Plate motion — where it appears
Named by 5 essays across 2 fields — each of them below, with the objects they name alongside it.
The epoch is part of the coordinate
A latitude and a longitude with no date on them are incomplete, because the ground they refer to is moving at between ten and seventy millimetres a year. Australia crosses an ordinary survey tolerance in under two years and moved 1.8 metres between two versions of its own datum.
A published coordinate is a result
Re-observe a control mark perfectly, with an instrument good to twenty millimetres, and the answer disagrees with the published value by a hundred metres. Neither number is wrong. The difference measures the interval between two definitions.
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.
A grid stops fitting the ground it was laid on
A hundred-kilometre baseline across a plate boundary changes by 815 millimetres in fifty years, and the same baseline on the fastest plate in the model changes by nothing at all in the same fifty. The interval before an ordinary first-order specification is broken is six years in one place and never in the other.
Named alongside it
The objects these essays reach for when they reach for this one.
EpochRealisationDatumReference frameRigid rotationStrain rateToleranceNanostrainNational GridPrincipal strainShear strainVelocity field