What exactly are the rock types that make up the underground laboratory of Utah FORGE? In this webinar, Dr. Clay Jones describes the geology of the site and surrounding area and the findings from core and cutting analyses of deep wells!
Muséum national d'histoire naturelle, CC BY 4.0 via Wikimedia Commons
Chrysomallon squamiferum — better known as the volcano snail, iron snail or scaly-foot snail — is a species of snail that lives in hydrothermal vents in the Indian Ocean. Hydrothermal vents are openings in the seafloor from which geothermally heated water escapes. They form in volcanically active areas like mid-ocean ridges where tectonic plates spread apart. Amazingly, these volcano snails embrace heat like few other species can, withstanding temperatures of up to 400 degrees Celsius!
Hydrothermal vents
Volcano snails are one of many deep-sea gastropods, but they are distinguished by their ability to sequester iron metal ions from water to form iron-sulfide coatings on their shells, bodies and feet. They’re the only existent creature we know of to incorporate these substances into their skeleton. Depending on the ratio of iron, sulfide, pyrite and gregite in the vent water, volcano snails can range in color from white to gold to black. I guess you could call these one-of-a-kind creatures the “ironmen” of the sea!
One of the many obstacles for hopeful settlers is the need for power and heat on these barren landscapes. Some geologists and other scientists theorize that geothermal energy may be the answer.
The team held a public Town Hall in Milford, UT to share the breakthroughs and future plans of Utah FORGE in a casual, relaxed setting.
Active from 1900 to 1904, the Waimangu geyser is the most powerful geyser in history, approximately 20 kilometers southeast of Rotorua on the northern island of New Zealand.