Pella

Tabaqat Fahl — ancient Pella — occupies a ten-hectare mound beside a perennial spring in the north Jordan Valley, 130 kilometres north of Amman. Settled since approximately 6000 BC, it ranks among the longest continuously occupied sites in the Near East, layering Neolithic, Bronze Age, Iron Age, Hellenistic, Roman, Byzantine and Early Islamic culture into one extraordinary stratigraphic record. University of Sydney excavations since the 1980s have uncovered the largest Canaanite Migdol temple of its type in the Levant, originally built around 1650 BC.

As a Decapolis member after 63 BC, Pella gained Roman civic infrastructure: a 2nd-century hillside odeon, baths, a nymphaeum and colonnaded streets. The Byzantine era brought the city to its greatest extent — three major churches, mosaic floors and a bishop's palace. A devastating earthquake in 749 AD ended urban life, preserving ruins beneath silt. Today, column drums, temple foundations and Islamic structures are explored with the help of one of Jordan's most comprehensive on-site interpretation centres.

Pella lies roughly 130 kilometres north of Amman and one hour southwest of Irbid, with 27 kilometres to the Sea of Galilee. Spring is the most rewarding season, when wildflowers surround the ancient spring. The site pairs naturally with Umm Qais and Ajloun for a northern Jordan circuit.