The most interesting (Hutchinson, 1957), and at the same time oldest graben
lakes of Europe, are Lakes Ohrid and Prespa. According to geologists and g
eographers, both originated during the Pliocene. They show karstic features
and differ by volume, much less by area.
At the occasion of an excursion to Lake Prespa in September 1994, an absenc
e of oxygen in the hypolimnion between 17 m and the maximum lake depth, 48
m, was observed, for the first time since Stankovic' (1926) record. Moreove
r, a continuous decrease in lake level since the 1960s, the lowest transpar
ency ever recorded from Megali Prespa, and high nutrient values, though onl
y observed during a short part of the late stagnation period, are alarming
signals, all suggesting eutrophication.