Image Archive

Janet Hershey, Tyee Middle School teachers, gets to experience the pilots view inside the deep diving submersible Alvin onboard the R/V Atlantis during the VISIONS'19 program.

Tyee Middle School teacher, Janel Hershey, gets a tour inside Alvin during the VISIONS19 program.

Author Susan Casey, climbs into the sphere of the deep diving submersible Alvin onboard the R/V Atlantis. Credit: J. Hershey.

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Supplies of a Stowaway

The underwater robotic remotely operated vehicle caught 'dabbing' by the Cabled Array camera on top of Axial Seamount, nearly a mile beneath the oceans' surface. Credit: University of Washington, V19.

In the pilot seat on DSV ALVIN. Credit: J. Nelson, University of Washington:V19

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The cabled digital still camera lights up the Tiny Towers vent site, covered in blue ciliates, worms and bacterial mats. Credit: UW/NSF-OOI/WHOI; V19.

An ~ 4+ft-long rat tail hangs out at the summit of Axial Seamount in the International District Hydrothermal Field. Credit:UW/NSF-OOI/WHOI;V19.

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A nearly 5 ft-long rattail eyes the ROV Jason at >5000 ft down at the summit of Axial Seamount. This solitary fish, or its friend, comes to see us each year. Credit: UW/NSF-OOI/WHOI; V19.

A nearly 5 ft-long rattail rests just above a lava flow on the summit of Axial Seamount, nearly a mile beneath the oceans' surface. White bacterial mats fill small cracks in the seafloor. Credit: UW/NSF-OOI/WHOI;V19.

A newly formed very active venting 'John Casey'site hosts beautiful healthy tubeworms with bright red plumes. A small black beehive chimney releases hot fluids into the near freezing seawater. Credit: UW/NSF-OOI/WHOI; V19.

Red-headed tubeworms thrive in the warm waters seeping out of the El Guapo chimney at the newly formed John Casey site. Credit: UW/NSF-OOI/WHOI; V19.

A fragile sulfide (beehive) structure sprouts in the John Casey area on the massive ~ 55ft tall El Guapo Edifice. Sulfide worms colonize the side of the actively venting chimlet. Credit: UW/NSF-OOI/NSF: V19.

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Extinct chimney deposits from stalagmite-like structures on the summit of Axial Seamount in the International District Hydrothermal Field; Credit: UW/NSF/WHOI; V19.

A nearly 1 m-tall, 1 day-old chimney springs from a venting orifice where a temperature-chlorinity probe is inserted sending real-time data to shore. Credit: UW/NSF-OOI/WHOI;V19.

The Diva vent site is hosted atop a narrow volcanic ridge in the International District Hydrothermal Field. A cabled sensor sends real-time data back to shore measuring pH-H2S- and temperature. Credit: UW/NSF-OOI/WHOI; V19.

A small anhydrite-rich deposit encrusts the pH-H2S-temperature sensor at the DIva vent site after 1-day since its installation. UW/NSF-OOI/WHOI; V19.

A 1-day old deposit of fine-grained sulfide and and anhydrite (CaSO4) encrusts the pH-H2S-Temperature sensor at Dive, sending data live from 300 miles off shore. Credit: UW/NSF-OOI/WHOI. V19.

>300°C vent fluids form flame-like structures at the summit of the ~ 55 ft tall hot spring deposit "El Guapo". Credit: UW/NSF-OOI/WHOI; V19.

Streams of super heated hydrothermal fluids issue from the summit of the hot spring deposit "El Guapo". Sulfide worms colonize warm parts of the outer walls, supported by nutrients in the fluids. Credit: UW/NSF-OOI/WHOI; V19.

Filamentous bacteria wave in the "breeze" on the side of Escargot. Credit: UW/NSF-OOI/WHOI; V18.