Tidal recession — where it appears
Named by 2 essays across one field — each of them below, with the objects they name alongside it.
A tilt the Moon should not have
A moon's orbit precesses about a plane that sits on its planet's equator close in and on the planet's own orbit far out. A Moon born in the Earth's equator and carried outward by the tides should have followed that plane all the way to the ecliptic, because the angle it keeps to it is an adiabatic invariant. It is inclined by five degrees instead, and slow recession cannot have put them there.
A tilt built from a thousand near misses
The Moon's orbit is tilted five degrees to the ecliptic, and slow tidal recession cannot have done it. One candidate is the leftover debris of planet formation: bodies the size of the Moon, passing the young Earth–Moon pair, each giving its orbit a kick of a fifth of a degree in a random direction. A random walk of a few thousand such kicks reaches five degrees — and the bodies that would supply them are the same population whose impacts left the Earth's mantle its gold.
Named alongside it
The objects these essays reach for when they reach for this one.
Angular momentumInclinationLaplace planeAdiabatic invariantGiant impactGravitational focusingImpulse approximationNodal precessionOblatenessObliquityRandom walk