Paglia Orba
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The Paglia Orba (pronounced ) is a mountain peak in the
Monte Cinto massif The Monte Cinto massif is one of the main massifs in the island of Corsica, France, taking its name from the highest mountain in Corsica, Monte Cinto. It is the northernmost and highest of the four massifs that form the spine of the island. The ma ...
in Corsica. It rises to an altitude of , between the valleys of the Golo (in the Niolo) and the Cavicchia (in the Filosorma). Relatively isolated, this peak, notable for its characteristic tooth-shaped silhouette, dominates the Fango Valley and the west coast of the island. Straddling the municipalities of Albertacce and Manso, Paglia Orba is the second highest peak of the central chain and the Filosorma, behind Punta Minuta at .


Geography

With an altitude of , the Paglia Orba is located in the municipalities of Albertacce and Manso. It is nearly lower than
Monte Cinto Monte Cinto ( co, Monte Cintu) is the highest mountain on the island of Corsica, a region of France. Geography The elevation of the mountain is and so is its prominence, making it one of the most prominent peaks in Europe. It is the highest ...
. The Golo, the longest river in Corsica, rises at its feet. On its slopes at an altitude of the Ruisseau Orba rises in the communal forest of Albertacce, which is a monoculture of
laricio pine ''Pinus nigra'', the Austrian pine or black pine, is a moderately variable species of pine, occurring across Southern Europe from the Iberian Peninsula to the eastern Mediterranean, on the Anatolian peninsula of Turkey, Corsica and Cyprus, as wel ...
s.


Geology

Unlike the other summits of the Cinto massif, which are formed mainly of volcanic rocks, the Paglia Orba is made up of sandstone and conglomerates (puddingstone) with some boulders exceeding in size. These sedimentary rocks accumulated during the
Permian The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last ...
-
Triassic The Triassic ( ) is a geologic period and system (stratigraphy), system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Year#Abbreviations yr and ya, Mya), to the beginning of the Jurassic Period 201.36 ...
within a vast zone of volcanic collapse (a lake occupying a caldera), before being raised to altitude then largely destroyed by erosion during the tertiary era. Only a few rare vestiges of this sedimentary filling remain today, including the Paglia Orba preserved on the southwestern edge of this caldera.


Access

The normal access road to the summit is somewhere between hiking and mountaineering. From the Ciottulu a i Mori refuge, a path leads to the Col des Maures (Moorish Pass) and then up a very steep corridor on the western slope of the Paglia Orba. The route marked by cairns then overlooks a cliff to reach a first summit, separated from the true summit by a ravine called "combe des Chèvres". Other steep routes exist on the south side (vertical fractures or chimneys) but require experience in climbing. Experienced hikers and mountaineers can also complete the tour of the Paglia Orba by crossing the "Geologists' Breach", named in memory of a geologist who died there,) and the "Sphinx Breach", near a characteristic looking rock block.


Climbing

The dizzying faces and ridges of this "queen of the Corsican mountains" offer climbers a multitude of routes rated “AD” to “ED”. File:Paglia-Orba.jpg, The Paglia Orba seen from the Pont des 5 Arcades (D81) in Galéria, above the Fango valley. File:Niolu.jpg, La Paglia Orba (left) seen from the
Lac de Calacuccia Lac de Calacuccia is a reservoir in the Haute-Corse department of France formed by damming the Golo river. It provides hydroelectric power and water for irrigation in the dry season. Location The Lac de Calacuccia is formed by damming the Golo ...
. In the middle, Monte Cintu.


Notes


Sources

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