Dive and Discover : Hot Topics : Lava Flows

Hydrothermal Vents

Godzilla, Sasquatch, and Homer Simpson: The Curious Names of Deep-sea Features

Bacteria at Hydrothermal Vents

Looking for Microbes

Biogeography of Hydrothermal Vents

Seafloor Geology

Seafloor Gravity

Seafloor Magnetics

What Does a Young Submarine Lava Flow Look Like?

Hotspots & Cool Volcanoes: The New England Seamounts

Extreme Creatures

Deep Sea Biology

Galápagos Animal and Marine Life

Seabird Observations in the Western Galápagos Islands

Deep-Sea Corals

The Watery World of Salps

Oceanographic Tools

Keeping the “Big O” Out of Alvin

Autonomous Hydrophone Array (AHA)

The Hydrothermal Vent Prospecting Team

Measuring Temperature At Hydrothermal Vents—Al Bradley’s Ingenuity

Finding Telltale Hydrothermal Plumes With MAPRs

The Hawaii MR1 Side-Scan Sonar Mapping System

ABE: the Autonomous Benthic Explorer

Antarctic Water Wear: Cold-Water Diving and Drysuits

History of the Earth

How Old is That Volcano?

The Galápagos Islands

Dating corals, knowing the ocean

Going vertical: Gauging ocean overturn rates

What's it like to go on a cruise?

Life at Palmer Station

Deception Island: Fire and Ice, History and Humans

To: The Paul Revere Science Club

What Is It Like To Go Down In Alvin?

Submarine pillow flows along an eruptive fissure near the crest of the East Pacific Rise at 2600 meters depth. Scale across photo is about 4 meters. Camera across the foreground is one of Alvin’s video cameras. Photo by Dan Fornari, WHOI. « Previous | Next »

Submarine pillow flows along an eruptive fissure near the crest of the East Pacific Rise at 2600 meters depth. Scale across photo is about 4 meters. Camera across the foreground is one of Alvin’s video cameras. Photo by Dan Fornari, WHOI.

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