What do they call a half horse and half man?
Centaur, Greek Kentauros, in Greek mythology, a race of creatures, part horse and part man, dwelling in the mountains of Thessaly and Arcadia.
What are centaurs space?
A centaur, in planetary astronomy, is a small Solar System body with either a perihelion or a semi-major axis between those of the outer planets.
How far is Nessus?
Does Nessus exist?
7066 Nessus is a Centaur minor planet with an irregular orbit. At perihelion, Nessus is closer to the Sun than Uranus; at aphelion, Nessus moves into the Kuiper belt, It is a place where Light is scarce….
|Population:||Vex, Fallen, Cabal|
Is Io a real planet?
Eruptive. The moon Io is the most volcanically active world in the solar system. Io even has lakes of molten silicate lava on its surface.
What is the mass of Nessus?
Can we live on Io?
Io is generally considered a poor candidate for life because of all the radiation Jupiter blasts it with. In addition, no organic molecules have been detected on its surface, and it has only an extremely thin atmosphere devoid of detectable water vapor.
Has anything landed on Io?
Pioneer 10 became the first spacecraft to reach the Jupiter system on December 3, 1973. It passed within 357,000 km (222,000 mi) of Io. During Pioneer 10’s fly-by of Io, the spacecraft performed a radio occultation experiment by transmitting an S-band signal as Io passed between it and Earth.
How long is a day on Io?
The atmosphere is collapsed and trapped as surface ice for about two hours each day on Io (note: A day on Io is equal to 1.7 Earth days, because that’s how long it takes the body to rotate on its axis in relation to the sun.
Does the moon have volcanic activity?
The Moon has been volcanically active throughout much of its history, with the first volcanic eruptions having occurred about 4.2 billion years ago. Today, the Moon has no active volcanoes even though a significant amount of magma may persist under the lunar surface.
Is there lava inside the moon?
The lava tubes beneath the moon’s surface are so large that they could, in fact, hold Padua’s entire city center, said Riccardo Pozzobon, study coauthor and planetary geologist in the department of geosciences of the University of Padua in Italy. The study published this month in the journal Earth-Science Reviews.
Why is our moon no longer experiencing volcanism?
A team of Dutch earth scientists — lead by Mirjam van Kan Parker and Wim van Westrenen from VU University Amsterdam — have now identified the likely reason for the lack of volcanic activity: the hot, molten rock contained within the Moon’s interior could be so dense that it is too heavy to rise to the surface.