The Regional Earthquake Likelihood Models (RELM) test of earthquake forecasts in California was the first competitive evaluation of forecasts of future earthquake occurrence. Participants submitted expected probabilities of occurrence of M ≥ 4.95 earthquakes in 0.1°× 0.1°cells for the period 1 January 1, 2006, to December 31, 2010. Probabilities were submitted for 7,682 cells in California and adjacent regions. During this period, 31 M ≥ 4.95 earthquakes occurred in the test region. These earthquakes occurred in 22 test cells. This seismic activity was dominated by earthquakes associated with the M ¼ 7.2, April 4, 2010, El MayorCucapah earthquake in northern Mexico. This earthquake occurred in the test region, and 16 of the other 30 earthquakes in the test region could be associated with it. Nine complete forecasts were submitted by six participants. In this paper, we present the forecasts in a way that allows the reader to evaluate which forecast is the most "successful" in terms of the locations of future earthquakes. We conclude that the RELM test was a success and suggest ways in which the results can be used to improve future forecasts.earthquake forecasting | forecast verification | earthquake clustering R eliable short-term earthquake prediction does not appear to be possible at this time. This was confirmed by the failure to observe any precursory phenomena prior to the 2004 Parkfield earthquake (1). However, earthquakes do not occur randomly in space and time. Large earthquakes occur preferentially in regions where small earthquakes occur. Earthquakes on active faults occur quasiperiodically in time.Earthquakes obey several scaling laws. One example is Gutenberg-Richter frequency-magnitude scaling (2). The cumulative number of earthquakes, N c , with magnitudes greater than M in a region over a specified period of time is well approximated by the relationwhere b is a near universal constant in the range 0.8 < b < 1.1 and a is a measure of the level of seismicity. Small earthquakes can be used to determine a, and Eq. 1 can be used to forecast the probability of occurrence of larger earthquakes. An alternative approach to quantifying earthquake hazard is to specify the recurrence statistics of earthquakes on mapped faults. Geodetic observations can be used to determine rates of strain accumulation, and paleoseismic studies can be used to determine the occurrence of past earthquakes. A problem with this approach is that many damaging earthquakes do not occur on mapped faults.A pattern informatics (PI) approach to earthquake forecasting has been proposed (3-5). In forecasting M ≥ 5 earthquakes, a region is divided into a grid of 0.1°× 0.1°subregions. The rates of seismicity in the subregions are studied to quantify anomalous behavior. Precursory changes that include either increases or decreases in seismicity are identified during a prescribed time interval. If changes exceed a prescribed threshold, hot spots are defined. The forecast is that future M ≥ 5 earthquakes will occur in the hot-spot regions in a ...