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TeamIndus Retweeted
Team Space4Life it is! The Italian teams radiation experiment is the winner! & they are the youngest!
#Lab2Moon@TeamIndus@SheerPriyapic.twitter.com/nHSOOhnqLR -
15mins before the final announcement ! Nails being bitten, coffee being gulped, anxious laughter and some non so anxious smiles
#Lab2Moon -
Final day of presentations. Teams talking about future plans. What would happen if they win & what's happens if they don't.pic.twitter.com/vz45W8m4EE
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TeamIndus Retweeted
Having fun
@TeamIndus Headquarters -- judging the Lab2Moon contest, the display of talent is awesome...http://timesofindia.indiatimes.com/companies/team-indus-moon-competition-attracts-global-youth-interest/articleshow/57641950.cms … -
That's all from me today. As ever, do send in idea suggestions for
#SpaceGrains to@sandygrains! Tata!pic.twitter.com/r5GAjBgB8B -
Wiki, of course, has a great list that you can sort by base to peak height, with lots of images. https://en.wikipedia.org/wiki/List_of_tallest_mountains_in_the_Solar_System …
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In fact, Earth mountains rank much behind in height than mountains not just on asteroids & Mars, but also moons of Jupiter, Saturn, Neptune!
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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.pic.twitter.com/OmSA5WTf9E
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Here's another question: what's the tallest mountain/peak from base to peak on earth? (hint: Everest is tallest from sea level only)?
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Impact that formed Rheasilvia 1 bn yrs ago dislodged so many particles into space, the most common source of meteorites on Earth is Vesta.pic.twitter.com/ITyFcaTMFs
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Then from edge of crater, all the liquid sloshed back in, meeting at the middle & rising up. Solidified in the process; formed the mountain.
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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.
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It's formation is interesting to say the least: during the impact that created the crater, the impact heat and pressure liquified the
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It's simply called the Rheasilvia crater peak, and has been the tallest mountain in our solar system since 2011.
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In one of these craters, called the Rheasilvia crater, rises a central mountain peak that is taller than Olympus Mons, by just 100 m.pic.twitter.com/6C1oh3lnJo
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Vesta's shape was distorted because of two HUGE impacts when it was still not fully solid, both craters visible clearly in its southern hemipic.twitter.com/oyzbuo2vlH
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hydrostatic equilibrium, ie, near-spherical shape bound by its own gravity. Vesta is obloid.pic.twitter.com/oIPuutPhC4
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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
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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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