Integrated paleomagnetic and U-Pb geochronologic studies are critical to establishing well-dated apparent polar wander paths in the Precambrian. By collecting samples for both paleomagnetism and U-Pb geochronology at the same sampling sites and conducting rigorous paleomagnetic field tests to ensure that magnetizations are primary, it is now possible to establish the age of paleomagnetic poles with uncertainties of no more than a few million years. We have conducted such integrated studies on mafic intrusions of the southern Superior Province and adjacent portions of the Southern Province of the Canadian Shield. These studies yield paleomagnetic tiepoints with high-precision ages for use in polar wander path construction in the 2220 to 2110 Ma period. They indicate a direction of polar wander contrary to that of the most widely used paths for the Superior Province and for the Canadian Shield as a whole. Thus, current interpretations of the movement of the Superior Province and the relative location and movement of the Superior Province and other structural elements of the Canadian Shield during this period are no longer valid.