Butrint, Sarandë District tide times

Predictions: Open-Meteo Marine (MeteoFrance SMOC, 0.08° grid) — heights relative to MSL (not chart datum / LAT). Model-derived.

Model-derived from a global ocean grid. Useful indication; expect about ±45 minutes on average vs. a local harmonic gauge, individual stations vary widely. See /methodology for per-region detail. Not for navigation.

Conditions as of 00:00 local time. Refreshes daily.

Predictions: Open-Meteo Marine (MeteoFrance SMOC, 0.08° grid) — heights relative to MSL (not chart datum / LAT). Model-derived. · Not for navigation.

The angler tradition for major/minor fishing windows: major ≈3-hour windows around moon transit and opposition; minor ≈2-hour windows around moonrise and moonset. Times are Europe/Tirane local. Folk tradition, not a scientific forecast.

Butrint — ancient Buthrotum — is one of the most consequential archaeological sites in the eastern Mediterranean, a wooded peninsula where Greek, Roman, Byzantine, Venetian, and Ottoman layers are not merely adjacent but physically stacked: a Roman theatre built over Greek foundations, a Venetian tower incorporating Byzantine stonework, a baptistery floor whose mosaics were laid in the 6th century and remain in place. The site became a UNESCO World Heritage Site in 1992. What distinguishes Butrint from other comparable sites is the ecological context: the peninsula is surrounded by water on three sides, hemmed by Butrint Lake to the north and the Vivari Channel to the south and east, and that water is not decorative — it is a functioning tidal system. The Vivari Channel is the connection between Butrint Lake and the Ionian Sea. The channel is roughly 50 m wide and several hundred metres long, running southwest from the lake to the sea near the village of Ksamil. Tidal exchange through this bottleneck drives the ecology of the entire lake. On the flood tide, Ionian seawater pushes through the channel into the lake, raising salinity in the lower water column. On the ebb, fresher water drains back toward the sea. The result is a brackish gradient maintained by the tidal cycle and reinforced by seasonal freshwater input from the Bistrica river, which enters the lake system from the north. The tidal regime at Butrint is the standard Ionian microtidal pattern: mean range 0.2-0.4 m, mixed semi-diurnal. Two unequal high waters and two unequal low waters per day. That small range, pushed through the 50 m throat of the Vivari Channel, generates a tidal current of up to 1.5 knots on spring tides — perceptible to anyone crossing by the cable ferry, and significant to anything swimming through the channel. The cable ferry, which connects the mainland road to the archaeological peninsula, crosses this current continuously throughout the day. The cable keeps the ferry on line; passengers who've not expected the current sometimes brace against the railing when the flow is running hard on a spring ebb. The eel fishery of Butrint Lake is the most ecologically distinctive consequence of this tidal connection. European eels (Anguilla anguilla) spend their juvenile and adult lives in brackish and freshwater systems before undertaking a transoceanic spawning migration to the Sargasso Sea. The Vivari Channel is one of the migratory corridors for eels moving between the lake and the open sea. Adult silver eels migrate outward through the channel on autumn nights, entering the Ionian and eventually reaching the Atlantic. Glass eels and elvers enter the lake from the sea in early spring, riding the flood current into the freshwater-brackish transition zone. This eel migration has supported a local fishery for centuries; traditional trap fishing in the channel dates to the Venetian period and records from that era document the channel's commercial importance. Water level in Butrint Lake fluctuates with the tidal cycle by roughly 0.3-0.5 m when seasonal freshwater input from the Bistrica is low. In winter and early spring, river input can dominate the lake level and suppress tidal variation; in summer, the Bistrica flow drops and the lake level tracks the Ionian tide more clearly. The consequence for the archaeology is visible: the Lion Gate, the Roman theatre, and the baptistery all sit within 5 m of the lake's current edge. During higher lake-level periods in winter, the lower path between the Lion Gate and the theatre is sometimes flooded. The proximity of major Roman and Byzantine structures to a fluctuating water body is not incidental — the original settlement chose the peninsula precisely because the water-controlled access was defensible. The Lion Gate itself — a basalt lintel carved with two heraldic lions above the entrance passage — dates to the 4th century BCE and marks the entrance to the ancient city from the lake shore side. The Roman theatre behind it is one of the best-preserved in the Balkans: tiered seating for roughly 1,500, orchestra circle intact, stage building partially reconstructed. The baptistery, built in the 5th-6th century CE over the ruins of a Roman public building, has a floor mosaic 14 m in diameter — geometric and animal motifs — that is covered with sand outside peak visiting hours to protect it from foot traffic and weather. All three monuments can be reached on foot from the cable ferry landing in under 10 minutes. For photographers, the view from the Venetian tower over the lake and channel captures the geographical logic of Butrint in a single frame: the wooded peninsula, the dark water of the lake, the narrow channel opening to a lighter Ionian horizon, and — in the right light — the silhouette of Ksamil's islets beyond. The best light is early morning, when the site opens and tour groups from Sarandë and Ksamil have not yet arrived. The cable ferry begins operating at 08:00. For kayakers and paddlers, the Vivari Channel presents an unusual opportunity: a tidal channel with measurable current in an otherwise microtidal sea. Paddling the channel on a flood tide with the current behind you from the sea side takes about 15 minutes and requires coordinating with ferry crossings. The lake beyond is calm and largely unexplored by kayak; circumnavigating the Butrint peninsula by water is possible but requires launching from outside the park boundary. Tide data for Butrint, Sarandë District comes from the Open-Meteo Marine API, a gridded model product. Timing accuracy is ±45 minutes, height accuracy ±0.3 m — usable for trip planning, not for navigation.