Venus has a global rift system stretching for thousands of kilometers. Moreover, there is now evidence of modern volcanism on Venus. Intraplate earthquakes, moonquakes, and marsquakes show that seismic activity can be associated not only with plate tectonic events, volcanism can act as a trigger, and there is no doubt that Venus is a seismically active planet. For upcoming seismic experiments on Venus [3–5] it is important to know in which areas the stresses are large enough to cause quakes.