For many decades the conventional wisdom has been that volcanic hotspots like Hawai,i’ are fed by plume of buoyant, upwelling material coming from deep in the mantle. The prevailing thought is that the plumes were hotter than the surrounding mantle to provide them with the necessary buoyancy to rise actively. EPSS Grad student Xiyuan Bao, Prof. Carolina Lithgow-Bertelloni together with UC colleagues Profs. Matt Jackson of U.C. Santa Barbara and Barbara Romanowicz of U.C. Berkeley have found that while some plumes (Hawaii, Iceland, Galapagos amongst them) are indeed hotter and carry signals of deep and ancient mantle domains, most are barely hot enough to rise actively. In some cases they are actually colder than the surrounding mantle. So how can such plumes rise? Are warm plumes carried by the background mantle or are there other mechanisms at play? The answer is not yet clear, but new frontiers are opened that will give us a window into the chemical and dynamical evolution of Earth’s interior.
This work is recently published in Science (Free Link), and also highlighted by Science Press Package as well as Nature.
Media Coverage:
ScienceNews: Some volcanic hot spots may have a surprisingly shallow heat source
Popular Science: Many volcanic islands have surprisingly cool origins
New Scientist: Plumes of rock that feed volcanic hotspots are surprisingly cold
New Scientist Netherlands: Volcanic hotspots turn out to be surprisingly cold
Spektrum (Scientific American German): Volcanic hotspots are surprisingly cool
Also on
Investigación y Ciencia,
German Geological Society - Geological Association e. V. (DGGV)
Scientific American Arabic Edition (Cover): Earth volcanic hotspots are surprisingly cool
Inside Science: Scientists Find Surprisingly Cool ‘Hotspots’ Under Earth’s Crust
Deutschlandfunk: Surprising results: some volcano hotspots are cool
Welt Der Physik: Cooler than expected under volcanoes
Scinexx: “Cold” hotspots are a mystery