Measure plate motion in a shared frame
Subtract two velocity vectors and interpret the relative motion across a local boundary.
Learning outcome: Calculate relative velocity component by component and distinguish speed from signed motion.
Starting recap
A velocity has direction as well as size. East and north components describe perpendicular parts of a local motion; negative means west or south.
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Try
A moves (2 east, 1 north) cm/year and B moves (5 east, 5 north). B relative to A is (3 east, 4 north), with speed 5 cm/year.
Open the experimentPredict
If the same extra velocity is added to both plates, will their relative velocity change?
Experiment
Start at across 3 and along 4 cm/year. Compare across -3 with along 4, then set both components to zero. Reconstruct B minus A from the displayed shared-frame velocities.
Resolve relative plate motion
Worked teaching model · synthetic values · Synthetic local planar model of a straight north-south boundary. A is west of B; positive east motion of B relative to A is separation, and positive north motion is along the boundary. In the chosen frame A moves (2 east, 1 north) cm/year; B equals A plus the selected relative components. The 5-million-year projection holds rates, orientation and reference axes constant. It is relative displacement, not a forecast of coastlines, ocean width, boundary migration or earthquake timing. No forces, elastic locking, crust type, subduction geometry, rotations or measurement uncertainties are simulated.
Reset keeps your prediction, captures and practice history.
| Vector | East (cm/year) | North (cm/year) | Magnitude (cm/year) |
|---|---|---|---|
| A in chosen frame | 2 | 1 | 2.236 |
| B in chosen frame | 5 | 5 | 7.071 |
| B relative to A | 3 | 4 | 5.000 |
| Time and assumption | East component | North component | Magnitude |
|---|---|---|---|
| 10 years, unchanged relative velocity | 30 cm | 40 cm | 50.000 cm |
| 5 million years, unchanged relative velocity | 150 km | 200 km | 250.000 km |
Across-boundary motion determines separation or convergence in this local geometry; along-boundary motion adds sliding. These components do not identify crust type, the downgoing plate, fault locking or the time of an earthquake.
Oblique divergent local motion; relative speed 5.000 cm/year.
B − A = (3 east, 4 north) cm/year. Over 5 million years at unchanged rates: (150 east, 200 north) km relative displacement. Negative components point west or south; a magnitude alone cannot classify the boundary.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
Understand
Apply
Public practice checks a specific claim. It does not establish independent mastery.
Show the subtraction, explain why the magnitude is not the sum of the components, and distinguish zero relative motion from zero motion in the shared frame.
Continue
Completion requires a saved prediction, at least one capture and a reflection. Presence checks do not grade your reasoning.
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