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The
Gargano or
Monte Gargano is a promontory in northern of Apulia belonging to the province of Foggia which juts into the Adriatic
Sea in a nest-east direction. It is some 65 km long, 40 km wide, covers
an area of 3,015 sq. km and reaches its highest point at Monte Calvo
(1065 m). The promontory
Monte Gargano (
Monte Gargano is a mountain in
Apulia
- Italy ) is a limestone and dolomite massif surrounded
on, three sides by sea and bordered by the Candelaro and Fortore rivers
to ihe west. Low hill-land separates it from the Apennines and gives it
thai unique geographic identity which has made it a sort of biological
island and which in the past led to an isolation which profoundly
affected both the population and culture. The origins of the Gargano
promontory are linked to a cretaceous uplift dating back to theMesozoic
age (about 70 million years ago) but its present configuration was
defined in the last 10,000 years above all due to fluvial transportation
which/armed the Tavoliere to the east and south and the Sipontoni lagoon
and Capitanata marshes around the gulfo Manfredonia, while the
accumulation of sediments led to the formation of coastal bars which
transformed what were originally gulp open up to the sea into the Lesina
and Varano lagoons. A unique characteristic of the
Gargano is the
widespread karst phenomena, an erosion process where water, enriched
with carbon dioxide, is able to disaggregate and model the limestone,
creating dolinns, swallow holes, underground cavities, rock bridges and
other characteristic phenomena such as ttu, furrowed fields, grooves in
the land alternating with limestone create. The comMned action of the
karst phenomena and mechanical erosion due to the motion of the waves
has created many sea
grottos and
rock arches dotted along most of the
splendid coastline, above all between
Mattinata ,Vieste
(
Map of Vieste ),
Peschici,
Tremiti Isles
and
Rodi Garganico. Despite the
shortage of surface water and the foci that one third of the area is
arid and stony, the central-eastern, zone of the promontory is covered
by dense forest became of the abundant rainfall (1.200 mm/year).
Furthermore, in winter there is a great dm! of snow and the temperature,
while generally fairly high, may drop to 10° below zero. Most of the
towns and villages have grown along two longitudinal axes, one passing
through the higher terraces to the south (Monte Sant'Angelo,
San Giovanni Rotondo,
San Marco in Lamis), and the other to the north (Apricena,
Sannicandro Garganico). There were few settlements along the coast throughout
Medieval times because of the continuous threat of barbarian pirates,
and towns began to spring up only in modern times, especially after the
Second World War, when tourism becameoneof the main sources of income
especially for the towns Mattinata, Vieste, Peschici and Ischitella.
Apart from the Manfredonia petrochemical plants, industrial activities
are few and far between. There are only some quarries (marble at San
Marco in Lamis and bauxite at San Giovanni Rotondo) and a few small
fond- industries. The economy of the Gargano is therefore still based on
breeding, mainly in the central-western zone, and on dgrwultvrp in the
coastal plains near springs. Hystory of
the Gargano Other links:
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Hotel to Apulia:
Alberobello -
Barletta -
Bisceglie -
Carovigno -
Castellaneta -
Castro Marina - Gallipoli
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Ginosa Marina -
Giovinazzo -
Leporano Marina -
Margherita di Savoia
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Marina di Chieuti -
Mola di Bari -
Monopoli -
Nardò -
Ostuni -
Otranto -
Palese -
Polignano a Mare -
Salento -
Map of Salento -
Porto Cesareo -
Pulsano Marina - San Foca
-
Santa Cesarea Terme
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Santa Maria di Leuca -
Torre a Canne -
Torre a Mare -
Torre San Giovanni -
Trani -
Margherita di Savoia
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Santa Cesarea Terme
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Torre a Canne
Francavilla Fontana -
Latiano -
Locorotondo -
Maglie -
Martina Franca -
Mesagne - San Donaci -
San Pancrazio
Salentino -
Torre Santa Susanna
-
Bari -
Brindisi -
Foggia -
Lecce -
Taranto
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