Images

New thermal feature beneath the boardwalk on Geyser Hill, Upper Geyser Basin. Boards removed for better observation. Pump Geyser is mound at end of boardwalk. Old Faithful Inn in distance.

An unnamed but charismatic thermal feature alongside Ferris Fork, near the Bechler River. The center of the pool is roiling with gas bubbles, but not boiling! The pool is only about 180 degrees F (81 degrees C), and all the gas is bubbling up from underground.

Mules loaded with sampling equipment and supplies for a mission to collect gas and thermal water samples from the Bechler River area in the southwest part of Yellowstone National Park. 

Ear Spring photographed on September 16, 2018. Rocks and other debris on the ground surrounding the spring were ejected during the September 15 water eruption. The spring is dry in this photo.

View of one of the geothermal seeps that flows into the Yellowstone River south of LaDuke Hot Spring.

Montana Bureau of Mines and Geology and Montana Tech scientists preparing for a UAV flight on the west side of the Yellowstone River adjacent from LaDuke Hot Springs.

Left: steel pipe with small temperature sensors placed every few inches. Right: temperature pipe installed in the streambed.

Serapeum, a Roman Marketplace in Pozzuoli, Italy, records deformation of Campi Flegrei caldera over two millennia.

Dragon’s Mouth in the Mud Volcano Area of Yellowstone National Park.

The Basalts of Warm River and Shotgun Valley, which erupted about 1.17 million years ago after the formation of Henrys Fork Caldera in southeast Idaho.  Photo by Brandi Lawler, University of Wyoming, August 8, 2018.

Hot spring waters with relatively high dissolved element concentrations on the floor of West Thumb, Yellowstone Lake. Image acquired by the Global Foundation for Ocean Exploration ROV Yogi on August 7, 2018.

Mushroom Pool, Lower Geyser Basin, Yellowstone National Park.

100 Spring Plain in Norris Geyser Basin, Yellowstone National Park.  The area is frequently flooded and impassable. Photo taken by Lauren Harrison in August 2018.

The Pinehaven Basalt, which erupted in Henrys Fork Caldera, southeast Idaho, about 35,000 years ago.  Photo by Brandi Lawler, University of Wyoming, August 6, 2018.

Fishing cone, a hot springs on the floor of Yellowstone Lake. The hot spring rim sits at lake level.

A sensor data logger recovered from the floor of Yellowstone Lake in the Deep Hole area in 2018 shows signs of melting due to unexpectedly high temperatures in sediments up to ~3 ft (1 m) away from an active hydrothermal vent. Image acquired by the Global Foundation for Ocean Exploration ROV Yogi on August 4, 2018.

Sensor (top), deformed battery/electronics package (bottom), and titanium sheath (left) following recovery from vent location A in teh Deep Hole area on the floor of Yellowstone Lake.

Sensor deployed in the Deep Hole, east of Stevenson Island to monitor long-term temperature and chemical variations in an active vent. Image acquired by the Global Foundation for Ocean Exploration ROV Yogi on August 4, 2018.

Sensor (left) and battery/electronics package (right) at vent location A in the Deep Hole area of Yellowstone Lake.  Photo was taken immediately before recovery from the lake floor. Notice the battery/electronics package slightly submerged in sediment.

Electrical Resistivity Tomography (ERT) line R3 during setup of ERT and induced polarization measurement near Rosette Spring, Lower Geyser Basin.  Photo by University of Wyoming Geophysics Team, July 17, 2018.

Spectrogram and wind data from stations on Stevenson Island for June 30, 2018. Warm colors in the spectrogram correspond to stronger seismic energy compared to cool colors. The ~1-second-period lake-generated microseism (outlined by the black box) that was generated on this day is correlated with elevated wind speeds (red circles) as a storm passed by overnight.