Io, the innermost of the four moons of Jupiter discovered by Galileo Galilei in 1610 and only slightly bigger than our own moon, is the most geologically active body in our solar system.
Hundreds of volcanic areas dot its surface, which is mostly covered with sulphur and sulphur dioxide.
The largest of these volcanic features, named Loki after the Norse god often associated with fire and chaos, is a volcanic depression called patera in which the denser lava crust solidifying on top of a lava lake episodically sinks in the lake, yielding a raise in the thermal emission that has been regularly observed from Earth.
With its two mirrors, each 8.4 meters across, set on the same mount 20 feet apart, the Large Binocular Telescope, or LBT, produces images at the same level of detail that a telescope with a single, 22.8-meter mirror would achieve by combining the light through interferometry.
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Thanks to the Large Binocular Telescope Interferometer, or LBTI, an international team of researchers was able to look at Loki Patera, revealing details as never before seen from Earth.
"In this way, for the first time we can measure the brightness coming from different regions within the lake," Conrad added.
"While we have seen bright emissions - always one unresolved spot - 'pop up' at different locations in Loki Patera over the years, these exquisite images from the LBTI show for the first time in ground-based images that emissions arise simultaneously from different sites in Loki Patera," said Imke de Pater, a professor at the University of California, Berkeley.
The study was published in the Astronomical Journal.