D. P. Savelyev1,2, O. L. Savelyeva1,2, O. V. Kuvikas2

1 Institute of Volcanology and Seismology FED RAS, 683006, Petropavlovsk-Kamchatsky, e-mail: savelyev@kscnet.ru
2 Kamchatka State University by Vitus Bering, 683032, Petropavlovsk-Kamchatsky, Pogranichnaya street, 4

The detailed description of the ophiolite-clastic breccias is presented in this paper. These rocks were found in the alluvium of the brooks which erode of the tectonic zones in the south part of the Kamchatsky Mys Peninsula. The edaphogenic sediment breccias consist of the serpentinite debris cemented pink limestone with the remains of foraminifers. We discuss a genetical.