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The sharp images of Prometheus released today come from two of Galileo's onboard instruments -- the camera, and the near- infrared mapping spectrometer which observes in wavelengths not visible to the naked eye. The images were taken during the close flyby of Io by Galileo on October 10, 1999, and are part of a large batch of data currently being transmitted to Earth.
Prometheus is the "Old Faithful" of Io's many volcanoes. It has been active during every observation over the past 20 years by NASA's Voyager and Galileo spacecraft and the Hubble Space Telescope. The new spectrometer images show two distinct hot spots at Prometheus -- a large one to the west and a fainter, cooler one to the east. The images reveal numerous lava flows near the western hot spot and enable scientists to identify a crater, or caldera, 28 kilometers (17 miles) long and 14 kilometers (9 miles) wide near the hot spot to the east.
Left:
The active volcano Prometheus on Jupiter's moon Io was imaged by the near-infrared mapping spectrometer
instrument onboard NASA's Galileo spacecraft during the close flyby of Io on October 10, 1999.
The spectrometer can detect active volcanoes on Io by measuring their heat in the near-infrared wavelengths (just
beyond the red end of human vision). It can also obtain information on the composition of materials on Iošs surface
using the same wavelengths.
The image on the left, taken at an infrared wavelength, shows the different compositions of materials on the volcano.
The dark material is thought to be silicate lava, and the white material is sulfur dioxide frost.
The image on the right was taken at a longer infrared wavelength that shows heat coming out of the volcano. The
hottest areas appear white and the coolest appear black.
[more information]
Previously, it was thought that the 50 to 100 kilometer- (30 to 60 mile-) tall plume observed at Prometheus formed where the lava erupts onto the surface. Now, however, it now appears that the plume forms at the far end of the lava flows. The caldera and eastern hot spot are thought to be associated with the vent where the molten rock rises to the surface. It appears that after the lava reaches the surface, it is transported westward through lava tubes for about 100 kilometers (60 miles) before breaking out onto the surface again. Here, numerous lava flows wander across a plain covered with sulfur dioxide-rich snow. The plume is created by the interaction of the hot lava with the snow.
Another Io flyby, this time at an altitude of 300 kilometers (186 miles), is planned for November 25 at 8:40 p.m. Pacific Time (11:40 p.m. Eastern Time). (Times given are in Earth-received time -- or the time when the signal of the event is received on Earth.) The Io flybys are challenging and risky, because Io lies in an area of intense radiation from Jupiter's radiation belts, and that radiation can harm spacecraft components. Because of the risk, the flybys were scheduled for the final portion of Galileo's extended mission. Additional information about the Galileo mission is available
on the Galileo home page at a new web address of http://galileo.jpl.nasa.gov.
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