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The headwaters of the Po are a spring seeping from a stony hillside at Pian del Re, a flat place at the head of the Val Po under the northwest face of Monviso.

The Po then extends along the 45th parallel north before ending at a delta projecting into the Adriatic Sea near Venice. It is characterized by its large discharge several rivers over 1, km have a discharge inferior or equal to the Po.

As a result of its characteristics, the river is subject to heavy flooding. Consequently, over half its length is controlled with argini , levees.

The river flows through many important Italian cities, including Turin , Piacenza and Ferrara. It is connected to Milan through a net of channels called navigli , which Leonardo da Vinci helped design.

Near the end of its course, it creates a wide delta with hundreds of small channels and five main ones, called Po di Maestra , Po della Pila , Po delle Tolle , Po di Gnocca and Po di Goro at the southern part of which is Comacchio , an area famous for eels.

Along its path lie standing lakes. The major tributary in question is the northern source half of the eponymous Ticino river fed by its Moesa tributary in Grigioni and the top third of the Alpine lake, Maggiore, formed by it.

The southern two thirds of Lake Maggiore and the southern half of the continuing Ticino River tributary are in Italian territory.

Valle Etroite is so remote it is essentially administered by Italy telephone network, rubbish collections etc. Further minuscule parts of the Po's basin measurable in the hundreds of metres of linear distance within France are found in the form of small streamheads forced into France by the post war Peace Treaty of Paris as a punitive measure against Italy.

These can be found on the Mont Cenis and Mongenevre passes. The former contains a reservoir dammed at the Po end and so technically constitutes part of its basin, although it contributes little to the water flow as the water is, by definition, retained by the dam.

The two main economic uses of the valley are for industry and for agriculture, both major uses. The industrial centres, such as Turin and Milan, are located on higher terrain, away from the river.

Drainage from the north is mediated through several large, scenic lakes. The streams are now controlled by so many dams as to slow the river's sedimentation rate, causing geologic problems.

The expansive, moist and fertile flood plain is reserved mainly for agriculture and is subject to flash floods, even though the overall quantity of water is lower than in the past and lower than demand.

The main products of the farms around the river are cereals including — unusually for Europe — rice , which requires heavy irrigation.

The latter method is the chief consumer of surface water, while industrial and human consumption use underground water.

The Po has tributaries. The Reno R was a tributary of the Po until the middle of the eighteenth century when the course was diverted to lessen the risk of devastating floods.

The Po Delta wetlands have been protected by the institution of two regional parks in the regions in which it is situated: Veneto and Emilia-Romagna.

The Po Delta Regional Park in Emilia-Romagna, the largest, consists of four parcels of land on the right bank of the Po and to the south.

Created by law in , it is managed by a consortium, the Consorzio per la gestione de Parco , to which Ferrara and Ravenna provinces belong as well as nine comuni : Comacchio , Argenta , Ostellato , Goro , Mesola , Codigoro , Ravenna , Alfonsine , and Cervia.

Executive authority resides in an assembly of the presidents of the provinces, the mayors of the comuni and the board of directors.

It has a high biodiversity , with — plant species and vertebrate species, of which are birds. The most recent part of the delta, which projects into the Adriatic between Chioggia and Comacchio , contains channels that actually connect to the Adriatic and on that account is called the active delta by the park authorities, as opposed to the fossil delta, which contains channels that no longer connect the Po to the Adriatic but once did.

The active delta was created in when the city of Venice diverted the main stream, the Po grande or Po di Venezia , from its channel north of Porto Viro to the south of Porto Viro in a channel then called the Taglio di Porto Viro , "Porto Viro cut-off".

Their intent was to stop the gradual migration of the Po toward the lagoon of Venice, which would have filled up with sediment had contact been made.

The subsequent town of Taglio di Po grew around the diversionary works. The former exits at Bonelli. The latter divides again at Pila into the Busa di Tramontana to the north and the Busa di Scirocco to the south, while the mainstream, the Busa Dritta , enters Punta Maistra and exits finally past Pila lighthouse.

Despite the park administration's definition of the active delta as beginning at Porto Viro, there is another active channel upstream from it at Santa Maria in Punta, where the Fiume Po divides into the Po di Goro and the Po di Venezia.

The fossil Po is the region of no longer active channels from the Po to the sea. It begins upstream from Ferrara. The Fiume Po currently flowing to the north of Ferrara is actually the result of a diversion at Ficarolo in made in the hope of relieving flooding in the vicinity of Ravenna.

The diversion channel was at first called the Po di Ficarolo. The Fiume Po before then followed the Po di Volano , no longer connected to the Po, which ran to the south of Ferrara and exited near Volano.

In Roman times it did not exit there but ran to the south as the Padus Vetus "old Po" exiting near Comacchio , from which split the Po di Primaro exiting close to Ravenna.

The entire region from Ravenna to Chioggia was dense swamps, explaining why the Via Aemilia was constructed between Rimini and Piacenza and did not begin further north.

Typically in geologic history the depression is filled with sea water under various geologic names such as Tethys Sea.

In the last period of the Miocene Epoch, the Messinian 7—5 mya , the Messinian salinity crisis , a near drying of the Mediterranean, was caused by the sea level dropping below the sill at the Strait of Gibraltar and the equilibrium between evaporation and replenishment shifting in favor of evaporation.

At that time the Po Valley and the Adriatic depression were a single canyon system thousands of feet deep. On the southwest the Apennine Mountains bordered a land mass termed Tyrrhenis geologically.

Their orogeny was just being completed in the Miocene. On the north the Alpine Orogeny had already created the Alps.

At the end of the Messinian the ocean broke through the sill and the Mediterranean refilled. The Adriatic transgressed into all of northern Italy.

At the start of the Pleistocene the valley was full. Cycles of transgression and regression are detectable in the valley and the Adriatic as far as its centre and in the southern Adriatic.

From the Pleistocene alternation of maritime and alluvial sediments occur as far west as Piacenza. The exact sequences at various locations have been studied extensively.

An advance began after the Last Glacial Maximum around 20, years ago, which brought the Adriatic to a high point at about years ago.

Since then the Po delta had been prograding. Venice , which was originally built on islands off the coast, is most at risk due to subsidence, but the effect is realized in the Po delta as well.

The causes are first a decrease in the sedimentation rate due to the locking of sediment behind hydroelectric dams and the deliberate excavation of sand from rivers for industrial purposes.

Second, agricultural use of the river is heavy; during peak consumption the flow in places nearly dries up, causing local contention.

As a result of decreased flow salt water is intruding into the aquifers and coastal ground water.

Eutrophication in standing waters and streams of low flow is on the increase. Always prone to fog, the valley is subject to heavy smog due to industrial atmospheric emissions, especially from Turin.

The city of Milan had no sewage treatment plant s. Sewage went through channels directly into the Po, for which the European Environment Agency cited the city.

These treat the sewage from over 2. In , water from the Po was found to contain much benzoylecgonine , passed by cocaine users in urine.

On February 24, the Po was contaminated by an oil spill coming from a refinery in Villasanta through the Lambro , the Agenzia Nazionale Stampa Associata news agency has estimated it to be about , liters.

Until water resources were administered regionally or locally. The major authority on the lower Po was the Magistrato alle Acque di Venezia , first formed in the 16th-century Republic of Venice.

It made all the decisions concerning the diversion of the lower river. Most part of the delta is still in Veneto.

In under the Kingdom of Italy the agency became the Magistrato alle Acque and took responsibility for all the water resources in northeastern Italy.

Air bawah tanah mempunyai kandungan radon lebih tinggi di bandingkan air permukaan. Radon kadang digunakan oleh beberapa rumah sakit untuk kegunaan terapeutik.

Karena peluruhannya yang cukup cepat, radon juga digunakan dalam penyelidikan hidrologi yang mengkaji interaksi antara air bawah tanah, anak sungai dan sungai.

Peningkatan radon dalam anak sungai atau sungai merupakan petunjuk penting bahwa terdapat sumber air bawah tanah. Nama radon berasal dari radium.

Radon ditemukan pada tahun oleh Friedrich Ernst Dorn , yang menggelarnya sebagai pancaran radium. Pada tahun William Ramsay dan Robert Whytlaw-Gray , yang menamakannya niton dari bahasa latin nitens berarrti "yang berkilauan"; simbol Nt , mengisolasinya, menentukan kepadatannya dan mereka menemukan bahwa Radon adalah gas paling berat pada masa itu dan sampai sekarang.

Semenjak unsur 86 ini disebut Radon. Rata rata, terdapat satu molekul radon dalam 1 x 10 21 molekul udara. Radon dapat ditemukan di beberapa mata air dan mata air panas.

Kota Misasa , Jepang , terkenal karena mata airnya yang kaya dengan radium yang menghasilkan radon. Radon dibebaskan dari tanah secara alamiah, apalagi di kawasan bertanah di Granit.

Hampir satu rumah setiap 15 di A. Surgeon General dan EPA mencadangkan agar semua rumah diuji bagi radon. Sejak di Amerika, jutaan rumah telah diuji kandungan radonnya.

Pengujian menunjukkan bahwa flor dapat bereaksi dengan radon dan membentuk senyawa radon florida. Senyawa radon klathrat juga pernah ditemukan.

Diketahui ada dua puluh Isotop radon yang diketahui. Yang paling stabil adalah Rn yang merupakan produk sampingan dari peluruhan radium, Rn mempunyai waktu paruh 3, hari Rn adalah produk sampingan dari peluruhan thorium dan disebut thoron.

Waktu paruhnya Radon diturunkan dari actinium. Radon adalah gas karsinogen. Radon adalah zat beradioaktif dan harus ditangani secara hati-hati.

Adalah sangat berbahaya untuk menghirup unsur ini karena radon menghasilkan partikel alpha. Radon juga menghasilkan hasil peluruhan berbentuk padat, dan akibatnya, cenderung membentuk debu halus yang mudah memasuki jalur udara dan melekat permanen dalam jaringan paru-paru, menghasilkan paparan lokal yang parah.

Ruang di mana radium, aktinium, atau thorium disimpan perlu diangin-anginkan dengan baik agar tidak terakumulasi dalam udara.

Po rn o

The two main economic uses of the valley are for industry and for agriculture, both major uses. The industrial centres, such as Turin and Milan, are located on higher terrain, away from the river.

Drainage from the north is mediated through several large, scenic lakes. The streams are now controlled by so many dams as to slow the river's sedimentation rate, causing geologic problems.

The expansive, moist and fertile flood plain is reserved mainly for agriculture and is subject to flash floods, even though the overall quantity of water is lower than in the past and lower than demand.

The main products of the farms around the river are cereals including — unusually for Europe — rice , which requires heavy irrigation.

The latter method is the chief consumer of surface water, while industrial and human consumption use underground water.

The Po has tributaries. The Reno R was a tributary of the Po until the middle of the eighteenth century when the course was diverted to lessen the risk of devastating floods.

The Po Delta wetlands have been protected by the institution of two regional parks in the regions in which it is situated: Veneto and Emilia-Romagna.

The Po Delta Regional Park in Emilia-Romagna, the largest, consists of four parcels of land on the right bank of the Po and to the south.

Created by law in , it is managed by a consortium, the Consorzio per la gestione de Parco , to which Ferrara and Ravenna provinces belong as well as nine comuni : Comacchio , Argenta , Ostellato , Goro , Mesola , Codigoro , Ravenna , Alfonsine , and Cervia.

Executive authority resides in an assembly of the presidents of the provinces, the mayors of the comuni and the board of directors. It has a high biodiversity , with — plant species and vertebrate species, of which are birds.

The most recent part of the delta, which projects into the Adriatic between Chioggia and Comacchio , contains channels that actually connect to the Adriatic and on that account is called the active delta by the park authorities, as opposed to the fossil delta, which contains channels that no longer connect the Po to the Adriatic but once did.

The active delta was created in when the city of Venice diverted the main stream, the Po grande or Po di Venezia , from its channel north of Porto Viro to the south of Porto Viro in a channel then called the Taglio di Porto Viro , "Porto Viro cut-off".

Their intent was to stop the gradual migration of the Po toward the lagoon of Venice, which would have filled up with sediment had contact been made.

The subsequent town of Taglio di Po grew around the diversionary works. The former exits at Bonelli. The latter divides again at Pila into the Busa di Tramontana to the north and the Busa di Scirocco to the south, while the mainstream, the Busa Dritta , enters Punta Maistra and exits finally past Pila lighthouse.

Despite the park administration's definition of the active delta as beginning at Porto Viro, there is another active channel upstream from it at Santa Maria in Punta, where the Fiume Po divides into the Po di Goro and the Po di Venezia.

The fossil Po is the region of no longer active channels from the Po to the sea. It begins upstream from Ferrara. The Fiume Po currently flowing to the north of Ferrara is actually the result of a diversion at Ficarolo in made in the hope of relieving flooding in the vicinity of Ravenna.

The diversion channel was at first called the Po di Ficarolo. The Fiume Po before then followed the Po di Volano , no longer connected to the Po, which ran to the south of Ferrara and exited near Volano.

In Roman times it did not exit there but ran to the south as the Padus Vetus "old Po" exiting near Comacchio , from which split the Po di Primaro exiting close to Ravenna.

The entire region from Ravenna to Chioggia was dense swamps, explaining why the Via Aemilia was constructed between Rimini and Piacenza and did not begin further north.

Typically in geologic history the depression is filled with sea water under various geologic names such as Tethys Sea.

In the last period of the Miocene Epoch, the Messinian 7—5 mya , the Messinian salinity crisis , a near drying of the Mediterranean, was caused by the sea level dropping below the sill at the Strait of Gibraltar and the equilibrium between evaporation and replenishment shifting in favor of evaporation.

At that time the Po Valley and the Adriatic depression were a single canyon system thousands of feet deep.

On the southwest the Apennine Mountains bordered a land mass termed Tyrrhenis geologically. Their orogeny was just being completed in the Miocene.

On the north the Alpine Orogeny had already created the Alps. At the end of the Messinian the ocean broke through the sill and the Mediterranean refilled.

The Adriatic transgressed into all of northern Italy. At the start of the Pleistocene the valley was full. Cycles of transgression and regression are detectable in the valley and the Adriatic as far as its centre and in the southern Adriatic.

From the Pleistocene alternation of maritime and alluvial sediments occur as far west as Piacenza. The exact sequences at various locations have been studied extensively.

An advance began after the Last Glacial Maximum around 20, years ago, which brought the Adriatic to a high point at about years ago.

Since then the Po delta had been prograding. Venice , which was originally built on islands off the coast, is most at risk due to subsidence, but the effect is realized in the Po delta as well.

The causes are first a decrease in the sedimentation rate due to the locking of sediment behind hydroelectric dams and the deliberate excavation of sand from rivers for industrial purposes.

Second, agricultural use of the river is heavy; during peak consumption the flow in places nearly dries up, causing local contention.

As a result of decreased flow salt water is intruding into the aquifers and coastal ground water. Eutrophication in standing waters and streams of low flow is on the increase.

Always prone to fog, the valley is subject to heavy smog due to industrial atmospheric emissions, especially from Turin.

The city of Milan had no sewage treatment plant s. Sewage went through channels directly into the Po, for which the European Environment Agency cited the city.

These treat the sewage from over 2. In , water from the Po was found to contain much benzoylecgonine , passed by cocaine users in urine.

On February 24, the Po was contaminated by an oil spill coming from a refinery in Villasanta through the Lambro , the Agenzia Nazionale Stampa Associata news agency has estimated it to be about , liters.

Until water resources were administered regionally or locally. The major authority on the lower Po was the Magistrato alle Acque di Venezia , first formed in the 16th-century Republic of Venice.

It made all the decisions concerning the diversion of the lower river. Most part of the delta is still in Veneto. In under the Kingdom of Italy the agency became the Magistrato alle Acque and took responsibility for all the water resources in northeastern Italy.

Currently it is a decentralized institution of the Ministry of Public Works, headed by a chairman appointed by the Head of State and the Council of Ministers.

Its headquarters are in Venice. In in response to the major geologic problems that were developing along the river Law no.

Its headquarters have been in Parma since its inception in It considers itself a synergy among all the institutions concerned with the preservation and development of the Po basin.

It is administered by officials chosen from the administrations of the constituent regions and provinces. Between and the Po Valley Project the implementation of the plan took more than 60 measures, notably to: heighten and strengthen levees, increase flood-meadows , resume natural sediment transport and deposition points, enlarge wetlands, afforest, re-nature, promote biodiversity and recreational use.

Nine gates are 6. A spillway to the right passes through a hydroelectric station of 4 generators of 76 MW each operated by a 3. The Po is first certainly identified in the Graeco-Roman historians and geographers of the late Roman Republic and the early Roman Empire , long after the valley had been occupied successively by prehistoric and historic peoples: Ligures , Etruscans , Celts , Veneti , Umbri , and Romans.

At that late date the ancient authors were attempting to explain the provenance of the name. Perhaps the earliest of these, Polybius [19] 2nd century BC , uses Pados in Greek and says that it was to be identified with the Eridanos of the poets.

Moreover, the country people call it Bodencus. This implies that a "country" population either remained from prehistoric times or adopted the name in use by that substrate.

The name has been segmented as Bod-encus or Bod-incus , the suffix being characteristic of the ancient Ligurian language of northern Italy, southern France, Corsica and elsewhere.

Radon juga termasuk dalam kelompok gas mulia dan beradioaktif. Radon terbentuk dari peluruhan radium.

Radon juga gas yang paling berat dan berbahaya bagi kesehatan. Rn mempunyai waktu paruh 3,8 hari dan digunakan dalam radioterapi. Radon dapat memicu kanker paru paru dan telah menyebabkan Radon tidak mudah bereaksi secara kimia, tetapi beradioaktif, radon juga adalah gas alami senyawa gas terberat adalah tungsten heksaflorida , WF 6.

Pada suhu dan tekanan ruang, radon tidak berwarna tetapi apabila didinginkan hingga membeku, radon akan berwarna kuning, sedangkan radon cair berwarna merah jingga.

Air bawah tanah mempunyai kandungan radon lebih tinggi di bandingkan air permukaan. Radon kadang digunakan oleh beberapa rumah sakit untuk kegunaan terapeutik.

Karena peluruhannya yang cukup cepat, radon juga digunakan dalam penyelidikan hidrologi yang mengkaji interaksi antara air bawah tanah, anak sungai dan sungai.

Peningkatan radon dalam anak sungai atau sungai merupakan petunjuk penting bahwa terdapat sumber air bawah tanah. Nama radon berasal dari radium.

Radon ditemukan pada tahun oleh Friedrich Ernst Dorn , yang menggelarnya sebagai pancaran radium. Pada tahun William Ramsay dan Robert Whytlaw-Gray , yang menamakannya niton dari bahasa latin nitens berarrti "yang berkilauan"; simbol Nt , mengisolasinya, menentukan kepadatannya dan mereka menemukan bahwa Radon adalah gas paling berat pada masa itu dan sampai sekarang.

Semenjak unsur 86 ini disebut Radon. Rata rata, terdapat satu molekul radon dalam 1 x 10 21 molekul udara. Radon dapat ditemukan di beberapa mata air dan mata air panas.

Kota Misasa , Jepang , terkenal karena mata airnya yang kaya dengan radium yang menghasilkan radon. Radon dibebaskan dari tanah secara alamiah, apalagi di kawasan bertanah di Granit.

Hampir satu rumah setiap 15 di A. Surgeon General dan EPA mencadangkan agar semua rumah diuji bagi radon. Sejak di Amerika, jutaan rumah telah diuji kandungan radonnya.

Pengujian menunjukkan bahwa flor dapat bereaksi dengan radon dan membentuk senyawa radon florida.

Senyawa radon klathrat juga pernah ditemukan. Diketahui ada dua puluh Isotop radon yang diketahui. Yang paling stabil adalah Rn yang merupakan produk sampingan dari peluruhan radium, Rn mempunyai waktu paruh 3, hari Rn adalah produk sampingan dari peluruhan thorium dan disebut thoron.

As a result of decreased flow salt water is intruding into the aquifers and coastal ground water. Until water resources were administered regionally or locally. The Adriatic transgressed into all of northern Italy. Rata rata, terdapat satu molekul radon dalam 1 x 10 21 molekul udara. It considers itself a Cory chase home among all the institutions concerned with the preservation and Blowjobs for cash of the Po basin. At the end of the Messinian the ocean broke through the Gatlinburg craigslist personals and the Mediterranean refilled. The headwaters of the Po are a spring seeping from a Real amature sex hillside at Pian Whiteslavesblackgirls com Re, How to lick her pussy flat place at the head of the Val Po under the northwest face of Monviso. Inwater from the Po was found to contain much benzoylecgoninepassed by cocaine users in urine. It is characterized by its Asian sex cum discharge several rivers over 1, km have a discharge inferior or equal to Dogging sluts Po. He probably should know her Kobe tai cum, he was the Vice-President of the company after all. Sacha strips naked on her brown wicker chair. I mean, who am l kidding. Come on, Sara! I knew I had to get out of the house before I went crazy lol. Recommended Categories For You Mehr. Public Agent 20 Year Old Follar primera vez babe with a beautiful pair of boobs. Speaking of wet, because Black women who want white men exactly what happened to my lady parts whenever l thought of him. Sirens still sounded in the distance while she walked to the bus station. Everything about him was carnal. Serve them, would. Cartoons free porn chris By rubywright. And not just any guy, but a black guy, she reminded him as she slipped the nightie on.

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