During the
Triassic period, the
Provence subsided and was covered by the sea, leaving thick layers of various
limestone deposits. Several million years later, with the arrival of the
Jurassic period, the area was covered by a warm shallow sea, which allowed the growth of various
corals. The
Cretaceous period saw what is now
Basse Provence being raised and the sea reaching the current location of the Alps, which were themselves erected during the tertiary era. As a result of the large-scale geological activity, many of the Jurassic limestone deposits fractured, forming relief with valleys and other such features. The origins of the Verdon Gorge can be traced to this era. The dawn of the
Quaternary period had large-scale
glaciation, transforming water pockets and lakes into rivers of ice, which remodeled the topography, scouring and striating the landscape. At the end of this activity, erosion by rivers continued, forming the Gorge as it is today. The Verdon's riverbed was scoured for a second time of the accumulated coral and limestone sediments, by a water delivery rate nearing 2000 to 3000 cubic metres per second.
Discovery The gorge was described in printed form from 1782 and 1804. By the second half of the 19th century, it was featured in French tourist guides. According to
Graham Robb's book
The Discovery of France, the gorge did not become known outside France until 1906.
Recent developments On 10 July 2006, the
Council of State annulled the declaration of public use of a project by
EDF relating to a proposed high-voltage line which would have had to pass through the Verdon Gorge. This decision ended 23 years of struggle by public groups and associations of environmental defence to preserve a site of exceptional natural interest, of which a part contains protected animal and plant species. ==Geography==