Principal strain — where it appears
Named by 2 essays across one field — each of them below, with the objects they name alongside it.
The ground has an indicatrix too
Two hundred and forty-six essays hold the Earth still while the page is measured. The ground is moving at tens of millimetres a year, and the motion is a map with four partial derivatives — so the same construction that draws Tissot's ellipse draws one for the ground, and the fastest plate in the model returns exactly nothing.
A velocity needs a frame and a strain rate does not
One place on a plate boundary moves at 5.3, 7.0, 10.2 or 54.6 millimetres a year, and towards the south-east or the north-west, depending on which rotation was subtracted first. Every one of those readings reports the same strain rate, to two parts in a hundred thousand million.
Named alongside it
The objects these essays reach for when they reach for this one.
Plate motionRigid rotationShear strainStrain rateVelocity fieldAngular deformationDeformation gradientDilatationEpochEuler poleInvariantJacobian