Cohesion — where it appears
Named by 2 essays across one field — each of them below, with the objects they name alongside it.
Also named here as porosity — the same set of essays touches all of them, so they are one junction rather than several.
A wall with no size in it
Spin a body held together by nothing but its own gravity, and past a certain rate it comes apart. The rate depends on density alone — 2.3 hours for the stuff asteroids are made of — and the observed population respects the limit exactly, for every body larger than a couple of hundred metres.
A spin barrier with a corner in it
A rubble pile cannot spin faster than a period set by its density alone — 2.3 hours for most asteroids — at any size. Give it a cohesion of a few tens of pascals, weaker than any rock, and the barrier bends into a slope below a corner at a few hundred metres. The thermal torque that drives bodies to the barrier doubles their spin in a time that grows as the square of their size, so the bodies it pushes hardest are the ones that can go past.
Named alongside it
The objects these essays reach for when they reach for this one.
Bulk densityPorosityRubble pileSpin barrierYORP effectAngular momentumAsteroid familyAsteroid spinCritical spin periodNear-earth asteroidRegolithRoche limit