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Silva Ciminia
The ''Silva Ciminia'', the Ciminian Forest, was the unbroken primeval forest that separated Ancient Rome from Etruria. According to the Roman historian Livy it was, in the 4th century BCE, a feared, pathless wilderness in which few dared tread. History The Ciminian Forest received its name from the Monti Cimini, which are still a densely wooded range of volcanic hills northwest of Rome. They form the part of the forerange of the Apennine main range that faces towards the Tyrrhenian Sea. In the south, the ''Silva Ciminia'' stretched from Lake Bracciano to the edges of the flat plain of the Roman Campagna, in the lower Tiber valley. Stretches of cleared fields round the major Etruscan settlements formed the ''Ager Veientanus'' that supported Veii, the ''Ager Faliscus'' of the Falisci, and the ''Ager Capenas'' of Capena. In the heart of the Ciminian woodlands lay the Ciminus Lake ( Lago di Vico). In the northwest, they reached as far as Tarquinia. The forest was predominantly f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancient Rome
In modern historiography, ancient Rome refers to Roman civilisation from the founding of the city of Rome in the 8th century BC to the collapse of the Western Roman Empire in the 5th century AD. It encompasses the Roman Kingdom (753–509 BC), Roman Republic (509–27 BC) and Roman Empire (27 BC–476 AD) until the fall of the western empire. Ancient Rome began as an Italic settlement, traditionally dated to 753 BC, beside the River Tiber in the Italian Peninsula. The settlement grew into the city and polity of Rome, and came to control its neighbours through a combination of treaties and military strength. It eventually dominated the Italian Peninsula, assimilated the Greek culture of southern Italy ( Magna Grecia) and the Etruscan culture and acquired an Empire that took in much of Europe and the lands and peoples surrounding the Mediterranean Sea. It was among the largest empires in the ancient world, with an estimated 50 to 90 million inhabitants, roughly 20% of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Bryan Ward-Perkins
John Bryan Ward-Perkins, (3 February 1912 – 28 May 1981) was a British Classical architectural historian and archaeologist, and director of the British School at Rome. Family and early life John Bryan Ward-Perkins was born on 3 February 1912 in Bromley, Kent, the eldest son of Bryan Ward-Perkins, a British civil servant in India, and Winifred Mary Hickman. He attended Winchester College and New College, Oxford, graduating in 1934. He was awarded the Craven travelling fellowship at Magdalen College, which he used to study archaeology in Great Britain and France. Career Ward-Perkins served as assistant under Sir R. E. Mortimer Wheeler (1890–1976) from 1936 to 1939 at the London Museum. There he wrote a catalogue of the museum's collection. During these years he was also involved in the excavation of a Roman villa near Welwyn Garden City. In 1939 he became chair of archaeology at the Royal University of Malta. During the Second World War, Ward-Perkins saw military servi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Via Flaminia
The Via Flaminia or Flaminian Way was an ancient Roman road leading from Rome over the Apennine Mountains to ''Ariminum'' (Rimini) on the coast of the Adriatic Sea, and due to the ruggedness of the mountains was the major option the Romans had for travel between Etruria, Latium, Campania, and the Po Valley. The section running through northern Rome is where Constantine the Great had his famous vision of the Chi Rho, leading to his conversion to Christianity and the Christianization of the Roman Empire. Today the same route, still called by the same name for much of its distance, is paralleled or overlaid by Strada Statale (SS) 3, also called Strada Regionale (SR) 3 in Lazio and Umbria, and Strada Provinciale (SP) 3 in Marche. It leaves Rome, goes up the Val Tevere ("Valley of the Tiber") and into the mountains at Castello delle Formiche, ascends to Gualdo Tadino, continuing over the divide at Scheggia Pass, to Cagli. From there it descends the eastern slope waterways betwe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Via Amerina
The ''Via Cassia'' ("way of Cassius") was an important Roman road striking out of the ''Via Flaminia'' near the Milvian Bridge in the immediate vicinity of Rome and, passing not far from Veii, traversed Etruria. The ''Via Cassia'' passed through Baccanae, Sutrium, Volsinii, Clusium, Arretium, Florentia, Pistoria, and Luca, joining the ''Via Aurelia'' at Luna. The ''Via Cassia'' intersected other important roads. At mile 11 the ''Via Clodia'' diverged north-north-west. At Sette Vene, another road, probably the ''Via Annia'', branched off to Falerii. In Sutrium, the ''Via Ciminia'' split off and later rejoined. The date of its construction is uncertain: it cannot have been earlier than 187 BC, when the consul Gaius Flaminius constructed a road from Bononia to Arretium, which must have coincided with a portion of the later Via Cassia. It is not mentioned by any ancient authorities before the time of Cicero, who in 45 BC speaks of the existence of three roads from Rome to Muti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Via Cassia
The ''Via Cassia'' ("way of Cassius") was an important Roman road striking out of the ''Via Flaminia'' near the Milvian Bridge in the immediate vicinity of Rome and, passing not far from Veii, traversed Etruria. The ''Via Cassia'' passed through Baccanae, Sutrium, Volsinii, Clusium, Arretium, Florentia, Pistoria, and Luca, joining the ''Via Aurelia'' at Luna. The ''Via Cassia'' intersected other important roads. At mile 11 the ''Via Clodia'' diverged north-north-west. At Sette Vene, another road, probably the ''Via Annia'', branched off to Falerii. In Sutrium, the ''Via Ciminia'' split off and later rejoined. The date of its construction is uncertain: it cannot have been earlier than 187 BC, when the consul Gaius Flaminius constructed a road from Bononia to Arretium, which must have coincided with a portion of the later Via Cassia. It is not mentioned by any ancient authorities before the time of Cicero, who in 45 BC speaks of the existence of three roads from Rome to Muti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roman Road
Roman roads ( la, viae Romanae ; singular: ; meaning "Roman way") were physical infrastructure vital to the maintenance and development of the Roman state, and were built from about 300 BC through the expansion and consolidation of the Roman Republic and the Roman Empire. They provided efficient means for the overland movement of armies, officials, civilians, inland carriage of official communications, and trade goods. Roman roads were of several kinds, ranging from small local roads to broad, long-distance highways built to connect cities, major towns and military bases. These major roads were often stone-paved and metaled, cambered for drainage, and were flanked by footpaths, bridleways and drainage ditches. They were laid along accurately surveyed courses, and some were cut through hills, or conducted over rivers and ravines on bridgework. Sections could be supported over marshy ground on rafted or piled foundations.Corbishley, Mike: "The Roman World", page 50. Warwick Press, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quercus Ilex
''Quercus ilex'', the evergreen oak, holly oak or holm oak is a large evergreen oak native to the Mediterranean region. It is a member of the ''Ilex'' section of the genus, with acorns that mature in a single summer. Description An evergreen tree of large size, attaining in favourable places a height of , and developing in open situations a huge head of densely leafy branches as much across, the terminal portions of the branches usually pendulous in old trees. The trunk is sometimes over in girth. The young shoots are clothed with a close gray felt. The leaves are very variable in shape, most frequently narrowly oval or ovate-lanceolate, long, 1.2–2.5 cm wide, rounded or broadly tapered at the base, pointed, the margins sometimes entire, sometimes (especially on young trees) more or less remotely toothed. When quite young, both surfaces are clothed with whitish down, which soon falls away entirely from the upper surface leaving it a dark glossy green; on the lower s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tundra
In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mountain tract". There are three regions and associated types of tundra: Arctic tundra, alpine tundra, and Antarctic tundra. Tundra vegetation is composed of dwarf shrubs, sedges, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monterosi
Monterosi is a ''comune'' (municipality) in the Province of Viterbo in the Italian region Lazio, located about 30 km (18,64 mi) north of the Grande Raccordo Anulare of Rome, about 40 km (24,85 mi) south of Viterbo. Geography Monterosi’s territory is located halfway through between Rome and Viterbo along the Via Cassia, on the north-easter foot of the Sabatine Hills, not far from Lake Bracciano. Within its borders lies the small Monterosi lake, legacy of a now-extinct volcanic activity in the region. Monterosi borders the following municipalities: Nepi, Sutri, Trevignano Romano Trevignano Romano is a small town and ''comune'' in the Metropolitan City of Rome, Lazio, central Italy. With a population of about 5,000, it is located on the volcanic Lake Bracciano. It is about away from Rome. History The presence of people .... References Cities and towns in Lazio {{Latium-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Crater Lake
A volcanic crater lake is a lake in a crater that was formed by explosive activity or a collapse during a volcanic eruption. Formation Lakes in calderas fill large craters formed by the collapse of a volcano during an eruption. Lakes in maars fill medium-sized craters where an eruption deposited debris around a vent. Crater lakes form as the created depression, within the crater rim, is filled by water. The water may come from precipitation, groundwater circulation (often hydrothermal fluids in the case of volcanic craters) or melted ice. Its level rises until an equilibrium is reached between the rates of incoming and outgoing water. Sources of water loss singly or together may include evaporation, subsurface seepage, and, in places, surface leakage or overflow when the lake level reaches the lowest point on its rim. At such a saddle location, the upper portion of the lake is contained only by its adjacent natural volcanic dam; continued leakage through or surface outflow ac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
