Although Nigeria is not located within the major seismic zones of the world;over the years,several minor earthquakes have been experienced in some parts of the country.The first widely reported occurrence of an Earth tremor in Nigeria was in 1933.Other events were reported in 1939,1964,1984,1990,1994,1997,2000 and 2006.The intensities of these events ranged from III to VI based on the Modified Mercalli Intensity Scale.Of these events,only the 1984,1990,1994 and 2000 events were instrumentally recorded.They had body wave magnitudes ranging from 4.3 to 4.5,local magnitudes between 3.7 and 4.2,and surface wave magnitudes of 3.7 to 3.9.When these events occurred,there were no functional seismological observatories in Nigeria.However,that has now changed with the establishment of a seismographic network managed by the Centre for Geodesy and Geodynamics(CGG),Toro,Nigeria.Presently,the network has four operational stations equipped with 24-bit 4-channel recorders and broadband 30-second seismometers.Efforts are being made to establish more stations and migrate to real-time collection of seismic data using the general packet radio service(GPRS) technology as well as automatic location of events.Remote sensing,geological and geophysical studies have revealed the presence of a NNE-SSW trending Ifewara-Zungeru fault zone which has been shown to be linked with the Atlantic fracture system.The dynamics of the Atlantic fracture zones have been suggested to be responsible for the seismic activities experienced in the areas. Over the years, several minor earthquakes have been experienced in some parts of the country the first broad reported occurrence of an Earth tremor in Nigeria was in 1933.Other events were reported in 1939, 1964, 1984, 1990, 1994, 1997, 2000 and 2006. The intensities of these events ranged from III to VI based on the Modified Mercalli Intensity Scale. Of these events, only the 1984, 1990, 1994 and 2000 events were instrumentally recorded. The had had body wave magnitudes ranging from 4.3 to 4.5, local magnitudes between 3.7 and 4.2, and surface wave magnitudes of 3.7 to 3.9.When these events occurred, there were no functional seismological observatories in Nigeria. Host, that has now changed with the establishment of a seismographic network managed by the Center for Geodesy and Geodynamics (CGG), Toro, Nigeria. Presentedly, the network has four operational stations equipped with 24-bit 4-channel recorders and broadband 30-second seism ometers.Efforts are being made to establish more stations and migrate to real-time collection of seismic data using the general packet radio service (GPRS) technology as well as automatic location of events .Remote sensing, geological and geophysical studies have revealed the presence of a NNE-SSW trending Ifewara-Zungeru fault zone which has been shown to be linked with the Atlantic fracture system. Dynamics of the Atlantic fracture zones have been suggested to be responsible for the seismic activities experienced in the areas.