Results of Cs-137 and Co-60 measurements in the bottom sediments in th
e north-west part of the Black Sea show the distribution unhomogeneity
of radionuclides concentration in the measurement area and in vertica
l cores. Intermittency of layers with different radionuclides concentr
ation in cores reflects the active horizontal movement of sediments at
the shelf edge and continental slope. As a result of such phenomenon
the sediment with age 7 years (according to the Chernobyl mark) were f
ound at the 5-7 cm from the surface of the bottom sediments. Maximum C
s-137 concentration (42 mBq/g) was found at the shelf edge in the surf
ace layer of sediments. Maximum Co-60 concentration (1320 mBq/g) was c
aused by a hot particle. There was no correlation between Cs-137 and C
o-60 distribution.