Salonika: Difference between revisions
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The original geographic footprint of the city of Salonika encompassed a shallow harbor and surrounding acreage on the northern shore of the Karpophoros peninsula, with tracts of farmland surrounding the ancient city walls. Ceaseless outward expansion has led the city footprint to envelop virtually the entire western half of the peninsula, as well as several historic towns which were incorporated into the city in the 18th century. The city's landscape is marked by intervening plains and hills, vast swaths of historic parkland, and various segments of beach shores and cliffed outcroppings to the sea. Salonika possesses a voluminous artificial reservoir, in the vicinity of the Imperial Palace, which feeds a system of historic canals that carry water toward districts situated closer to the urban center of the city. | The original geographic footprint of the city of Salonika encompassed a shallow harbor and surrounding acreage on the northern shore of the Karpophoros peninsula, with tracts of farmland surrounding the ancient city walls. Ceaseless outward expansion has led the city footprint to envelop virtually the entire western half of the peninsula, as well as several historic towns which were incorporated into the city in the 18th century. The city's landscape is marked by intervening plains and hills, vast swaths of historic parkland, and various segments of beach shores and cliffed outcroppings to the sea. Salonika possesses a voluminous artificial reservoir, in the vicinity of the Imperial Palace, which feeds a system of historic canals that carry water toward districts situated closer to the urban center of the city. | ||
Much of the old city center is densely populated and consists of narrow streets and medieval boulevards interrupted by urban plazas; the outer ring districts often provide much greater swaths of green space. During the | Much of the old city center is densely populated and consists of narrow streets and medieval boulevards interrupted by urban plazas; the outer ring districts often provide much greater swaths of green space. During the city's expansion in the 19th and early 20th century, large tracts of parks, water features, and monumental outdoor spaces were constructed as part of a beautification rivalry with Praetonian city of Kingston and the Cravanian city of Laurana. | ||
The city itself encompasses a total area of 18,000 square kilometres, extending roughly 150 kilometres east-west and 120 kilometers north-south; with a population density of 2,351 persons per square kilometre, and a population exceeding 40 million, it is one of thirteen cities in mainland Willink to be considered a {{wpl|Megacity|megacity}} for statistical purposes. Salonika possesses a {{wpl|Mediterranean climate#Hot-Summer mediterranean climate|hot summer Mediterranean climate}}, with hot, dry summers and mild winters marked by increased rainfall. Salonika has experienced sporadic snowfall, the most recent instances being in 2017. Generally, temperatures rarely fall below below 65.0 °F (18.3 °C), and the summer daily mean temperature charts at 80 °F (26.6 °C). | The city itself encompasses a total area of 18,000 square kilometres, extending roughly 150 kilometres east-west and 120 kilometers north-south; with a population density of 2,351 persons per square kilometre, and a population exceeding 40 million, it is one of thirteen cities in mainland Willink to be considered a {{wpl|Megacity|megacity}} for statistical purposes. Salonika possesses a {{wpl|Mediterranean climate#Hot-Summer mediterranean climate|hot summer Mediterranean climate}}, with hot, dry summers and mild winters marked by increased rainfall. Salonika has experienced sporadic snowfall, the most recent instances being in 2017. Generally, temperatures rarely fall below below 65.0 °F (18.3 °C), and the summer daily mean temperature charts at 80 °F (26.6 °C). |
Revision as of 01:40, 2 June 2020
Salonika | |
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Clockwise from the top: The skyline of the city from Karpophoros Bay, the Salonika Canal Bridge, the ancient sea-facing port facilities of Salonika, residences along hills in the Nótiapýli periochí, cityscape near the waterfront in the Fulbertus periochí | |
Country | Willink |
Episkopi | Patriarchate of Salonika |
Settled | c.640 BC |
Government | |
• Type | Association of municipal corporations |
• Body | Estates of Salonika |
• Hypatos | Emilios Frangopoulos |
Population (2020) | |
• Urban | 42,320,500 |
• Metro | 162,520,000 |
Demonym | Salonikan |
Time zone | +1 (Kingston Mean Time) |
Salonika (Willinkian: Σαλονίκα) (Mariac: 𐡎𐡀𐡋𐡅𐡍𐡉𐡊𐡀) is the de facto and historical capital, as well as most populous city of Willink. Salonika is a port situated on the Karpophoros Peninsula, a 200 kilometer long landmass extending outward from the southern extension of Vóreios mountain range toward the Fospontis Sea. With a population of over 42 million persons, Salonika is the largest and most important city in the central Fospontia region of Willink, as well as the traditional seat of the Willinkian Basileus and the Willinkian Orthodox Church.
Salonika is believed to have been founded around 640 BC, and had attained prominence as a significant Norian polis of some 50,000 people by 300 BC; it was later incorporated into the Kingdom of Fospontia and Kingdom of Fillinkis, alternating as the capital with the cities of Epidaurum and Botrys from 200 BC to 1400 AD; in the 1400s in assumed position as the permanent seat of government. As the principle internal seaport of the Fospontis Sea, the city thereafter experienced massive population growth, swelling to over two million residents and becoming one of Haven's largest cities by the 16th century. For over six hundred years, Salonika has constituted one of Haven's most important centers of finance, trade, art, architecture and science, and is considered an alpha world city by the Pacitalian affairs publication The Economist.
History
Evidence of neolithic occupation of the current site of the city points to settlement in the year 1200 BC, but there is no mention of any large settlements in the Kanis record reflective of the site. The current city is believed to have been founded by colonists sailing east from Myrina in 640 BC; the coast where the ancient city was established was sheltered from the Fospontis Sea and possessive of a convenient, shallow harbor which permitted the construction of expansive quays to unload goods. Eventually, the ancient city was further linked with Norian city-states to the west via the construction of the Grand Coastal Road. Located roughly midpoint the Fospontis, Salonika developed into an early important port and emporium, providing the link to the isolated eastern city-state of Ismaros and seclusion from Vatae tribal polities in the north given the vast mountain ranges inland the coast.
The ancient core of the city lies on the northern coast of the Karapophoros peninsula; the original city walls, dating from the 5th century BC exist in several small segments, but were mostly built over by the turn of the millennium. The extant city walls cover a much larger footprint, and date from the fifteenth century by which the city had expanded tremendously in every direction. Several important pre-Christian sites remain within the confines of the ancient walls, including the city's public baths, asklepieion, and partial elements of the basilica.
Administration
Local Administration
Salonika does not possess a government per se; it consists of the historical City of Salonika, whose boundaries are confined to the original city walls, and various dēmos, subdivisions hosting their own voluntary municipal corporations. The main body politic of these associations is the Estates of Salonika, a deliberative body encompassing both corporate entities and individual property owners. The city estates generally are responsible for what would be approximated as urban planning by means of a system of market urbanism, including collective provision of street maintenance and utilities through merchant and landlord associations, provision of emergency services, and voluntary zoning and protection of historic buildings through restrictive covenant on allowable property usage. Salonika is thought to be one of the largest cities in the world without zoning laws and without government provision of policing or roads.
National Administration
Geography
The original geographic footprint of the city of Salonika encompassed a shallow harbor and surrounding acreage on the northern shore of the Karpophoros peninsula, with tracts of farmland surrounding the ancient city walls. Ceaseless outward expansion has led the city footprint to envelop virtually the entire western half of the peninsula, as well as several historic towns which were incorporated into the city in the 18th century. The city's landscape is marked by intervening plains and hills, vast swaths of historic parkland, and various segments of beach shores and cliffed outcroppings to the sea. Salonika possesses a voluminous artificial reservoir, in the vicinity of the Imperial Palace, which feeds a system of historic canals that carry water toward districts situated closer to the urban center of the city.
Much of the old city center is densely populated and consists of narrow streets and medieval boulevards interrupted by urban plazas; the outer ring districts often provide much greater swaths of green space. During the city's expansion in the 19th and early 20th century, large tracts of parks, water features, and monumental outdoor spaces were constructed as part of a beautification rivalry with Praetonian city of Kingston and the Cravanian city of Laurana.
The city itself encompasses a total area of 18,000 square kilometres, extending roughly 150 kilometres east-west and 120 kilometers north-south; with a population density of 2,351 persons per square kilometre, and a population exceeding 40 million, it is one of thirteen cities in mainland Willink to be considered a megacity for statistical purposes. Salonika possesses a hot summer Mediterranean climate, with hot, dry summers and mild winters marked by increased rainfall. Salonika has experienced sporadic snowfall, the most recent instances being in 2017. Generally, temperatures rarely fall below below 65.0 °F (18.3 °C), and the summer daily mean temperature charts at 80 °F (26.6 °C).