Eagle Peak is not a
man-made site; it is a natural rocky outcrop formed through thousands of
years of geological erosion, wind shaping, and tectonic uplift. This part of
the Greater Caucasus underwent significant tectonic activity during the
Pleistocene and Holocene periods, creating steep slopes, deep valleys, and exposed
cliffs.
In the 19th–20th
centuries, Russian imperial and early Soviet explorers described this area as
“rugged terrain covered with deep forests.” The Qusar road, constructed in the
Soviet era, revealed this scenic rocky edge, which gradually became a popular
viewpoint for travelers moving between Quba and Qusar.
Today, it remains one
of the most photographed natural stops along the route.