Italy also separates the western basin of the Mediterranean Sea from the eastern basin — that is, theTyrrhenian Sea from theIonian Sea — extending towards the west withCalabria andSicily, which together geologically form a peninsular extension. Only 140 km (87 mi) separate Sicily and Africa (theTunisian peninsula), by thechannel of Sicily.[5]
The coastal development of the Italian peninsula and islands is vast; about 8,000 kilometres (5,000 mi),[7][8] which is much larger than that of the Iberian peninsula, but much less than that of the Balkans.
Italy has a prevalence of hilly areas (41.6% of the territory) compared to mountainous areas (35.2% of the territory), or flat areas (23.2%).[9]
The Italian soil today is the result ofanthropization and is partly mountainous, partly hilly, partly volcanic, partly endolagunar with bumps, polesine, islands, dried up by reclamation (Bonifiche Circeo, Ferraresi, Comacchio, Ostiense, Pisana and so on) with ever greater raising of embankments (for example the withdrawal of 1.7 billion cubic meters per year of fresh water, from 20 consortia fromVeneto alone).
The distance that separates the Testa Gemella Occidentale from Punta Pesce Spada is 1,291 km (802 mi); the maximum distance between the eastern and western borders is about 600 km (370 mi). The municipalities at the ends of Italy are:
Although theIstituto Geografico Militare ofFlorence has repeatedly declared that it is impossible to uniquely determine the center of a non-geometric shape such as that of Italy,[11] there are several locations that, depending on the measurement criteria adopted, compete for the primacy of thegeographical centre of Italy:
Peninsular Italy refers to the entire southern part of the aforementioned line, up toPunta Melito inCalabria (which is the southernmost point of the peninsula) andSanta Maria di Leuca inApulia.San Marino and theVatican City are foreign territories, although included in the Italian geographical region.
TheItalian peninsula occupies a median position between the three main peninsulas ofsouthern Europe, emerging right in the center of theMediterranean Sea, with large islands and some archipelagos.
Insular Italy is made up ofSardinia,Sicily and numerous smaller islands, scattered or grouped intoarchipelagos in the seas that bathe the coasts of the peninsula.Corsica is not politically included in insular Italy since it belongs toFrance, however, it is included in the Italian geographical region.
The five largest islands belonging to the Italian state are, in order of size:
Archipelago of theAeolian Islands or Lipari, which includesSalina,Lipari, the largest of the group,Vulcano, a now almost extinct volcano;Panarea and thenStromboli, an eruptive cone still in activity which was calledStronghilo by theancient Greeks (hence Stromboli), due to its conical shape of an inverted top on the sea; to these must be addedFilicudi andAlicudi;
Almost 40% of the Italian territory is mountainous,[17] with theAlps as the northern boundary and theApennine Mountains forming the backbone of the peninsula and extending for 1,350 km (840 mi).[17] The Alpine mountain range is linked with the Apennines with theColle di Cadibona pass in theLigurian Alps.[18] NineteenItalian regions are crossed by either the Alps or the Apennines, or their offshoots.Sardinia has mountains with their own characteristics and are included in the Sardinian-Corsican relief, since it also affectsCorsica.
The Alps (formed during theMesozoic andCenozoic)[19] surround the Po Valley to the north, east and west, and develop along the entire northern border of Italy (about 1,000 km or 620 mi), creating a natural border. The Alps contain the highest peak in theEuropean Union,Mont Blanc, at 4,810 meters (15,780 ft)above sea level, located between theAosta Valley andFrance.
The Apennines (formed during theOligocene)[20] rise south of the Po Valley and run from north to south throughout the Italian peninsula, fromLiguria toCalabria and continue in northernSicily ending in theMadonie, acting as a watershed between the Tyrrhenian and Adriatic-Ionian coast.
The highest peaks in Italy are found in theWestern Alps, where there are numerous peaks that exceed 4,000 meters (13,000 ft) includingMonte Rosa (4,634 meters or 15,203 feet), theCervino (4,478 meters or 14,692 feet) and Mont Blanc which with its 4,810 meters (15,780 ft). The maximum height of the Apennines is theGran Sasso d'Italia (2,912 meters or 9,554 feet).
The hills cover most of the Italian territory. They are mainly located in the central-southern part of the peninsula,[21] along the sides of the Apennine ridge, but also in the pre-Alpine area, close to the Alps.[21]
The hilly reliefs, which alternate with hollows and valleys, have slight slopes and do not exceed 800 meters or 2,600 feet.
The first two hilly systems are the subalpine hills and the Preappennino, two hilly strips arranged between the Alps and the Po Valley and between the Apennines and the Adriatic coast respectively.[22] The subalpine hills widen more in the western part of the Po Valley, where they form the hills of theLanghe andMontferrat.[22] Two other hill systems are the Tyrrhenian Anti-Apennine, which extends from theColline Metallifere of Tuscany toVesuvius and the Beneventane Hills in Campania, and the Adriatic Anti-Apennine, present in Puglia with theMurge andGargano hills.[22]
The Italian hills have different origins:
The Langhe, Monferrato,Chianti and Murge are sedimentary hills[21] formed by the lifting of the seabed.
The Beneventane Hills are of tertiary formation, that is, composed of gravel stratifications or masses of pebbles mixed with limestone and sandstone, probably due to the raising of the lake bottom.
The hills ofBrianza, ofCanavese and more generally of the entire strip that runs at the foot of the Alps are morainic,[21] that is, made up of deposits of earth and crushed stone transported by ancient glaciers.
TheEuganean Hills and numerous other formations in Tuscany, Lazio, Campania are of volcanic origin,[21] i.e. they are the remains of ancient extinct volcanoes, rounded by a long erosion.
The plains make up 23.2% of the Italian national territory. In between the two lies alarge plain in the valley of thePo, the largest river in Italy, which flows 652 km (405 mi) eastward from theCottian Alps to the Adriatic. The Po Valley is the largest plain in Italy, with 46,000 km2 (18,000 sq mi), and it represents over 70% of the total plain area in the country.[17] The Po Valley is divided into two bands:[22] the high plain, which borders the Alpine and Apennine hills, and the low plain located in the center and extended up to the Po delta.
In the peninsular part and in the islands there are only small plains often located along the coasts and at the mouth of the major rivers, near which they formed:[22] this is the case, for example, of theTavoliere delle Puglie, of theCampidano in Sardinia or theMaremma in Tuscany.[22]
The second largest Italian plain is the Tavoliere delle Puglie,[23] which is a rising plain, formed from the raising of the seabed.
Other plains, for example thePlain of Campania, are of volcanic origin[23] where the ashes of the volcanoes have filled the surrounding valleys, transforming them into fertile plains.
Italy is surrounded, except to the north, by the sea, and its territory has a rich reserve of inland waters (rivers and lakes). The southern regions, however, are drier than the northern ones, due to the scarcity of rains and the absence of glaciers that can feed the rivers.
Italianrivers are shorter than those of other European regions due to the Apennines that run along the entire length of the peninsula, dividing the waters into two opposite sides. They are numerous however, due to the relative abundance of rains in Italy in general, and to the presence of the Alpine chain, rich in snowfields and glaciers, in northern Italy.
The fundamentalwatershed follows the ridge of the Alps and the Apennines and defines five main slopes, corresponding to the seas into which the rivers flow: the Adriatic, Ionic, Tyrrhenian, Ligurian and Mediterranean sides.[24] Italian rivers are categorized into two main groups: the Alpine-Po river rivers and the Apennine-island rivers.[24]
The longest Italian river is thePo (652 km or 405 mi), which flows from theMonviso, runs through the entirePo Valley from west to east, and then flows, with adelta, into theAdriatic Sea. In addition to being the longest, it is also the river with the largest basin and the largest flow at its mouth. The second longest Italian river is theAdige (410 km or 250 mi), which originates nearLake Resia and flows into the Adriatic Sea, after having made a north–south route, nearChioggia. The third longest river in Italy is theTiber (405 km or 252 mi), the second longest Italian river in terms of hydrographic basin; it was formed onMonte Fumaiolo (inEmilia-Romagna) and flows into theTyrrhenian Sea after having crossed the center ofRome. After the Tiber, in order of length are the riversAdda (313 km or 194 mi),Oglio (280 km or 170 mi),Tanaro (276 km or 171 mi) andTicino (248 km (154 mi), of which 157 km (98 mi) is in Italy).
In Italy there are more than 1,000 lakes, mostly artificially created by the damming of river valleys.[25]
In the north of the country are a number of subalpinemoraine-dammed lakes (theItalian Lakes), including the largest in Italy, theGarda (370 km2 or 143 sq mi).[26] Other well known of these subalpine lakes areLake Maggiore (212.5 km2 or 82 sq mi), whose most northerly section is part of Switzerland,Como (which holds the record of depth in the Italian Republic, which amounts to 410 m or 1,350 ft)[27] (146 km2 or 56 sq mi),Orta,Lugano,Iseo,Idro. These lakes occupy wide valleys carved by ancient glaciers.
In Italy there are also coastal lakes, such asLake Lesina, separated from the sea by a narrow strip of land, and volcanic lakes (Lake Bolsena,Lake Vico,Lake Bracciano), which occupy the craters of extinct volcanoes.Lake Trasimeno, on the other hand, formed in a hollow in the territory.[26] Other notable lakes in the Italian peninsula areVarano andOmodeo inSardinia.
The swamps and ponds that in the past covered vast flat areas of Italy, in recent centuries have been largely dried up;[26] the few remaining wetlands, such as theValli di Comacchio in Emilia-Romagna or theStagno di Cagliari in Sardinia, are protected as very precious natural environments.[26]
Along the Italian coasts there are lagoons, among which theVenetian Lagoon, that ofGrado Lagoon and that ofMarano Lagoon in the northern Adriatic stand out for their size and importance, and theOrbetello Lagoon on the Tuscan coast.
View of theStrait of MessinaPopulation density (left) and elevation above sea level (right) inVeneto (2010). Veneto is particularly vulnerable to risingsea level.
The Italian peninsula overlooks theMediterranean Sea, which around it is divided into various seas.[26]
TheLigurian Sea bathes the coasts ofLiguria and, according to the cartography of the Hydrographic Institute of the Navy, the northern Tuscan coasts to the south as far as the island ofElba.
TheTyrrhenian Sea bathes the western coasts of the peninsula south of the island of Elba (and therefore all the regions fromTuscany toCalabria), the northern coasts ofSicily and the eastern coasts ofSardinia.
Italy has a coastline of approximately 7,900 km (4,900 mi),[29][30] with a great variety of shapes that depends both on the nature of the mainland and on the action of the sea.
The Adriatic coasts are quite straight, characterized to the north by the gulfs ofTrieste andVenice, in the center by theConero promontory, to the south by that of theGargano, which forms theGulf of Manfredonia. The Adriatic coasts are low and sandy,[26] with lagoons in the northern section. Only in the Trieste area, in correspondence with the Gargano, the Conero and the lower easternSalento (betweenOtranto andSanta Maria di Leuca) do rocky sections follow one another.
The Ionian coasts are mainly low and sandy and are characterized by the wideGulf of Taranto, closed to the east by the Salento Peninsula (which divides it from the Adriatic) and to the west by the Calabrian peninsula (which divides it from the Tyrrhenian Sea).
The Tyrrhenian coasts are very articulated, with rocky stretches alternating with sandy beaches, with numerous gulfs and headlands. Among the many gulfs includeNaples,Salerno andGaeta, between the peninsulas that ofSorrento and the promontories that ofCirceo and that ofPiombino. In the Tyrrhenian Sea, there are three important channels: between the island of Elba and the Tuscan coast theStrait of Piombino, between Elba and Corsica theStrait of Corsica,[26] and between Sardinia and Corsica theStrait of Bonifacio.
The underground thrusts that millions of years ago gave rise to the reliefs of Italy still continue: the earthquakes and the eruptive activity of volcanoes testify to this.
Squeezed between twoplates, theAfrican Plate and theEurasian Plate, Italy is very subject to earthquakes, even intense ones, so much so that it holds the record inEurope.[31] In particular, the areas at greatest seismic risk are the north and south-west ofSicily, the wholeApennines (but in particular the central-southern area), northernApulia, almost all ofFriuli-Venezia Giulia and finally the north-west ofVeneto. On the contrary, the areas with little or no seismic risk are theAlps (excluding the extreme western and eastern area), most of thePo Valley, the Tyrrhenian coasts up toLazio, central-southern Apulia,Sardinia and central Sicily.[32]
In recent years, numerous studies have also been conducted to better understand the structure and destructive potential of thesubmarine volcanoMarsili, located about 140 km (87 mi) north ofSicily and about 150 km (93 mi) west ofCalabria. With its 70 km (43 mi) of length and 30 km (19 mi) of width (equal to 2,100 km2 (810 sq mi) of surface) the Marsili is one of the largest volcanoes in Europe.
^If theCaucasus Mountains is considered outside the natural borders of the European continent, Etna appears to be the highest volcano in Europe; including the Caucasus, Etna still remains the continent's highest active volcano.
^"PETRANGELI: "IL CENTRO D'ITALIA NON SI TOCCA. SIAMO NOI!"" (in Italian). RietiLife. 2 March 2015. Retrieved22 May 2016.The Military Geographic Institute denied my offices the fact that the prestigious Army structure carried out a study on central Italy. The IGM not only knows nothing about it but has also reiterated, and will formally do so in the coming days, an information already known: the boot is not a geometric figure and it is therefore impossible to determine the exact location of central Italy.