A network of seismograph stations was established by the National Center for Earthquake Research (NCER) to study in detail the earthquakes along the San Andreas fault system in central California (Eaton, Lee, and Pakiser, 1970). This report, in the form of a catalog, summarizes the results of routine earthquake locations from that network for the year 1971, and provides the basic data for further studies to be published elsewhere. Similar catalogs for 1969 and 1970 have been prepared by Lee, Roller, Bauer, and Johnson, (1972), and Lee, Roller, Meagher, and Bennett, (1972).

We located a total of 2,429 events that occurred in 1971 from primarily 34,111 first P-wave arrival times recorded at 121 seismograph stations. Among these events, 339 were blasts (mostly in quarries), 8 were suspected blasts, and 41 were either too far away from available stations or too small in magnitude to be adequately located. The remaining 2,041 events which were identified as earthquakes are presented in the catalog. The 121 seismograph stations consisted of 93 telemetered stations operated by NCER, and 28 stations operated by several other organizations. Readings from the latter stations were obtained through the courtesy of the Seismographic Stations, University of California, Berkeley, the Earthquake Mechanism Laboratory, National Oceanic and Atmospheric Administration, San Francisco, and the California Department of Water Resources, Sacramento.

Data on local earthquakes in northern California, Nevada, and Oregon have been published in the Bulletins of the Seismographic Stations of the University of California, Berkeley (UCB) for many decades. The present catalog covers earthquakes which occurred in a smaller area but in greater detail than those covered by the UCB Bulletins. For example, the UCB Bulletins for 1971 (Cloud and Qamar, 1972; Cloud, Tomblin, and Litehiser, 1972) list a total of 116 earthquakes (most with magnitude greater than 2.5) in the region covered by this report (a coastal strip from Santa Rosa to Parkfield). In addition, we attempted to use all available data in locating earthquakes within and near our seismic network.