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@TeamIndus

New world thinking for tomorrow's challenges. TeamIndus is landing on the Moon in 2017. Follow our journey.

Bangalore, India
Joined January 2011

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  1. Retweeted
    6 hours ago

    Team Space4Life it is! The Italian teams radiation experiment is the winner! & they are the youngest!

  2. 7 hours ago

    15mins before the final announcement ! Nails being bitten, coffee being gulped, anxious laughter and some non so anxious smiles

  3. Final day of presentations. Teams talking about future plans. What would happen if they win & what's happens if they don't.

  4. Retweeted
    10 hours ago
  5. That's all from me today. As ever, do send in idea suggestions for to ! Tata!

  6. Wiki, of course, has a great list that you can sort by base to peak height, with lots of images.

  7. In fact, Earth mountains rank much behind in height than mountains not just on asteroids & Mars, but also moons of Jupiter, Saturn, Neptune!

  8. Yep, lots of right guesses! Mauna Kea at Hawaii. It's mostly underwater with base to peak height >10km, while Everest base to peak is <5km.

  9. Here's another question: what's the tallest mountain/peak from base to peak on earth? (hint: Everest is tallest from sea level only)?

  10. Impact that formed Rheasilvia 1 bn yrs ago dislodged so many particles into space, the most common source of meteorites on Earth is Vesta.

  11. Then from edge of crater, all the liquid sloshed back in, meeting at the middle & rising up. Solidified in the process; formed the mountain.

  12. surface of the asteroid. This liquid bounced out of the crater, just like what happens when you drop a large stone into a puddle of water.

  13. It's formation is interesting to say the least: during the impact that created the crater, the impact heat and pressure liquified the

  14. It's simply called the Rheasilvia crater peak, and has been the tallest mountain in our solar system since 2011.

  15. In one of these craters, called the Rheasilvia crater, rises a central mountain peak that is taller than Olympus Mons, by just 100 m.

  16. Vesta's shape was distorted because of two HUGE impacts when it was still not fully solid, both craters visible clearly in its southern hemi

  17. hydrostatic equilibrium, ie, near-spherical shape bound by its own gravity. Vesta is obloid.

  18. iron and nickel, a mantle, and a distinct crust that's made of different material. But it never became a dwarf planet bcz it didn't achieve

  19. That means that it started becoming a [dwarf] planet, but stopped. It has a differentiated core; ie core that's made of heavy elements like

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