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This view is of the front of the active lava flow, looking upslope....
Pu‘u ‘Ō‘ō is partly obscured in the clouds at upper left.
Pu‘u ‘Ō‘ō is partly obscured in the clouds at upper left.
Pu‘u ‘Ō‘ō is partly obscured in the clouds at upper left.

This view is of the front of the active lava flow, looking upslope. Pu‘u ‘Ō‘ō is partly obscured in the clouds at upper left. Most surface activity on the advancing flow is actually where the flow widens, upslope of the flow front.

This view is of the front of the active lava flow, looking upslope. Pu‘u ‘Ō‘ō is partly obscured in the clouds at upper left. Most surface activity on the advancing flow is actually where the flow widens, upslope of the flow front.

The lava stream was flowing toward the photographer in this photo. ...
The lava stream was flowing toward the photographer in this photo. ...
The lava stream was flowing toward the photographer in this photo. ...
The lava stream was flowing toward the photographer in this photo. ...

The lava stream was flowing toward the photographer in this photo. Higher lava levels are preserved in the shelf-like protrusions on the darker orange wall to the left.

Vents on Pu‘u ‘Ō‘ō's northeast flank...
Vents on Pu‘u ‘Ō‘ō's NE flank
Vents on Pu‘u ‘Ō‘ō's NE flank
Vents on Pu‘u ‘Ō‘ō's NE flank

Several vents have opened on Pu‘u ‘Ō‘ō's northeast flank since last December. A spatter cone grew over one of the vents in mid-May and is visible at the center of the photo emitting bluish fume. In recent weeks, a vent opened upslope from (to the left of) the spatter cone, revealing bright incandescence.

Several vents have opened on Pu‘u ‘Ō‘ō's northeast flank since last December. A spatter cone grew over one of the vents in mid-May and is visible at the center of the photo emitting bluish fume. In recent weeks, a vent opened upslope from (to the left of) the spatter cone, revealing bright incandescence.

Though difficult to photograph, aerial views showed that this open ...
Though difficult to photograph, aerial views showed that this open ...
Though difficult to photograph, aerial views showed that this open ...
Though difficult to photograph, aerial views showed that this open ...

Though difficult to photograph, aerial views showed that this open vent was but a small window into a large, hot cavity beneath Pu‘u ‘Ō‘ō's northeast flank. Inside, streams of lava from an unseen source (or sources) closer to the crater rim (visible at lower right) were cascading toward the upper left into unknown depths.

Though difficult to photograph, aerial views showed that this open vent was but a small window into a large, hot cavity beneath Pu‘u ‘Ō‘ō's northeast flank. Inside, streams of lava from an unseen source (or sources) closer to the crater rim (visible at lower right) were cascading toward the upper left into unknown depths.

Small-scale map of flow field...
Small-scale map of flow field
Small-scale map of flow field
Small-scale map of flow field

This small-scale map shows Kīlauea's active East Rift Zone lava flow field in relation to the southeastern part of the Island of Hawai‘i. The area of the active flow field on June 8 is shown in pink, while widening and advancement of the flow field as mapped on June 10 is shown in red.

This small-scale map shows Kīlauea's active East Rift Zone lava flow field in relation to the southeastern part of the Island of Hawai‘i. The area of the active flow field on June 8 is shown in pink, while widening and advancement of the flow field as mapped on June 10 is shown in red.

Large-scale map of flow field...
Large-scale map of flow field
Large-scale map of flow field
Large-scale map of flow field

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area covered by the June 27th flow (now inactive) as of June 2 is shown in orange. The areas covered by the recent breakouts at Pu‘u ‘Ō‘ō as of June 8 are shown in pink, while widening and advancement of the active flow as mapped on June 10 is shown in red.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area covered by the June 27th flow (now inactive) as of June 2 is shown in orange. The areas covered by the recent breakouts at Pu‘u ‘Ō‘ō as of June 8 are shown in pink, while widening and advancement of the active flow as mapped on June 10 is shown in red.

Seafloor map with many different colors and shading to give a 3D effect and to display data with a color scheme.
Potential Marine Benthic Habitats of Monterey Canyon and Vicinity
Potential Marine Benthic Habitats of Monterey Canyon and Vicinity
Potential Marine Benthic Habitats of Monterey Canyon and Vicinity

The map on sheet 7 shows “potential” marine benthic habitats in the Monterey Canyon and Vicinity map area, representing a substrate type, geomorphology, seafloor process, or any other attribute that may provide a habitat for a specific species or assemblage of organisms.

The map on sheet 7 shows “potential” marine benthic habitats in the Monterey Canyon and Vicinity map area, representing a substrate type, geomorphology, seafloor process, or any other attribute that may provide a habitat for a specific species or assemblage of organisms.

Lava flow southeast of Pu‘u ‘Ō‘ō...
Lava flow SE of Pu‘u ‘Ō‘ō
Lava flow SE of Pu‘u ‘Ō‘ō
Lava flow SE of Pu‘u ‘Ō‘ō

The only active surface lava on Kīlauea's East Rift Zone is the flow that erupted from the lower east flank of Pu‘u ‘Ō‘ō on May 24, 2014. This flow continues to advance southeast, and was 3.3 km (2.1 mi) long today (June 10). This photo shows the front of the flow; Pu‘u ‘Ō‘ō is in the background.

The only active surface lava on Kīlauea's East Rift Zone is the flow that erupted from the lower east flank of Pu‘u ‘Ō‘ō on May 24, 2014. This flow continues to advance southeast, and was 3.3 km (2.1 mi) long today (June 10). This photo shows the front of the flow; Pu‘u ‘Ō‘ō is in the background.

Mauna Loa Southwest Rift Zone's eruptions stopped traffic—and more...
Mauna Loa Southwest Rift Zone's eruptions stopped traffic—and more
Mauna Loa Southwest Rift Zone's eruptions stopped traffic—and more
Mauna Loa Southwest Rift Zone's eruptions stopped traffic—and more

This rapidly moving ‘A‘ā lava flow was one of several that advanced down the west flank of Mauna Loa during the volcano's 1950 eruption. The massive flow, tens of meters (yards) high, traveled from the Southwest Rift Zone vent to the ocean, a distance of about 18 km (11 mi), in around 18 hours.

This rapidly moving ‘A‘ā lava flow was one of several that advanced down the west flank of Mauna Loa during the volcano's 1950 eruption. The massive flow, tens of meters (yards) high, traveled from the Southwest Rift Zone vent to the ocean, a distance of about 18 km (11 mi), in around 18 hours.

Large-scale map of flow field...
Large-scale map of flow field
Large-scale map of flow field
Large-scale map of flow field

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area covered by the June 27th flow (which may be inactive) as of June 2 is shown in orange. The areas covered by the recent breakouts at Pu‘u ‘Ō‘ō as of June 2 are shown in pink, while widening and advancement of the new breakouts as mapped on June 8 is shown in red.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area covered by the June 27th flow (which may be inactive) as of June 2 is shown in orange. The areas covered by the recent breakouts at Pu‘u ‘Ō‘ō as of June 2 are shown in pink, while widening and advancement of the new breakouts as mapped on June 8 is shown in red.

South Crillon Glacier
South Crillon Glacier
South Crillon Glacier
South Crillon Glacier

Nearly 60 years after a magnitude 7.7 earthquake struck Lituya Bay, Alaska — leading to a tsunami that devastated the area — six U.S. Geological Survey geologists revisited the isolated region of Alaska, to pick up where their scientific predecessors left off.

Nearly 60 years after a magnitude 7.7 earthquake struck Lituya Bay, Alaska — leading to a tsunami that devastated the area — six U.S. Geological Survey geologists revisited the isolated region of Alaska, to pick up where their scientific predecessors left off.

Fairweather Fault
Fairweather Fault
Fairweather Fault
Fairweather Fault

USGS research geologist Kate Scharer with her finger on the Fairweather Fault in southeast Alaska. The magnitude 7.8 Lituya Bay earthquake caused shaking that toppled trees along the fault, which left a break in the forest shown here.

USGS research geologist Kate Scharer with her finger on the Fairweather Fault in southeast Alaska. The magnitude 7.8 Lituya Bay earthquake caused shaking that toppled trees along the fault, which left a break in the forest shown here.

South Crillon Glacier
South Crillon Glacier
South Crillon Glacier
South Crillon Glacier

Periodic calving of ice from the snout of South Crillon Glacier.

Glacier Bay National Park
Glacier Bay National Park
Glacier Bay National Park
Glacier Bay National Park

Trench site along the southern Fairweather Fault, in Glacier Bay National Park, Alaska. The alluvial fan at left consists of lake, stream channel and debris flow deposits impounded by the Fairweather Fault scarp, at right.

Trench site along the southern Fairweather Fault, in Glacier Bay National Park, Alaska. The alluvial fan at left consists of lake, stream channel and debris flow deposits impounded by the Fairweather Fault scarp, at right.

Alaska field team
Alaska field team
Alaska field team
Alaska field team

The field team included USGS geologists Rob Witter, Adrian Bender, Chris DuRoss, Peter Haeussler, Richard Lease and Kate Scharer

The field team included USGS geologists Rob Witter, Adrian Bender, Chris DuRoss, Peter Haeussler, Richard Lease and Kate Scharer

Large-scale map of flow field...
Large-scale map of flow field
Large-scale map of flow field
Large-scale map of flow field

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area covered by the June 27th flow as of June 2 is shown in orange. The areas covered by the new breakouts at Pu‘u ‘Ō‘ō as of May 26 are shown in pink, while widening and advancement of the new breakouts as mapped on June 2 is shown in red.

This map shows recent changes to Kīlauea's active East Rift Zone lava flow field. The area covered by the June 27th flow as of June 2 is shown in orange. The areas covered by the new breakouts at Pu‘u ‘Ō‘ō as of May 26 are shown in pink, while widening and advancement of the new breakouts as mapped on June 2 is shown in red.

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