The Pagasetic Gulf (Greek: Παγασητικός Κόλπος, romanized: Pagasitikós Kólpos) is a rounded gulf (max. depth 102 metres) in the Magnesia regional unit (east central Greece) that is formed by the Mount Pelion peninsula. It is connected with the Euboic Sea. The passage into the Euboic Sea is narrow and is about 4 km.
Its main port is Volos.
Mount Othrys (Greek: όρος Όθρυς – oros Othrys, also Όθρη – Othri) is a mountain range of central Greece, in the northeastern part of Phthiotis and southern part of Magnesia. Its highest summit, Gerakovouni, situated on the border of Phthiotis and Magnesia, is 1,726 m (5,663 ft) above sea level. The population density in the mountains is low: there are a few small villages, including Anavra in the northwest, Kokkotoi in the northeast, Palaiokerasia in the south and Neraida in the southwest. The length from west to east is about 35 km (22 mi) and the width from north to south is about 25 km (16 mi). The Pagasetic Gulf lies to the northeast, and the Malian Gulf lies to the south. The summit Gerakovouni lies 19 km (12 mi) south of Almyros, 27 km (17 mi) northeast of Lamia and 44 km (27 mi) southwest of Volos. The peaks of the range are above the tree line. The main mineral constituent of the rock is ophiolite.
A Natura 2000 protected area has been defined over much, but not all, of the range according to the Birds Directive. Of interest to the government is the protection of the raptors and the prevention of clear-cutting and other settlement measures that would destroy their traditional habitat. The area, named Oros Othrys, Vouna Gkouras kai Farangi Palaio Kerasias, ID GR1430006, includes the eastern range, a spur to the south to cover Palaiokerasia Gorge, and a spur to the north to cover Gkouras Hill.
Pelion or Pelium (Modern Greek: Πήλιο, Pílio; Ancient Greek/Katharevousa: Πήλιον, Pēlion) is a mountain at the southeastern part of Thessaly in northern Greece, forming a hook-like peninsula between the Pagasetic Gulf and the Aegean Sea. Its highest summit, Pourianos Stavros, is 1,624 metres (5,328 ft) amsl. The Greek National Road 38 (GR-38) runs through the southern portion of the peninsula and GR-38A runs through the middle.
Achaea Phthiotis (Ancient Greek: Ἀχαΐα Φθιῶτις, lit. 'Achaea of Phthia') or simply Phthiotis (Φθιῶτις) was a historical region of Thessaly, in ancient Greece.
It lay in southeastern Thessaly, between Mount Othrys and the northern shore of the Pagasetic Gulf. Inhabited by perioikoi, it was originally formally not a part of Thessaly proper but a Thessalian dependency, and had a seat of its own in the Delphic Amphictyony. From 363 BC it came under Boeotian control, but split away during the Lamian War. In the 3rd century BC it became a member of the Aetolian League, until declared free and autonomous by the Roman Republic in 196 BC, following the Second Macedonian War, and re-incorporated into Thessaly.
The Arta–Volos line (Greek: Γραμμή Άρτας - Βόλου) or Ambracian–Pagasetic line (Greek: Γραμμή Αμβρακικού - Παγασητικού) was the land border of the Kingdom of Greece and the Ottoman Empire between 1832 and the Annexation of Thessaly in 1881. It was named after the two principal cities in proximity of the border on the Ottoman side, Arta and Volos, and the Ambracian Gulf and the Pagasetic Gulf between which it extended.
The border had been proposed by the Great Powers in the London Protocol of 1829 as the northern boundary of an autonomous Greek state under Ottoman suzerainty, but when the full independence of Greece was agreed on in the London Protocol of 1830, the borders of the new state were reduced to the Aspropotamos–Spercheios line, only to be again expanded in the London Conference of 1832, which was confirmed by the Treaty of Constantinople (1832).
Halos (Ancient Greek: Ἅλος), Latinised as Halus, was a town and polis in the region of Achaea Phthiotis in ancient Thessaly, on the west side of the Pagasetic Gulf.
Coracae or Korakai (Ancient Greek: Κορακαί) was a town and polis (city-state) on the Pagasetic Gulf in Magnesia in ancient Thessaly. It is mentioned in the Periplus of Pseudo-Scylax as between Methone and Spalauthra. Earlier writers tried to equate the town with Korope, but that has not been generally accepted.
Coracae is noted in two inscriptions from Delphi of the fourth century BCE. It has been suggested that the town's location could have been on a hill called Nevestiki, near the current village of Lekonas, where remains of a fortification have been found, but that location has been suggested by others as the site of Methone.
Methone (Ancient Greek: Μεθώνη, Methṓnē) was an ancient Greek city-state on the Pagasetic Gulf of Magnesia in ancient Thessaly. The town is mentioned by Homer in the Catalogue of Ships in the Iliad as belonging to Philoctetes. It is also mentioned in the Periplus of Pseudo-Scylax as a city in Magnesia, together with Iolcus, Coracae, Spalauthra and Olizon.
Some accept that the town's location is on a hill called Nevestiki (39°19′54″N 23°03′10″E / 39.3316°N 23.0527°E), near the current village of Ano Lechonia, where remains of a fortification have been found, but that location has been suggested by others as the site of Coracae.