Pliny the Elder
Pliny the Elder was a Roman author and natural philosopher, a naval and army commander of the early Roman Empire, friend of emperor Vespasian. Spending most of his spare time studying and investigating natural and geographic phenomena in the field, Pliny wrote the encyclopedic Naturalis Historia, which became an editorial model for encyclopedias, his nephew, Pliny the Younger, wrote of him in a letter to the historian Tacitus: For my part I deem those blessed to whom, by favour of the gods, it has been granted either to do what is worth writing of, or to write what is worth reading. In the latter number will be my uncle, of your compositions. Pliny the Younger refers to Tacitus’s reliance upon his uncle's book, the History of the German Wars. Pliny the Elder died in AD 79 in Stabiae while attempting the rescue of a friend and his family by ship from the eruption of Mount Vesuvius, which had destroyed the cities of Pompeii and Herculaneum; the wind caused by the sixth and largest pyroclastic surge of the volcano’s eruption did not allow his ship to leave port, Pliny died during that event.
Pliny's dates are pinned to the eruption of Mount Vesuvius in AD 79 and a statement of his nephew that he died in his 56th year, which would put his birth in AD 23 or 24. Pliny was the son of an equestrian, Gaius Plinius Celer, his wife, Marcella. Neither the younger nor the elder Pliny mention the names, their ultimate source is a fragmentary inscription found in a field in Verona and recorded by the 16th-century Augustinian monk Onofrio Panvinio at Verona. The form is an elegy; the most accepted reconstruction is PLINIVS SECVNDVS AVGV. LERI. PATRI. MATRI. MARCELLAE. TESTAMENTO FIERI IVSSOThe Vs represent Us, it should say "Plinius Secundus augur ordered this to be made as a testament to his father ler and his mother Marcella"The actual words are fragmentary. The reading of the inscription depends on the reconstruction, but in all cases the names come through. Whether he was an augur and whether she was named Grania Marcella are less certain. Jean Hardouin presents a statement from an unknown source that he claims was ancient, that Pliny was from Verona and that his parents were Celer and Marcella.
Hardouin cites the conterraneity of Catullus. How the inscription got to Verona is unknown, but it could have arrived by dispersal of property from Pliny the Younger's Tuscan estate at Colle Plinio, north of Città di Castello, identified for certain by his initials in the roof tiles, he kept statues of his ancestors there. Pliny the Elder was born at Como, not at Verona: it is only as a native of old Gallia Transpadana that he calls Catullus of Verona his conterraneus, or fellow-countryman, not his municeps, or fellow-townsman. A statue of Pliny on the façade of the Duomo of Como celebrates him as a native son, he had a sister, who married into the Caecilii and was the mother of his nephew, Pliny the Younger, whose letters describe his work and study regimen in detail. In one of his letters to Tacitus, Pliny the Younger details how his uncle's breakfasts would be light and simple following the customs of our forefathers; this shows that Pliny the Younger wanted it to be conveyed that Pliny the Elder was a "good Roman", which means that he maintained the customs of the great Roman forefathers.
This statement would have pleased Tacitus. Two inscriptions identifying the hometown of Pliny the Younger as Como take precedence over the Verona theory. One commemorates the younger's career as the imperial magistrate and details his considerable charitable and municipal expenses on behalf of the people of Como. Another identifies his father Lucius' village as Fecchio near Como. Therefore, Plinia was a local girl and Pliny the Elder, her brother, was from Como. Gaius was a member of the Plinia gens: the insubric root Plina still persists, with rhotacism, in the local surname "Prina", he did not take his father's cognomen, but assumed his own, Secundus. As his adopted son took the same cognomen, Pliny founded the Plinii Secundi; the family was prosperous. No earlier instances of the Plinii are known. In 59 BC, only about 82 years before Pliny's birth, Julius Caesar founded Novum Comum as a colonia to secure the region against the Alpine tribes, whom he had been unable to defeat, he imported a population of 4,500 from other provinces to be placed in Comasco and 500 aristocratic Greeks to found Novum Comum itself.
The community was thus multi-ethnic and the Plinies could have come from anywhere. No record of any ethnic distinctions in Pliny's time is apparent; the population prided themselves on being Roman citizens. Pliny the Elder had no children. In his will, he adopted his nephew; the adoption is called a "testamental adoption" by writers on the topic, who assert that it applied to the name change only, but Roman jurisprudence recognizes no such category. Pliny the Younger thus became the adopted son of Pliny the Elder after the latter's death. Fo
Emilia-Romagna is an administrative region of Northeast Italy comprising the historical regions of Emilia and Romagna. Its capital is Bologna, it has an area of 22,446 km2, about 4.4 million inhabitants. Emilia-Romagna is one of the wealthiest and most developed regions in Europe, with the third highest GDP per capita in Italy. Bologna, its capital, has one of Italy's highest quality of life indices and advanced social services. Emilia-Romagna is a cultural and tourist centre, being the home of the University of Bologna, the oldest university in the world, containing Romanesque and Renaissance cities, a former Eastern Roman Empire capital such as Ravenna, encompassing eleven UNESCO heritage sites, being a centre for food and automobile production and having popular coastal resorts such as Cervia, Cesenatico and Riccione. In 2018, the Lonely Planet guide named Emilia Romagna as the best place to see in Europe; the name Emilia-Romagna is a legacy of Ancient Rome. Emilia derives from the via Aemilia, the Roman road connecting Piacenza to Rimini, completed in 187 BC and named after the consul Marcus Aemilius Lepidus.
Romagna derives from Romània, the name of the Eastern Roman Empire applied to Ravenna by the Lombards when the western Empire had ceased to exist and Ravenna was an outpost of the east. Before the Romans took control of present-day Emilia-Romagna, it had been part of the Etruscan world and that of the Gauls. During the first thousand years of Christianity trade flourished, as did culture and religion, thanks to the region's monasteries. Afterwards the University of Bologna—arguably the oldest university in Europe—and its bustling towns kept trade and intellectual life alive, its unstable political history is exemplified in such figures as Matilda of Canossa and contending seigniories such as the Este of Ferrara, the Malatesta of Rimini, the Popes of Rome, the Farnese of Parma and Piacenza, the Duchy of Modena and Reggio. In the 16th century, most of these were seized by the Papal States, but the territories of Parma and Modena remained independent until Emilia-Romagna became part of the Italian kingdom between 1859 and 1861.
After the referendum of 2006, seven municipalities of Montefeltro were detached from the Province of Pesaro and Urbino to join that of Rimini on 15 August 2009. The municipalities are Casteldelci, Novafeltria, San Leo, Sant'Agata Feltria and Talamello. On 20 and 29 May 2012 two powerful earthquakes hit the area, they caused churches and factories to collapse. 200 were injured. The 5.8 magnitude quake left 14,000 people homeless. The region of Emilia-Romagna consists of nine provinces and covers an area of 22,446 km², ranking sixth in Italy. Nearly half of the region consists of plains while 27 % is 25 % mountainous; the region's section of the Apennines is marked by areas of badland erosion and caves. The mountains stretch for more than 300 km from the north to the south-east, with only three peaks above 2,000 m – Monte Cimone, Monte Cusna and Alpe di Succiso; the plain was formed by the gradual retreat of the sea from the Po basin and by the detritus deposited by the rivers. Marshland in ancient times, its history is characterised by the hard work of its people to reclaim and reshape the land in order to achieve a better standard of living.
The geology varies, with lagoons and saline areas in the north and many thermal springs throughout the rest of the region as a result of groundwater rising towards the surface at different periods of history. All the rivers rise locally in the Apennines except for the Po, which has its source in the Alps in Piedmont; the northern border of Emilia-Romagna follows the path of the river for 263 km. The region has a temperate broadleaved and mixed forests and the vegetation may be divided into belts: the Common oak-European hornbeam belt, now covered with fruit orchards and fields of wheat and sugar beet, the Pubescent oak-European hop-hornbeam belt on the lower slopes up to 900 m, the European beech-Silver fir belt between 1,000 and 1,500 m and the final mountain heath belt. Emilia-Romagna has two Italian National Parks, the Foreste Casentinesi National Park and the Appennino Tosco-Emiliano National Park. Emilia-Romagna has been a populated area since ancient times. Inhabitants over the centuries have radically altered the landscape, building cities, reclaiming wetlands, establishing large agricultural areas.
All these transformations in past centuries changed the aspect of the region, converting large natural areas to cultivation, up until the 1960s. The trend changed, agricultural lands began giving way to residential and industrial areas; the increase of urban-industrial areas continued at high rates until the end of the 2010s. In the same period and mountainous areas saw an increase in the registration of semi-natural areas, because of the abandonment of agricultural lands. Land use changes can have strong effects on ecological functions. Human interactions such as agriculture and deforestation affect soil function, e.g. food and other biomass production, storing and transformation, habitat and gene pool. In the Emilia-Romagna plain, which represents half of the region and where three quarters of the population of the region live, the agricultural land area has been reduced by 157 km2 while urban and industrial areas
Alpe di Succiso
The Alpe di Succiso is a mountain in the northern Apennines, located in the trait between the Cerreto and Lagastrello Passes, with an altitude of 2,017 m. It has a pyramidal appearance, carved by several gorges; the rivers Secchia and Enza, right affluences of the Po River, have their source in the Alpe di Succiso. The mountain is part of the National Park of the Appennino Tosco-Emiliano
The Po Valley, Po Plain, Plain of the Po, or Padan Plain is a major geographical feature of Northern Italy. It extends 650 km in an east-west direction, with an area of 46,000 square kilometres including its Venetic extension not related to the Po river basin; the flatlands of Veneto and Friuli are considered apart since they do not drain into the Po, but they combine into an unbroken plain. The plain is the surface of an in-filled system of ancient canyons extending from the Apennines in the south to the Alps in the north, including the northern Adriatic. In addition to the Po and its affluents the contemporary surface may be considered to include the Savio and Reno to the south, the Adige, Brenta and Tagliamento of the Venetian Plain to the north, among the many streams that empty into the north Adriatic from the west and north. Geo-political definitions of the valley depend on the defining authority; the Po Basin Water Board, authorized in 1989 by Law no. 183/89 to oversee "protection of lands, water rehabilitation, the use and management of hydro resources for the national economic and social development, protection of related environment" within the Po basin, has authority in several administrative regions of north Italy, including the plain north of the Adriatic and the territory south of the lower Po, as shown in the regional depiction included with this article.
The law defines the Po basin as "the territory from which rainwater or snow and glacier melt flows on the surface, gathers in streams of water either directly or via tributaries...". The United Nations Environment Program includes the Alps and Apennines as far as the sources of the tributaries of the Po but excludes Veneto and that portion of Emilia-Romagna south of the lower Po; the altitude of the valley through which the Po flows, exclusive of its tributaries, varies from 4 m below sea level in the Polesine subregion to about 2,100 m at the river's origin in the southern Piedmontese province of Cuneo known as the Provincia granda. The valley is crossed by a number of affluents running down from the Alps in the north and from the Apennines in the south; the Po's major affluents include the Tanaro, Trebbia and Secchia in the south, Dora Riparia, Dora Baltea, Ticino, Adda and Mincio in the north. The Po Valley and the Adriatic overlay a foreland basin and a system of buried ancient canyons surviving from the tectonic collision of an offshore land mass, with the mainland, an incident within the collision of the African and Eurasian plates.
Since the Messinian the system has been filling with sediment from the older Apennines but from the Alps. The shoreline of the Adriatic depends on a balance between the sedimentation rate and isostatic factors; until about 1950 the Po delta was prograding into the Adriatic. After that time due to human alteration of geologic factors, such as the sedimentation rate, the delta has been degrading and the coastline subsiding, resulting in ongoing contemporaneous crises in the city of Venice, where much irreplaceable art and architecture is to be lost due to soaring sea level in the next centuries. Where the land surface now dips below sea level the river must run at a relative elevation between dikes; the Malossa gas condensate field was discovered in 1973 and produces at depths of 6 km from the Upper Triassic Dolomia Principale dolomite and the Lower Jurassic Zandobbio dolomite, capped by the Lower Cretaceous Marne di Bruntino marl. The Po Valley is regarded as a syncline, or dip in the crust due to compression at the edges.
Regardless of whether this concept describes its geology, the valley is manifestly a sediment-filled trough, or virtual syncline, continuous with the deeps of the Adriatic Sea. The surface terrain is therefore divided into two overall types of landform: the plain, or flat surface of the fill, the anticline at the edges, taking the form of hilly country in which the outcrops of the original rock are visible along with alluvial fans formed from the outwash of the more severe anticlinal terrain; the valley is broadly divided into an upper, drier part not suited for agriculture, a lower fertile, well irrigated section, known in Lombardy and western Emilia as la Bassa, "the low". The upper areas of the Po valley take local names which reflect in their meanings their being modestly suited for farming. So we have the Piedmontese vaude and baragge, the Lombard brughiere and Groane, or, exiting from the Po valley proper, the Friulian magredi, areas remote from reachable water tables and covered with dense woods or dry soils.
This specific meaning for "lower plain" derive from a geologic feature called the fontanili line or zone, a band of springs around the Val Po, heaviest on the north, on the lowermost slopes of the anticline. It varies from a few kilometres to as much as 50 km wide; the fontanili line is the outcrop, or intersection, of the anticline's water table with the surface at the edge of the bassa. The rock above the line is porous. Surface water in the intermittent streams of the mountains tends to disappear below ground only to spring out again in the spring zone; the spring zone is called "the middle valley." Sur
Pavullo nel Frignano
Pavullo nel Frignano is a town and comune in the province of Modena, Emilia-Romagna, Italy, in the Modenese Apeninnes. It is home to the medieval Castle of Montecuccolo, birthplace of the 17th century condottiero Raimondo Montecuccoli, of the pieve of San Giovanni Battista di Renno; the town was extensively damaged during World War II due to its proximity to the Gothic Line. The economy is based on agriculture; the 2006 World Cup winning Italian footballer Luca Toni was born in Pavullo nel Frignano. The airport Pavullo nel Frignano Airport is in the commune
Tuscany is a region in central Italy with an area of about 23,000 square kilometres and a population of about 3.8 million inhabitants. The regional capital is Florence. Tuscany is known for its landscapes, artistic legacy, its influence on high culture, it is regarded as the birthplace of the Italian Renaissance and has been home to many figures influential in the history of art and science, contains well-known museums such as the Uffizi and the Pitti Palace. Tuscany produces wines, including Chianti, Vino Nobile di Montepulciano, Morellino di Scansano and Brunello di Montalcino. Having a strong linguistic and cultural identity, it is sometimes considered "a nation within a nation". Tuscany is a popular destination in Italy, the main tourist spots are Florence, Lucca, Versilia and Chianti; the village of Castiglione della Pescaia is the most visited seaside destination in the region, with seaside tourism accounting for 40% of tourist arrivals. Additionally, Lucca, the Chianti region and Val d'Orcia are internationally renowned and popular spots among travellers.
Seven Tuscan localities have been designated World Heritage Sites: the historic centre of Florence. Tuscany has over 120 protected nature reserves, making Tuscany and its capital Florence popular tourist destinations that attract millions of tourists every year. In 2012, the city of Florence was the world's 89th most visited city, with over 1.834 million arrivals. Triangular in shape, Tuscany borders the regions of Liguria to the northwest, Emilia-Romagna to the north, Marche to the northeast, Umbria to the east and Lazio to the southeast; the comune of Badia Tedalda, in the Tuscan Province of Arezzo, has an exclave named Ca' Raffaello within Emilia-Romagna. Tuscany has a western coastline on the Ligurian Sea and the Tyrrhenian Sea, among, the Tuscan Archipelago, of which the largest island is Elba. Tuscany has an area of 22,993 square kilometres. Surrounded and crossed by major mountain chains, with few plains, the region has a relief, dominated by hilly country used for agriculture. Hills make up nearly two-thirds of the region's total area, covering 15,292 square kilometres, mountains, a further 25%, or 5,770 square kilometres.
Plains occupy 8.4% of the total area—1,930 square kilometres —mostly around the valley of the Arno. Many of Tuscany's largest cities lie on the banks of the Arno, including the capital Florence and Pisa; the climate is mild in the coastal areas, is harsher and rainy in the interior, with considerable fluctuations in temperature between winter and summer, giving the region a soil-building active freeze-thaw cycle, in part accounting for the region's once having served as a key breadbasket of ancient Rome. The pre-Etruscan history of the area in the late Bronze and Iron Ages parallels that of the early Greeks; the Tuscan area was inhabited by peoples of the so-called Apennine culture in the late second millennium BC who had trading relationships with the Minoan and Mycenaean civilizations in the Aegean Sea. Following this, the Villanovan culture saw Tuscany, the rest of Etruria, taken over by chiefdoms. City-states developed in the late Villanovan before "Orientalization" occurred and the Etruscan civilization rose.
The Etruscans created the first major civilization in this region, large enough to establish a transport infrastructure, to implement agriculture and mining and to produce vibrant art. The Etruscans lived in the area of Etruria well into prehistory; the civilization grew to fill the area between the Arno and Tiber from the eighth century BCE, reaching its peak during the seventh and sixth centuries B. C. succumbing to the Romans by the first century BCE. Throughout their existence, they lost territory to Magna Graecia and Celts. Despite being seen as distinct in its manners and customs by contemporary Greeks, the cultures of Greece, Rome, influenced the civilization to a great extent. One reason for its eventual demise was this increasing absorption by surrounding cultures, including the adoption of the Etruscan upper class by the Romans. Soon after absorbing Etruria, Rome established the cities of Lucca, Pisa and Florence, endowed the area with new technologies and development, ensured peace.
These developments included extensions of existing roads, introduction of aqueducts and sewers, the construction of many buildings, both public and private. However, many of these structures have been destroyed by erosion due to weather; the Roman civilization in the West of the Roman Republic and Roman Empire collapsed in the fifth century, the region fell to barbarians migrating through the Empire from Eastern Europe and Central Asia of the Goths was re-conquered by the revived Eastern Roman Empire under the strong Emperor Justinian. In the years following 572, the Lombards arrived and designated Lucca the capital of their subsequent Tuscia. Pilgrims travelling along the Via Francigena between Rome and France brought wealth and development during the medieval period; the food and shelter required by the
A river mouth is the part of a river where the river debouches into another river, a lake, a reservoir, a sea, or an ocean. The water from a river can enter the receiving body in a variety of different ways; the motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface; the river water will either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alongside these advective transports, inflowing water will diffuse. At the mouth of a river, the change in flow condition can cause the river to drop any sediment it is carrying; this sediment deposition can generate a variety of landforms, such as deltas, sand bars and tie channels.
Many places in the United Kingdom take their names from their positions at the mouths of rivers, such as Plymouth and Great Yarmouth. Confluence River delta Estuary Liman