjacent to Tongariro Volcano, Ne...220 kV transmission lines running adjacent to Tongariro Volcano, New Zealand, two days after the 6 August 2012 Te MÄri crater eruption.
220 kV transmission lines running adjacent to Tongariro Volcano, Ne...
220 kV transmission lines running adjacent to Tongariro Volcano, Ne...220 kV transmission lines running adjacent to Tongariro Volcano, New Zealand, two days after the 6 August 2012 Te MÄri crater eruption.
Exposed Tsunami Sand Layers in a Pit Excavated by Scientists
Exposed Tsunami Sand Layers in a Pit Excavated by ScientistsOn a ridge behind Stardust Bay at an elevation of 46 feet above sea level, a shallow pit reveals five sand sheets deposited by tsunamis in the past 1700 years.
Location: Stardust Bay, Sendanka Island, Alaska
Exposed Tsunami Sand Layers in a Pit Excavated by Scientists
Exposed Tsunami Sand Layers in a Pit Excavated by ScientistsOn a ridge behind Stardust Bay at an elevation of 46 feet above sea level, a shallow pit reveals five sand sheets deposited by tsunamis in the past 1700 years.
Location: Stardust Bay, Sendanka Island, Alaska
Hawaiian Volcano Observatory's Recent Earthquakes Web page from Tuesday, July 31, with earthquake shown as colored circles, according to their times of occurrence.
Hawaiian Volcano Observatory's Recent Earthquakes Web page from Tuesday, July 31, with earthquake shown as colored circles, according to their times of occurrence.
Examining layers of rock and ash in pyroclastic flow strata helps s...
Examining layers of rock and ash in pyroclastic flow strata helps s...Photo taken north of Mount St. Helens; view is to the south.
Examining layers of rock and ash in pyroclastic flow strata helps s...
Examining layers of rock and ash in pyroclastic flow strata helps s...Photo taken north of Mount St. Helens; view is to the south.
This image is a composite of a thermal image and a normal photograph, showing the coastal plain and pali. Red areas are warm portions of the flow field that were active in the past weeks or months, while yellow and white areas are areas of active breakouts.
This image is a composite of a thermal image and a normal photograph, showing the coastal plain and pali. Red areas are warm portions of the flow field that were active in the past weeks or months, while yellow and white areas are areas of active breakouts.
The lava pond in the NE portion of Pu‘u ‘Ō‘ō remains active, though...
The lava pond in the NE portion of Pu‘u ‘Ō‘ō remains active, though...The lava pond in the northeast portion of Pu‘u ‘Ō‘ō crater remains active, though the level of lava was low in the pit today. Over this past weekend, a small collapse of the rim enlarged the pit slightly. The lava pond is about 30 meters (100 feet) wide.
The lava pond in the NE portion of Pu‘u ‘Ō‘ō remains active, though...
The lava pond in the NE portion of Pu‘u ‘Ō‘ō remains active, though...The lava pond in the northeast portion of Pu‘u ‘Ō‘ō crater remains active, though the level of lava was low in the pit today. Over this past weekend, a small collapse of the rim enlarged the pit slightly. The lava pond is about 30 meters (100 feet) wide.
Andesite lava flow of Kerr Notch (near Sun Creek) developed columna...
Andesite lava flow of Kerr Notch (near Sun Creek) developed columna...Andesite lava flow of Kerr Notch (near Sun Creek) developed columnar joints as it cooled after it was deposited, Crater Lake, Oregon.
Andesite lava flow of Kerr Notch (near Sun Creek) developed columna...
Andesite lava flow of Kerr Notch (near Sun Creek) developed columna...Andesite lava flow of Kerr Notch (near Sun Creek) developed columnar joints as it cooled after it was deposited, Crater Lake, Oregon.
Debris flow damage following the 2012 Waldo Canyon fire, Colorado, U.S.
Debris flow damage following the 2012 Waldo Canyon fire, Colorado, U.S.
USGS scientist Deborah Bergfeld collects a gas sample from a fumarole on the flank of Akutan Volcano, Akutan Island, Alaska.
USGS scientist Deborah Bergfeld collects a gas sample from a fumarole on the flank of Akutan Volcano, Akutan Island, Alaska.
Steam rises from degassing fumaroles (middle right) and a boiling pool (middle left) on the flank of Akutan Volcano, Akutan Island, Alaska.
Steam rises from degassing fumaroles (middle right) and a boiling pool (middle left) on the flank of Akutan Volcano, Akutan Island, Alaska.
Lava fountains, occasionally surging to heights of 45-55 m (150-180 ft), erupted south and north of Keanakāko‘i Crater (top and middle fissures, respectively) and on the floor of Kīlauea Caldera (foreground fissure) in a spectacular summit eruption on July 19, 1974.
Lava fountains, occasionally surging to heights of 45-55 m (150-180 ft), erupted south and north of Keanakāko‘i Crater (top and middle fissures, respectively) and on the floor of Kīlauea Caldera (foreground fissure) in a spectacular summit eruption on July 19, 1974.
USGS geologist uses a UV spectrometer to detect gases from a fumarole
USGS geologist uses a UV spectrometer to detect gases from a fumaroleUSGS geologist uses a UV spectrometer to detect gases from fumarole at Crater Rock, Mount Hood.
USGS geologist uses a UV spectrometer to detect gases from a fumarole
USGS geologist uses a UV spectrometer to detect gases from a fumaroleUSGS geologist uses a UV spectrometer to detect gases from fumarole at Crater Rock, Mount Hood.
Exploring Mount Rainier: living near a volcano provides an opportu...
Exploring Mount Rainier: living near a volcano provides an opportu...Exploring Mount Rainier: living near a volcano provides an opportunity for field-based learning.
Exploring Mount Rainier: living near a volcano provides an opportu...
Exploring Mount Rainier: living near a volcano provides an opportu...Exploring Mount Rainier: living near a volcano provides an opportunity for field-based learning.
Surface flows on pali and coastal plain; small lava lake in Pu‘u ‘Ō‘ō
Surface flows on pali and coastal plain; small lava lake in Pu‘u ‘Ō‘ōSurface flows remain active on the coastal plain, but have retreated inland compared to their position last week. The active front is now about 1.3 km (0.8 miles) from the ocean.
Surface flows on pali and coastal plain; small lava lake in Pu‘u ‘Ō‘ō
Surface flows on pali and coastal plain; small lava lake in Pu‘u ‘Ō‘ōSurface flows remain active on the coastal plain, but have retreated inland compared to their position last week. The active front is now about 1.3 km (0.8 miles) from the ocean.
In addition to active flows on the coastal plain, lava flows were a...
In addition to active flows on the coastal plain, lava flows were a...In addition to the active flows on the coastal plain, lava flows were also active on the pali and at the base of the pali. Pu‘u ‘Ō‘ō and the Halema‘uma‘u plume are visible near the top of the image.
In addition to active flows on the coastal plain, lava flows were a...
In addition to active flows on the coastal plain, lava flows were a...In addition to the active flows on the coastal plain, lava flows were also active on the pali and at the base of the pali. Pu‘u ‘Ō‘ō and the Halema‘uma‘u plume are visible near the top of the image.
The lava lake on the northeastern edge of the Pu‘u ‘Ō‘ō crater floor is about 30 m (100 ft) across. It's level rises and falls with changes in pressure in the magma storage body beneath Pu‘u ‘Ō‘ō. Today, the lava lake was at a relatively low level, compared to its condition over the last few months.
The lava lake on the northeastern edge of the Pu‘u ‘Ō‘ō crater floor is about 30 m (100 ft) across. It's level rises and falls with changes in pressure in the magma storage body beneath Pu‘u ‘Ō‘ō. Today, the lava lake was at a relatively low level, compared to its condition over the last few months.
Several openings on the floor of the Pu‘u ‘Ō‘ō crater and along the Peace Day flow tube system continue to degas profusely. The only visible lava, however, is the small lava lake confined to a pit on the northeastern side of the crater floor. The lava lake has been present for the last several months.
Several openings on the floor of the Pu‘u ‘Ō‘ō crater and along the Peace Day flow tube system continue to degas profusely. The only visible lava, however, is the small lava lake confined to a pit on the northeastern side of the crater floor. The lava lake has been present for the last several months.