Using data from temporary networks of portable seismolgraphy in southern Peru, we located 888 shallow and intermediate depth events near a proposed discontinuity in the seismic zone there. These events reveal a prominent contortion, instead of a discontinuity, that trends approximately N80¿E, parallel to the direction of relative plate motion. North of about 15¿S, the seismic zone beneath Peru is nearly horizontal, but south of about 15.5¿S, it dips at about 25¿. Volcanoes lie above the more steeply dipping some where earthquakes occur between 120 and 140 km, and the volcanic line in southern Peru stops abruptly at the contortion.