Hot Topics
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
Lava Flows
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
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?
Seasickness
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The “half life” of a parent isotope is the time it takes for half of it to decay to its daughter isotopes.
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