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Results for Póros
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| Poros Πόρος |
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|---|---|
Poros Town |
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| Geography | |
| Coordinates: | Coordinates: |
| Island Chain: | Saronic Islands |
| Area:[1] | km² ( sq.mi.) |
| Highest Mountain: | Vigla ( m ( ft)) |
| Government | |
| Periphery: | Attica |
| Prefecture: | Piraeus |
| Capital: | Poros (city) |
| Statistics | |
| Population: | (as of 2001) |
| Density: | /km² ( /sq.mi.) |
| Postal Code: | 180 20 |
| Area Code: | 22980 |
| License Code: | YI, YK, YM, YN |
| Website | |
| www.poros.com.gr | |
Poros (Greek: Πόρος) is a small Greek island-pair
in the southern part of the Saronic Gulf, at a distance about 48 km (32 miles) south from
Piraeus and separated from the Peloponnese by a 200-metre
wide sea channel. Its surface is about
Poros consists of two islands: Sphairia or Sferia, the southern part, which is of volcanic origin, where today's city is located, and Kalaureia, also Kalavria or Calauria (meaning 'gentle breeze'), the northern and largest part. A bridge connects the two islands over a narrow isthmus. The Municipality of Poros also includes a part of the mainland, Kyaní Aktí (pop. 231), at the easternmost point of the Peloponnese Peninsula, between the island of Poros and the island of Hydra and next to the municipalities of Troizina and Ermioni. map The total land area of the municipality is 49.582 km², and the total population is 4,348 persons.
Poros is an island with rich vegetation. Much of the northern and far eastern/western sides of the island are bushy, whereas large areas of old pine forest are found in the south and center of the island. It has a good road network and adequate tourist infrastructure, which makes it a popular resort for short holidays. Though possessing no airport, it is easily accessible from Athens via ferry or hydrofoil or from the adjacent mainland at Galatas.
The landscape is very hilly and mountainous. The highest peak is the Vigla (358 m) in the west-central part. Following the island's topography and geology, small creeks and seasonal streams flow through steep valleys of the southern and northeastern part. The western and northern part of the island feature smooth hills and shallow valleys. Sandy beaches are restricted to the southern shore of the island, except for a bay in the northern part called Vayionia.
The geology of the island comprises Mesozoic to Cenozoic sedimentary rocks (limestone, and Flysch-type sandstone) and ophiolites, as well as Neogene volcanic rocks on Sferia. The island is tectonically dissected and part of a Tertiary tectonic mélange. There are karstic sinkholes in the island's central limestone massif, and limestone caves with stalactites. Visible marine fossils are mainly found in the limestone, no occurrences of precious stones or ore deposits are known.
Recent studies suggest that Poros has been inhabited since the Bronze Age. Graves on the island have been dated to the Mycenaean period, and manmade structures have existed on it since at least 1000 BCE.
The ancient polis of Kalaureia was home to an asylum dedicated to Poseidon, the ruins of which are still accessible on a hilltop close to the town. This asylum may have been linked to the sanctuaries at Geraistos and Tainaros. Ancient historians claimed that Poros was home to an Amphictyony in the Archaic period, a league of the poleis Poros, Athens, Prassiai, Aegina, Epidaurus, Hermione, Troizene, Nauplion and Orchomenos. However, there is no evidence for this, and modern scholars believe the Amphictyony may have been a Hellenistic invention. An enormous feast was found dating to the Hellenistic period in the ruins of the Kalaureia asylum, along with a plaque celebrating the "revival" of the Kalaureian League.
In Byzantine times, Poros and other islands were often raided by pirates. During the Ottoman occupation Poros remained independent, and helped neighbouring islands after the start of the Greek War of Independence.
Poros was ravaged by a forest fire that overran the southwestern portion of the larger island of Kalavria on June 26, 2007; it also destroyed several houses and businesses. The view from the Saronic Gulf resembled a disaster and it could be seen plainly from the mainland. The cause of the fire was the enormous heatwave that plagued Southeastern Europe at that time, causing temperatures to soar above 45 degrees. It took firefighters on the ground and water-bombing aircraft several hours to control the blaze and the horrific fire was extinguished only in the latter part of the day.
| Year | Communal population | Change | Overall Island population | Change |
|---|---|---|---|---|
| 1981 | 3,929 | - | - | - |
| 1991 | 3,273 | -656/-16.7% | 3,570 | - |
| 2001 | - | - | 4,348 | +778/+21.79% |
| The Saronic Islands |
|---|
| Aegina • Hydra • Poros • Spetses • Angistri • Salamina • Psyttaleia • Leros Salaminos • Revythoussa • Moni Aiginas • Dokos • Spetsopoula • Romvi • Plateia • Psili • Agios Georgios • Patroklou • Fleves • Agios Georgios Salaminos • Ypsili Diaporion • Ypsili Argolidos • Agios Thomas Diaporion • Agios Ioannis Diaporion • Plateia Aiginis • Laousses Islets • Kyra Aiginis • Trikeri Hydras • Alexandros Hydras • Stavronisi Hydras • Velopoula • Falkonera |
| Municipalities and Communities of the Piraeus Prefecture | |
|---|---|
| Municipalities | Aegina • Agios Ioannis Rentis • Ampelakia • Drapetsona • Hydra • Keratsini • Korydallos • Kythira • Methana • Nikaia • Perama • Piraeus • Poros • Salamis • Spetses • Troizina |
| Communities | Agkistri • Antikythera |
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![]() | Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/ Read more | |
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