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Information concerning a total number of 13700 instrumentally recorded earthquakes is used to study the geographical and the vertical distribution of the Earth's seismicity. From these earthquakes, which form four complete samples of data (M ≥ 7.0, 1894–1992; M ≥ 6.5, 1930–1992; M ≥ 6.0, 1953–1992; M ≥ 5.5, 1966–1992), 11511 are shallow (h ≤ 60 km), 2085 are of intermediate focal depth (61 ≤ h ≤ 300 km) and 564 are deep focus earthquakes (301 ≤ h ≤ 720 km). The parameters a and b of the frequency-magnitude relationship were calculated in a grid of equally spaced points at 1° by using the data of earthquakes located inside circles centered at each point. The radius of the circles increased from 30 km with a step of 10 km until the information for the earthquakes located inside the circle fulfil three criteria which concern the size of the sample used to compute these parameters at each point of the grid. The results are given in a qualitative way (epicenter maps) as well as in a quantitative way (mean return periods).