A type of slow earthquake known as a slow-slip occurred after a March 9, 2011, magnitude-7.3 foreshock to the 2011 Great East Japan Earthquake, and was thought to have been related to that magnitude-9 megaquake two days later. Along the Nankai Trough, a slow earthquake will occur in the region where the boundary between the continental and the Philippine Sea plates are not firmly attached. According to assistant professor of seismology Yusuke Yamashita at Kyoto University's Disaster Prevention Research Institute Miyazaki Observatory, slow quake activity has been detected at a shallow location on the boundary of the plates since Aug. 8 and is currently picking up. The slow earthquake activity detected by Yamashita has included two types of weak shaking: low wavelength micromotion, with cycles of every 0.1 to 0.5 seconds, and ultra-low frequency earthquake every 10 to 20 seconds. To determine the exact location of the activity will require the installation of seismometers on the sea floor, but it is believed to be occurring in a roughly 100-kilometer radius area on the ocean floor at least 50 kilometers southeast of the Miyazaki Prefecture coast.