january 2012

As North Dakota’s state geologist, Ed Murphy has spent a fair amount of time mapping the geology of the Killdeer Mountains in the western part of the state, hiking up and down buttes of the White River Group and the Arikaree Formation. In the 1980s, he and colleagues mapped large deposits of rocks bearing erionite — a zeolite mineral formed when volcanic ash is altered by water — that may have had some commercial use.

Despite worldwide efforts to curtail plastic use — to ban plastic grocery bags, to switch to reusable water bottles instead of disposable plastic bottles, and to get rid of the microplastics in cosmetics, for example — we still produce more than 260 million tons of plastic each year. Almost a third of that plastic goes into disposable, one-time-use items. Only about 1 percent of it is recycled globally, so much ends up in landfills. Worse still, some of the plastic winds up in the world’s oceans.

Supervolcanoes are one of nature’s most destructive forces, but given that there are no recorded observations of super-eruptions — the last occurred 74,000 years ago in Indonesia — scientists don’t fully understand how they work. Now a team studying the world’s fastest-inflating volcano, Bolivia’s Uturuncu, is shedding some light on how supervolcanoes become so powerful.

Ten years ago, John Eiler couldn’t convince anyone to build him his dream machine. He wanted a mass spectrometer that could measure the mass of common gases with extreme precision and sensitivity, but such a device would cost more than a million dollars and might not find a market: The companies that could make it didn’t think they would be able to sell more than just the one to Eiler, which didn’t make it worth their while. Even Eiler didn’t know exactly what problems he could solve with the device, though he had a hunch it would be useful.