Umbria holiday rentals Umbria Italy
Umbria holiday rentals Umbria Italy
Umbria holiday rentals Umbria Italy: Umbria is a Region (8456 km2s; 832.675
abs. in 2000) of Italy centrale_[1v\h1"10410139"_[0v, without result
to the sea; it confines to Of it and to And with the Marche_[1v\h5"marche"_[0vs,
to S with the Lazio_[1v\h5"lazio_1"_[0v, to W and NW with the Toscana_[1v\h5"toscana"_[0v
_[1v\h6"map00214"_[0v. Regional chief town is Perugia_[1v\h5"perugia_2"_[0v:
administratively it is separated in the two provinces of Perugia_[1v\h5"perugia_1"_[0v
and Terni_[1v\h5"terni_1"_[0v. The denomination Umbria goes up again
to the antiquity and is due to the Umbri_[1v\h5"umbri"_[0vs, that
in epoch protostoricas lived the region appenninica between the Tevere_[1v\h5"tevere"_[0v
and the Adriatico_[1v\h5"adriatico_mare_"_[0v. Umbria during the
Italian unification also included the territory of the today's province of
Rieti_[1v\h5"rieti_1"_[0v, that was constituted in 1923 passing
to the Lazio, and he/she was formed from the alone province of Perugia up
to 1927, when the regional territory was separated in the two today's provincial
circoscrizioni_[1v\h5"circoscrizione"_[0v.
Geomorphology and climate
The depth furrow vallivo of tectonic origin, constituted from the Val Tiberina_[1v\h5"tiberina_valle_"_[0v
and from the Valley Umbra, it separates the reliefs appenninici to And from
those subappenninicis to W; the first ones are more raised and sour, the lowest
seconds and characterized by forms rounded off for the most greater frequency
of more tender rocks, in prevalence arenacee and clayey. Between the most
greater alignments and mountainous groups they are the Sibillini_[1v\h5"sibillini_monti_"_[0v
Mountains, to the border with the Brands, the arenacea Shuts of May and the
Subasio_[1v\h5"subasio"_[0v mountain. In the mountainous region
they open some vast tectonic conche_[1v\h5"conca1"_[0vs, that formed
lake bacini_[1v\h5"bacino"_[0v to the beginning of the Quaternario_[1v\h5"quaternario_1"_[0v,
subsequently gradually filled by the river floods, except that of the Trasimeno.
Mended by the continental influences of the areas more northern appenniniche
and open to the influences mitigatrici of the sea, that makes him feel in
depth along the valley of the Tevere, the region it has a climate of transition
with prevailing imprint submediterranea. The winters are not very cold and
the fresh summers and you ventilate. Remarkable I am however the thermal differences
and pluviometriche between the inside basins and the more elevated mountainous
reliefs, due to the differences of altitudine_[1v\h5"altitudine"_[0v,
to the orientation of the mountainous groups and their exposure. The precipitations
gradually extend to increase proceeding from the lowest basins and better
sheltered to the mountainous slopes that are exposed more directly to the
damp tides of air, where superior values are also reached to the 1400 annual
mms. The Tevere assumes in territory umbro an enough regular regime for I
bring him equalizer of his tributary of right, that has winter floods and
you accents thin summer, and of those of left, that they cross a more permeable
and richer region of precipitazioni_[1v\h5"precipitazione"_[0v and
they have long periods of soft in the spring and summer months. The vast lake
is the Trasimeno, one of the most greater of the Italian peninsula, sets in
proximity of the border with Tuscany.
