The Phlegrean Fields is a vast active volcanic area west of Naples, containing one of the world's largest calderas. The area features fumaroles, hot springs, and ancient ruins including the Roman amphitheater at Pozzuoli, offering a unique geological experience.
The Phlegrean Fields (Campi Flegrei, meaning 'burning fields' in ancient Greek) constitute one of the world's largest and most scientifically significant active volcanic zones, covering approximately 150 square kilometres west of Naples in the Campania region of Italy. Rather than a single cone volcano, Campi Flegrei is a caldera supervolcano whose last major eruption in 1538 created Monte Nuovo—a new volcanic hill 123 metres high—in just two days. The entire area undergoes a geological process called bradyseism (slow vertical ground movement), which has caused the ancient Roman town of Puteoli (modern Pozzuoli) to rise and fall by several metres over the centuries, a process still actively measured today. The main visitor attractions are concentrated around Pozzuoli and the coastal area. The Flavian Amphitheatre (Anfiteatro Flavio) in Pozzuoli, the third largest amphitheatre in the Roman world with a capacity of 40,000 spectators, has some of the best-preserved underground machinery (hypogea) of any Roman arena. The Solfatara crater, a 770-metre-wide active volcanic depression near Pozzuoli, features steaming fumaroles, boiling mud pools, and sulphurous jets on a compacted white mineral surface—however the Solfatara site has been closed to visitors since a fatal accident in 2017 and access should be verified before any visit. Lake Avernus (Lago d'Averno), once believed by the ancients to be the entrance to the underworld and described as such by Virgil in the Aeneid, is now a tranquil lake within a volcanic crater where walking paths encircle the perimeter. Baia, an underwater archaeological site, contains sunken remains of Roman imperial thermal baths submerged due to bradyseism.
Good to know
- Hours
- 9:00 AM - 5:00 PM (seasonal variation)
- Best time
- morning
- Best for
- nature lovers, adventure, history
Location
Via Anfiteatro 2, 80078 Pozzuoli NA
40.8258, 14.1286 View on map
Highlights
- Explore the Flavian Amphitheatre in Pozzuoli, the Roman world's third-largest arena with intact underground machinery
- Visit Lake Avernus, the crater lake once believed by Virgil and Dante to be the entrance to the underworld
- See the Temple of Serapis (Macellum) in Pozzuoli, whose columns show clear evidence of ancient sea-level changes
- Discover the Roman ruins at Baia, partially underwater due to volcanic bradyseism
- Observe the steaming fumaroles and volcanic landscape of this active caldera zone
Tips for visiting
- Solfatara volcanic crater is a highlight
- The town of Pozzuoli has a great fish market
- Accessible by Naples Metro Line 2
When to visit
Spring and autumn are ideal for exploring the outdoor sites comfortably. Midday visits in summer are uncomfortably hot in the open volcanic landscape. Pozzuoli's fish market is most active in the morning and pairs well with a visit to the amphitheatre.
Accessibility
The Flavian Amphitheatre has partially accessible pathways at ground level but the cavea seating areas involve stairs. The Lake Avernus perimeter path is relatively flat and accessible on foot. The Pozzuoli town centre and waterfront are accessible by Metro and on foot.
Frequently asked questions
Is Campi Flegrei dangerous to visit?
The area is continuously monitored for seismic and volcanic activity by the Vesuvius Observatory and INGV. Alert level notices are issued and visitor access to specific areas may be restricted during periods of elevated activity. Visitors should check current alert levels before travelling to the area.
How is Campi Flegrei reached from Naples?
The area is accessible from Naples by Metro Line 2 to Pozzuoli (approximately 20 minutes from Naples Piazza Garibaldi). From Pozzuoli, local buses serve the main sites. By car, the Tangenziale motorway provides fast access to the Pozzuoli exit.
What is bradyseism and why does it matter at Campi Flegrei?
Bradyseism is the gradual rise and fall of the ground caused by magma and hydrothermal fluid movement beneath the caldera. At Pozzuoli, this process raised the harbour floor by several metres over centuries, submerging Roman port buildings visible underwater. It is ongoing and is one reason the area is intensively monitored.