Depth distribution in Lake Ladoga reflects the geological structure of
the lake basin. Bottom relief determines the distribution of bottom s
ediments, benthic organisms, horizontal temperature distribution and o
ther characteristics and effects general current pattern in different
seasons of the year. In this paper new values of mean depth, volume an
d area of Lake Ladoga and its parts are presented, and also the length
and fractal dimension of the shoreline are determined. Based on the a
nalysis of relative volume curves, the integrity of morphogenesis of t
he northern and the southern parts of Lake Ladoga despite their quite
different bottom topography was established.