Full Day Tours

Argolis Tour

The Corinth Canal is a canal that connects the Gulf of Corinth with the Saronic Gulf in the Aegean Sea. It cuts through the narrow Isthmus of Corinth and separates the Peloponnese from the Greek mainland, thus effectively making the former peninsula an island. The builders dug the canal through the Isthmus at sea level; no locks are employed. It is 6.4 kilometres (4 mi) in length and only 21.4 metres (70 ft) wide at its base, making it impassable for most modern ships. It now has little economic importance.

Mycenae is an archaeological site in Greece, located about 90 kilometres (56 miles) southwest of Athens, in the north-eastern Peloponnese. Argos is 11 kilometres (7 miles) to the south; Corinth, 48 kilometres (30 miles) to the north. From the hill on which the palace was located, one can see across the Argolid to the Saronic Gulf.

Nafplio is a seaport town in the Peloponnese in Greece that has expanded up the hillsides near the north end of the Argolic Gulf. The town was an important seaport held under a succession of royal houses in the Middle Ages as part of the lordship of Argos and Nauplia, held initially by the de la Roche following the Fourth Crusade before coming under the Republic of Venice and, lastly, the Ottoman Empire. The town was the capital of the First Hellenic Republic and of the Kingdom of Greece, from the start of the Greek Revolution in 1821 until 1834. Nafplio is now the capital of the regional unit of Argolis.

Acronauplia is the oldest part of the city though a modern hotel has been built on it. Until the thirteenth century, it was a town on its own. The arrival of the Venetians and the Franks transformed it into part of the town fortifications. Other fortifications of the city include the Palamidi and Bourtzi, which is located in the middle of the harbour.

Nafplion maintains a traditional architectural style with many traditional-style colourful buildings and houses, partly influenced by the Venetians, because of the domination of 1338-1540. Also, modern-era neoclassical buildings are also preserved, while the building of the National Bank of Greece is an example of Mycenaean Revival architecture.

Epidaurus was a small city in ancient Greece, on the Argolid Peninsula at the Saronic Gulf. Two modern towns bear the name Epidavros (Modern Greek: Επίδαυρος): Palaia Epidavros and Nea Epidavros. Since 2010 they belong to the new municipality of Epidaurus, part of the regional unit of Argolis. The seat of the municipality is the town Asklipieio.

Tour Duration: 10 hours.

* An official guide is available at extra charge. Please contact us for details.

Delphi Tour

Delphi is both an archaeological site and a modern town in Greece on the south-western spur of Mount Parnassus in the valley of Phocis. In myths dating to the classical period of Ancient Greece (510-323 BC), the site of Delphi was believed to be determined by Zeus when he sought to find the centre of his "Grandmother Earth". He sent two eagles flying from the eastern and western extremities, and the path of the eagles crossed over Delphi where the omphalos, or navel of Gaia was found.

Earlier myths include traditions that Pythia, or the Delphic oracle, already was the site of an important oracle in the pre-classical Greek world (as early as 1400 BC) and, rededicated from about 800 BCE, when it served as the major site during classical times for the worship of the god Apollo. Apollo was said to have slain Python, "a dragon" who lived there and protected the navel of the Earth. "Python" is claimed by some to be the original name of the site in recognition of Python which Apollo defeated. The Homeric Hymn to Delphic Apollo recalled that the ancient name of this site had been Krisa. Others relate that it was named Pytho and that Pythia, the priestess serving as the oracle, was chosen from their ranks by a group of priestesses who officiated at the temple.

Tour Duration: 10 hours.

* An official guide is available at extra charge. Please contact us for details.

Olympia Tour

Olympia, a sanctuary of ancient Greece in Elis on the Peloponnese peninsula, is known for having been the site of the Olympic Games in classical times. The Olympic Games were held every four years throughout Classical Antiquity, from the 8th century BC to the 4th century AD. The first Olympic Games were in honor of Zeus.

The sanctuary, known as the Altis, consists of an unordered arrangement of various buildings. Enclosed within the temenos are the Temple of Hera, the Temple of Zeus, the Pelopion, and the area of the altar, where the sacrifices were made.

To the north of the sanctuary can be found the Prytaneion and the Philippeion, as well as the array of treasuries representing the various city-states. The Metroon lies to the south of these treasuries, with the Echo Stoa to the east. The hippodrome and later stadium were located east of the Echo Stoa. To the south of the sanctuary is the South Stoa and the Bouleuterion, whereas the Palaestra, the workshop of Pheidias, the Gymnasion, and the Leonidaion lie to the west.

Tour Duration: 12 hours.

* An official guide is available at extra charge. Please contact us for details.

Meteora Tour

The Metéora is one of the largest and most important complexes of Greek Orthodox monasteries in Greece, second only to Mount Athos. The six monasteries are built on natural sandstone rock pillars, at the northwestern edge of the Plain of Thessaly near the Pineios river and Pindus Mountains, in central Greece. The nearest town is Kalambaka. The Metéora is included on the UNESCO World Heritage List.

Studies suggest that the pinnacles were formed about 60 million years ago during the Paleogene Period. Weathering and earthquakes then shaped them into their present shape.

Beside the Pindos Mountains, at the western region of the Thessaly, in the middle of northern Greece, these sandstone rocks rise from the ground. The rocks are composed of a mixture of sandstone and conglomerate. They were formed about 60 million years ago. A series of earth movements pushed the seabed upwards, creating a high plateau and causing many fault lines to appear in the thick layer of sandstone.

Continuous weathering by water, wind and extremes of temperature turned them into huge rock pillars, marked by horizontal lines which geologists maintain were made by the waters of a prehistoric sea. Greek historian Herodotus wrote in the 5th century BC that local people believed the plain of Thessaly had once been a sea. If this was accurate, there was most probably an inundation at the end of the last Ice Age, around 8000 BC.

Tour Duration: 12 hours.

* An official guide is available at extra charge. Please contact us for details.