Gargano

Gargano typical coast

Gargano (Italian pronunciation: [gar'gano]) is a historical and geographical sub-region in the province of Foggia, Apulia, southeast Italy, consisting of a wide isolated mountain massif made of highland and several peaks and forming the backbone of the Gargano Promontory projecting into the Adriatic Sea, the "spur" on the Italian "boot". The high point is Monte Calvo at 1,065 m (3,494 ft). Most of the upland area, about 1,200 km2 (460 sq mi), is part of the Gargano National Park, founded in 1991. It is within the Italian Province of Foggia.

The Gargano peninsula is partly covered by the remains of an ancient forest, Foresta Umbra, the only remaining part in Italy of the ancient oak and beech forest that once covered much of Central Europe as well as the Apennine deciduous montane forest biome. The Latin poet Horace spoke of the oaks of Garganus in Ode II, ix.

Tourism

The coast around Mattinata

The coast of Gargano houses numerous beaches and tourist facilities, including resorts such as Vieste, Peschici and Mattinata. The two major salt lakes of Lesina and Varano are located in the northern part of the peninsula. Monte Gargano is the site of the oldest shrine in Western Europe dedicated to the archangel Michael, Monte Sant'Angelo sul Gargano.

Other tourist attractions include the cathedral, the episcopal palace, the Abbey of Santa Maria of Ripalta and the volcanic rocks dating back to the Triassic Period, known as "Black Stones", as well as the Sanctuary of San Nazario.

Annual events

Gargano Peninsula fossils

Some 12 to 4 million years ago, during the Late Miocene to Early Pliocene, a highly endemic vertebrate fauna evolved on what was then Gargano Island due to higher sea levels than today. Several of these animals were subject to island gigantism.

Monte Sant'Angelo on the slopes of Monte Gargano

The fossils are found in partially infilled paleokarst fissures across Monte Gargano. The Gargano Island fauna is known as Mikrotia fauna after an endemic rodent genus of the area. Initially named Microtia, this had to be corrected, because the genus name Microtia was already used for butterflies.

The surface features of the ancient karst developed in Mesozoic limestone. In these, sediment accumulated together with the remains of the local fauna, forming thick layers of reddish, massive or crudely stratified silty-sandy clays, known as terrae rossae ("red soils"). Through the mid-Pliocene, some of these deposits were flooded, probably due to tectonic movement of the Apulian Plate. Others were overlaid by other sediments of terrestrial or freshwater origin. In this way a buried, partially reworked paleokarst originated.

Later, as the ice ages cycle got underway, sea levels sank and the former island was continentalized. In the cool and semiarid conditions of the Early Pleistocene (some 1.8–0.8 mya) a second karstic cycle occurred, producing the neokarst which removed part of the paleokarst fill.

Fauna

The Gargano Island endemic mammals included:

Non-endemic mammals found on the island included:

Bird species occurring at Gargano included (studied by Ballmann, 1973, 1976):

See also

References

  1. ↑ "Gargano Running Week". Retrieved September 25, 2014.
  2. ↑ Pavia, M.; Meijer, H. J. M.; Rossi, M. A.; Göhlich, U. B. (2017-01-11). "The extreme insular adaptation of Garganornis ballmanni Meijer, 2014: a giant Anseriformes of the Neogene of the Mediterranean Basin". Royal Society Open Science. 4 (1): 160722. doi:10.1098/rsos.160722.

Sources


Coordinates: 41°43′59″N 15°45′00″E / 41.733°N 15.750°E / 41.733; 15.750

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