Holy hell! OK -- do they burn up on entry? What's the criteria for that?
Holy hell! OK -- do they burn up on entry? What's the criteria for that?
It's complicated. Depends on the cross-sectional area and the materials the boulders are made of. Ice, for example, burns up (melts) on reentry much more readily than iron!
Also depends on the angle of attack. Heading straight down (perpendicular to the ground beneath it) passes through much less atmosphere than a glancing blow, so has a lot less time to burn up.
It could also be some lighter rock (a matrix) with iron clasts, created from a collision between a huge, light asteroid and smaller iron planetessimal fragments. Then if our planetary defense system breaks off a bunch of boulders, some could contain the heavy iron fragments and some might not, so different things would happen on reentry for each boulder.
Isn’t this among the easier to deflect? You literally smash other asteroids into it without much fear of it breaking up.
As for smashing “other asteroids” into it, that’s likely not feasible due to the vast distances between asteroids and the masses involved.
Momentum is a function of mass and velocity. The momentum of two similarly-massive asteroids, one rock the other metal, is the same. Given existing technologies, deflecting a solid-ish body is easier than a loose pile of gravel.
But this doesn’t take into account the masses. Asteroids vary in size from about 1 metre across to the dwarf planet Ceres, at 1000 km across. A giant asteroid is unlikely to have other giant asteroids nearby. If one giant asteroid is on a collision course with earth, what is the likelihood we’ll find a similar-enough sized one within a reasonable enough distance to be able to make them collide? Extremely remote.
https://www.nasa.gov/mission_pages/asteroids/overview/fastfa...
I'll say you're a scammer. I'm willing to sell it for half the price. Comes with a certificate demarcating the plot as well.