Bungalow cavallino Jesolo

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Benvenuti a Garden Paradiso: Bungalow cavallino Jesolo - Ièsolo [ò], up to the 1930 Cavazuccherina, common of Veneto (prov. Venice), situated to 2 ms of halt. to the oriental limit of the Venetian lagoon (mouth of the Sile), near the mouth of the Piave, to 3-4 kms from the open sea; 95,72 km²s; 22.395 abs. (Iesolani). Near the country they flow the ancient branch of the Piave, says Piave Vecchia and the navigable channel that it unites the Piave to the sea. Important center ortofrutticolo; breeding of cattle. Tourist station very frequented (Beach of Iesolo).
—St. it is the ancient Equilia, already garrison Roman, destroyed by Pipino king of the Franchis in the IX sec. Risen in the X sec., it was Episcopalian center up to the XV sec. During the first world war it was theater of sour fights.
Geography
Region (18.390 km2s; 4.525.200 abs. respects 2000) of Italy northern gulf in Venice), it confines to N with Austria and you/he/she is delimited to Of it from the Friuli-Venice Giulia, to NW from the Trentino-tall Adige, to W from the Lombardy, to S from the Emilia-Romagna. Regional chief town is Venice. Administratively it is separated in the seven provinces of Belluno, Padua, Rovigo, Treviso, Venice, Verona, Vicenza. The term Veneto, that refers to the ancient people illirico of the Venetian ones, appeared only in the second halves the sec. XVIII to designate the territories of dry land of the Republic in Venice, that is the actual Venetian provinces, anymore the territories lombardi of the Bresciano, of the Bergamasco and of the Cremasco, the Friuli and big part of the Istria. You tried to replace him/it with the names in Venice Propria, that it didn't have fortune, and of Venice Euganea, made among the two world conflicts but the name official Veneto it always prevailed both in the use of the people and in the scientific publications and at the end of the second world war you/he/she was welcomed in the today's form in the Italian Constitution.
Geomorphology and climate
From the morphological point of view you/they can be individualized in the regional territory at least four zones. The alpine zone includes the whole northern sector of the region and corresponds in its great lines to the superior basin of the Piave with the oriental Dolomiteses; it deals with a whole elevated mountainous groups, among which the most known are the Antelao, the Crystal, Her Tofane, the Three Tops of Lavaredo, the Marmaroles, the Marmolada, the Owl and the Pelmo, constituted in great prevalence by sedimentary rocks, for the more dolomies and limestones. The band prealpina extends a great deal him less in depth in the alpine system but it is more continuous lengthening himself/herself/itself from the Garda to the border with the Friuli-Venice Giulia. The reliefs are more lower part and introduces the aspect of calcareous highlands, largely interested by the phenomenons carsici, or from ample backs undulated, individualized by the deep throats of the most greater Venetian rivers. From SW to Of it they happen him: the group of the Daring mountain, delimited from the Lake of Garda and from the furrow vallivo of the Adige; the Lessini mountains; the Prealpis of Schio (or Small Dolomiteses) with part of the thick one of the Pasubio; the highland of Tonezza among the deep incisions vallive of the streams Posina and Astico; the undulated highland of the Seven Communes (or of Asiago), that the deep gorge of the Channel of Brenta clearly separates from the Grappa; the Prealpis Bellunesi (With the Visentin) and more over still the Prealpis of the Alpago with the highland of the Cansiglio and the Prealpis Clautane (the Priests' Top). The passage among the zone prealpina and that of lowland you/he/she is marked by a wider band of hilly reliefs subalpini, among which the dorsal ones lower than the Lessini mountains, the Berici mountains, the Necks Euganei, the morainic reliefs of the Garda and the Meschio, the Necks Asolani and the Montello. The lowland happens, finally formed by recent floods and divided by the band of the risorgives in the tall and low lowland. The coast, that extends him to arc among the mouths of the Po of Goro and the Tagliamento, is low and uniform, for vast lines interested by lagoon areas, that constitute a landscape of transition between the dry land and the sea: the two showier morphological elements are the Delta Padano and the Venetian Lagoon. The climate introduces very different characters from zone to zone, with extreme in correspondence of the tall basin of the Piave and in the zone of the Garda. In the lowland the summers are warm and the cold winters; on the reliefs prealpini and alpine they sensitively increase the daily thermal excursions, while they are having the tendency to decrease those annual: the summers are fresh almost everywhere and you ventilate and the winters are not rigid, especially in the areas exposed better to the sun. The precipitations are plentiful in the alpine zone and especially in that prealpina, but they are scarce in the areas of lowland, especially in the Delta Padano. Protected from the colds winds of the North from the alpine chain, the region is exposed to the winds of Of it and of If, that is to the bora, cold and dry, and to the damp sirocco. The principals raced of water are the Po, that interests only the region with its inferior course, marking good part of the border with the Emilia-Romagna and the Adige, of which it belongs to Veneto the whole line in the lowland: entirely Venetian it is the Piave. All the other rivers (Brenta, Bacchiglione, Livenza, Sile, Zero and Dese) they have origin in the region prealpina and they cross the lowland, following the general inclination of it to If, and they have enriched from the waters of risorgiva. The courses of water have the most greater courses in the autumn months and especially in those spring, when to the abundant precipitations the waters of breakup of the snows are added.