Ancient Corinth

37°54′19″N 22°52′49″E / 37.9053455°N 22.8801924°E / 37.9053455; 22.8801924

Corinth (/ˈkɒrɪnθ/ KORR-inth; Ancient Greek: Κόρινθος Kórinthos; Doric Greek: Ϙόρινθος Qórinthos; Latin: Corinthus) was a city-state (polis) on the Isthmus of Corinth, the narrow stretch of land that joins the Peloponnese peninsula to the mainland of Greece, roughly halfway between Athens and Sparta. The modern city of Corinth is located approximately 5 kilometres (3.1 mi) northeast of the ancient ruins. Since 1896, systematic archaeological investigations of the Corinth Excavations by the American School of Classical Studies at Athens have revealed large parts of the ancient city, and recent excavations conducted by the Greek Ministry of Culture have brought to light important new facets of antiquity.

For Christians, Corinth is well known from the two letters from Paul the Apostle in the New Testament, the First Epistle to the Corinthians and the Second Epistle to the Corinthians. Corinth is also mentioned in the Acts of the Apostles as part of Paul the Apostle's missionary travels. In addition, the second book of Pausanias' Description of Greece is devoted to Corinth.

Ancient Corinth was one of the largest and most important cities of Greece, with a population of 90,000 in 400 BC. The Romans demolished Corinth in 146 BC, built a new city in its place in 44 BC, and later made it the provincial capital of Greece.

The geophysical situation at Corinth is in many ways ideal for human habitation. The city is situated on two large geomorphic terraces, at the southern edge of which is located both arable plains and a number of natural springs. These abundant sources of fresh water are further supplemented by seasonal rivers descending from the Ayios Vasilios valley and Mount Ziria. Natural drainage patterns in the region have formed a broad valley, enabling the movement of wheeled and pedestrian traffic between the terraces.

The geological makeup of Corinth provided the basic materials for the city's construction. The oolitic limestone of the region’s marine sand bars was used extensively in both domestic and public architecture, and local Corinthian stone was quarried extensively and traded widely across the Aegean. Supplementing this resource are abundant local deposits of calcareous marl, which served as a rich source for the production of ceramics. These marls, when dug, dried, powdered, heated, and mixed with water, made for a highly workable clay, excellent for the production of lightweight ceramic vessels. Pottery created from Corinthian limestone concrete was exported widely in various periods.

Neolithic pottery suggests that the site of Corinth was occupied from at least as early as 6500 BC, and continually occupied into the Early Bronze Age, when, it has been suggested, the settlement acted as a centre of trade. However, there is a huge drop in ceramic remains during the Early Helladic II phase and only sparse ceramic remains in the EHIII^{[clarification needed]} and MH^{[clarification needed]} phases; thus, it appears that the area was very sparsely inhabited in the period immediately before the Mycenaean period. There was a settlement on the coast near Lechaion which traded across the Corinthian Gulf; the site of Corinth itself was likely not heavily occupied again until around 900 BC, when it is believed that the Dorians settled there.

According to Corinthian myth as reported by Pausanias, the city was founded by Corinthos, a descendant of the god Zeus. However, other myths hold that it was founded by the goddess Ephyra, a daughter of the Titan Oceanus, thus the ancient name of the city (also Ephyra).