Qeshm Island 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 07:30 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 Asia/Tehran local. Folk tradition, not a scientific forecast.

Last spring tide on Tue 19 May (range 3.8m). Next neap on Sat 23 May.

Spring tides cluster around new and full moons (biggest swings). Neap tides land on quarter moons (smallest swings). See the spring tide and neap tide glossary entries for the why.

Qeshm is Iran's largest island, sitting in the narrow Clarence Strait that separates it from the Hormozgan mainland. The strait is shallow and tidal — at low water on a spring tide, sections of the mudflat on the eastern side are exposed for hundreds of metres, and traditional wooden dhow builders use the tidal exposure to work on hulls beached against the flats. The island's geography is a study in geological contrast: ancient salt formations, rugged canyon systems, and the most northerly mangrove forest in the world, all within 1,500 square kilometres. The Hara Forest — formally the Hara Biosphere Reserve — covers approximately 400 square kilometres of the island's northern coast and spreads across the channel into the mainland mudflats. The mangroves here are dominated by Avicennia marina (white or grey mangrove), reaching 3 to 4 metres in height. Access is by small motorboat from the village of Qeshm or from Laft on the northwest coast. The tidal regime is central to how the forest functions: at high water, the channels between the mangrove stands are navigable by small boat and the prop roots are submerged; at low water, those same channels drain and the prop roots are exposed, supporting nesting herons, cormorants, and flamingos that feed on the mudflat. The boat operators know the tidal window — plan to enter the forest channels in the two hours before high water and exit on the first of the ebb. The tidal range at Qeshm runs 1.0 to 1.5 metres on spring tides, mixed semidiurnal in character. The pattern means that on some days the two high tides are nearly equal; on others they differ by 0.4 to 0.6 metres. For the Hara Forest visit, the absolute height of high water matters more than the range — a low high tide (neap cycle) may leave some channels too shallow for comfortable navigation. Chakooh Canyon cuts through a salt formation in the central part of the island. Salt is plastic over geological timescales and the canyon walls show contorted layering — salt mixed with coloured mineral sediments, carved by the rare but intense flash floods that the island receives. The canyon is accessible on foot; the entrance is narrow (1 to 2 metres in some sections) and the walls rise 8 to 10 metres. There is no standing water; this is a dry geological feature, not a coastal one, but it is among the island's most visited sites. Namakdan Salt Cave, in the western part of the island, is one of the world's longest salt caves at approximately 6,580 metres of surveyed passage. Salt caves are uncommon globally — salt dissolves rapidly in humid air, so most are found only in hyperarid environments. The Qeshm cave formed in conditions dry enough to preserve the passage. The entrance section is accessible to visitors without specialist equipment; deeper sections require a guide and proper footwear. Qeshm Free Trade Zone covers the eastern part of the island and operates under a separate customs regime from mainland Iran. Duty-free goods — electronics, appliances, clothing — attract significant domestic traffic, particularly from Bandar Abbas. The commercial zone is not of particular interest to international visitors, but it explains the island's well-developed infrastructure: good roads, accommodation, and reliable ferry connections. Dhow building continues at the village of Laft on the northwestern tip of the island. The traditional wooden vessels — lenger — are built using techniques that have changed little in 500 years: adze-shaped planks, hand-finished joinery, no written plans. The master builders carry the design in memory. Visits to the boatyard are possible; the best time to observe hull work is at low tide when beached vessels are accessible. The island's western salt formations are worth a half-day. The salt dome that underlies much of western Qeshm expresses itself in a landscape of eroded salt pillars, coloured mineral seeps, and the distinctive plasticity of salt under erosion — smooth, rounded forms that look nothing like limestone karst. The road from Qeshm town to Laft (the northwestern village) passes through this landscape; the combination of the geological scenery and the mangrove channels of the Hara Reserve visible from the road makes the Laft circuit the most productive half-day on the island. Allow three hours for the round trip if combining a Laft market visit with the mangrove boat entry. Fishing from Qeshm town's harbour and the southern beaches is consistent year-round. Hammour (grouper), snapper, and queenfish are the principal species. The incoming tide in the early morning, when the Clarence Strait current is running flood into the shallow eastern channel, produces the most active feeding conditions. Predictions on this page come from Open-Meteo Marine, a gridded global ocean model. Accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height — model-derived, not from a local gauge. The authoritative source for tidal data in this region is the Ports and Maritime Organization of Iran (PMO).