Outcrops of the
Permian period (Severodvinian stage), composed by
limestones,
conglomerates,
sandstones,
siltstones,
marls and
dolomites, are located to the southwest of the village, on the right bank of the Belaya River.
Fossils of the
ostracod genera
Paleodarwinula and
Suchonellina were found in the siltstones of these deposits. == References ==