Ages of ca. 2.43–2.44 Ga are determined for a mafic suite in the Kaapvaal craton.
Paleomagnetism yields a Virtual Geomagnetic Pole (18.9°N, 285.0°E, A95 = 14.1°, K = 43.4).
The possible primary or secondary origin of the VGP is discussed.
Results are used to complement the apparent polar wander path of Kaapvaal.
A test of the supercraton hypothesis Kaapvaal + Pilbara (Vaalbara) is performed.