In this study, we propose an analysis of the earthquake clusters that occurred in North-Eastern Italy and western Slovenia from 1977 to today. Given a mainshock generating alarm in the population, we are interested in forecasting if a similar magnitude earthquake will follow. We classify the earthquake clusters associated with mainshocks of magnitude Mm into two classes: if the strongest aftershock has a magnitude ≥Mm-1 (swarms or large aftershock seismic sequences) as type A, otherwise (smaller aftershocks seismic sequences) as type B. A large aftershock following a main shock can cause significant damages to already weakened buildings and infrastructures, so a timely advisory information to the civil protection is of great interest for effective decision-making. For the first time, we applied to a new catalogue a pattern recognition algorithm for cluster type forecasting that we developed for all Italy (Gentili and Di Giovambattista, 2017). Thanks to the lower completeness magnitude of the local OGS catalogue, compared to the national one, and to a new version of the algorithm, we were able to lower the threshold of the clusters mainshocks magnitude from 4.5 to 3.7. The method has been validated by rigorous statistical tests. We tested the algorithm on the 1976 highly destructive earthquake cluster (mainshock magnitude 6.5the strongest in the last 80 years in the region) and we retrospectively forecasted it as an A cluster.Successful results were obtained also on other three smaller earthquake clusters in 2019. et al., 2016), which caused about 1000 casualties and the complete destruction of little towns and villages, a seismic network managed by OGS (National Institute of Oceanography and Experimental Geophysics) was installed. From 1977, seismicity has been recorded by the OGS network. Main events, with magnitude greater than 5, recorded by the network are: the ML=5.2 16 September 1977 Trasaghis earthquake, in the central-western part of the analysed area, corresponding to Friuli Venezia Giulia Italian region, and two more recent earthquakes respectively on 12 April 1998 (ML=5.6) and on 12 July 2004 (ML=5.1), located near the border between Italy and Slovenia. However, several clusters of lower magnitude have been detected in different parts of the analyzed region. This study is possible thanks to the OGS bulletins, available at the website www.crs.ogs.trieste.it/bollettino/RSFVG/RSFVG.en.html, an accurate local catalogue characterized by low completeness magnitude that has been compiled by the National Institute of Oceanography and Experimental Geophysics, Centre of Seismological Research, since 1977. Evenif many clusters in the region are characterized by a mainshock followed by smaller aftershocks, in some cases repeated strong earthquakes have been recorded. These earthquakes constitute a big danger from the civil protection point of view, because they imply accumulated damage on already damaged structures, increasing the probability of building collapse. The last strong earthquake in the region, the 1976...