NASA’s plasma rocket making progress toward a 100-hour firing

Enlarge / With 200 kW of solar power, the VASIMR engine could be used as a lunar tug. (credit: Ad Astra Rocket Company) Almost everyone recognizes that if humans are truly to go deeper into the Solar System, we need faster and more efficient propulsion systems than conventional chemical rockets. Rocket engines powered by chemical propellants are great for breaking the chains of Earth’s gravity, but they consume way too much fuel when used in space and don’t offer optimal control of a spacecraft’s thrust. NASA recognizes this, too. So in 2015, the space agency awarded three different contracts for development of advanced propulsion systems. Of these, perhaps the most intriguing is a plasma-based rocket—which runs on Argon fuel, generates a plasma, excites it, and then pushes it out a nozzle at high speed. This solution has the potential to shorten the travel time between Earth and Mars to weeks, rather than months. But to realize that potential, Houston-based Ad Astra Rocket Company must first demonstrate that its plasma rocket, VASIMR, can fire continuously for a long period of time. The three year, $9 million contract from NASA required the company to fire its plasma rocket for 100 hours, at a power level of 100 kilowatts, by 2018. Read 5 remaining paragraphs | Comments

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NASA’s plasma rocket making progress toward a 100-hour firing

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

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Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

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Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

Read More:
Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

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Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

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Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

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Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

Read More:
Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

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Watching two waves of hot lava in the Solar System’s largest volcano

Watching two waves of hot lava in the Solar System’s largest volcano

Enlarge / Loki Patera, in the lower-center, has a central island that divides two waves of molten material. (credit: NASA/JPL/USGS ) Volcanic activity appears to be a common feature in our Solar System; we have evidence of it on three planets and two moons and hints of it elsewhere. But that doesn’t mean all volcanic activity is the same. Venus’ activity is driven by a simple version of plate tectonics. On the Moon, massive lava flows were released by large impacts, and Mars just seems to have vented heat left over from its formation. There are also hints of cryovolcanoes, which belch up ice rather than lava, on some of the bodies of the outer Solar System. But when it comes to sheer volume of activity, all of this takes a back seat to Jupiter’s moon Io. Io is partially molten due to gravitational stress from its proximity to three large moons and a massive planet. The results are active volcanoes and vast pools of molten material on the Moon’s surface. And we just got a good look inside the biggest of them. Slicing up Loki Loki Patera is the most powerful active volcano in the Solar System. It’s an enormous crater with a central island; around that island is a sea of hot material that covers more than 20,000 square kilometers. By all appearances, that hot material isn’t stable, since the entire surface seems to be reworked every few years, temporarily replaced by new hot material. Read 10 remaining paragraphs | Comments

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Watching two waves of hot lava in the Solar System’s largest volcano