Images

Frank Perret (left) and Thomas Jaggar (right) examine Cone Crater, Kīlauea southwest rift zone, during a return visit by Perret in 1914.

Pioneer Park in Bismarck, ND flooded by the Missouri River.

The Missouri River floods Pioneer Park and its shelter. Located in Bismarck, North Dakota.

Runoff due to recent wide-scale rainfall in South Dakota has led to very high streamflows for local Missouri River tributaries, according to several U.S.

High floodwaters on the Elk River upstream of Routt County Road 42 near Milner, CO.

High floodwaters on the Elk River upstream of Routt County Road 42 near Milner, CO

The boat ramp sign at Keelboat Park Boat Ramp in Bismarck, North Dakota.

Keelboat Park flooded by the Missouri River in Bismarck, North Dakota.

Souris River near Bantry, North Dakota flooding roadway.

The Garrison Dam flooding the boat ramp and boat dock.

Floodwaters partially submerge a USGS streamgage station near Slater, CO.

A roadway is broken down due to high streamflow near Slater, CO. A USGS streamgage can be seen next to the road.

Boreholes being drilled at Cinder Lake as part of a U.S. Geological Survey study to determine the feature's floodwater storage capacity. Cinder Lake, which is located on the Coconino National Forest, has been used to store runoff from areas affected by the 2010 Schultz Fire outside of Flagstaff, Arizona.

Aerial view looking south toward a lava flow advancing through forest along the Roger James fishing access road. The recently active Puhi O Kalaikini delta is to the left. The current ocean entry at Ki is at upper right.

View of the active lava lake at Halema‘uma‘u. The lava upwells at the upper right corner of the lake (north) and sinks back down at lower left (south) where weak spattering is occurring.

Viewing looking west at Pu‘u ‘Ō‘ō. The summit gas plume is in the distance at upper right.

View looking north at the spatter cone on the northwest side of Pu‘u ‘Ō‘ō crater floor. The cone is about 6 m (20 ft) high.

A near-vertical look at a lava cascade inside the vent cavity of the Halema‘uma‘u Overlook vent.

Numerous spattering sources were active on the east end of the pond, causing pond level fluctuations throughout the day.

Looking down into the vent cavity of the Halema‘uma‘u Overlook vent. The black ring on the walls surrounding the lava pond is a high lava mark, outlining the height the lava rose during a recent rise/fall cycle.

A new spattering vent formed on the south side of the TEB shield, just before daybreak on February 4.