Salt Cay 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 19:00 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 America/Grand Turk local. Folk tradition, not a scientific forecast.

Next spring tide on Sun 17 May (range 1.0m). Next neap on Fri 15 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.

Salt Cay is the southernmost inhabited island of the Turks and Caicos, 14 km south of Grand Turk across open water. It is the smallest and least visited of the TCI's populated islands — roughly 60 permanent residents, no airport, no ATM, no resort infrastructure — and arguably the most intact example of a Bermudan salt-raking settlement in the Caribbean. The island's economy for two centuries ran on a single product: solar-evaporated salt harvested from the crystallisation ponds that cover a significant fraction of its low-lying interior. Bermudian and British merchants built the white-painted salt-era houses that line the small harbour, and the windmill remnants and salina gates are still standing as functional artefacts rather than museum pieces. The tidal regime at Salt Cay is mixed semidiurnal with a spring range of 0.4–0.6 m above Chart Datum — the same microtidal character as the rest of the Turks Islands. The island's position on the Turks Bank south of the Turks Island Passage means it catches more direct exposure from northeast trade swell than Grand Turk; the south and east coasts take Atlantic fetch in winter cold-front passages. Mean low water springs at Salt Cay drops to approximately 0.0 m Chart Datum, exposing the shallow reef crest on the western shore and rock platform on the north and east sides. The western reef at Salt Cay shares the same geological structure as the Grand Turk wall — the Turks Bank edge drops precipitously on its western face — but receives a fraction of the dive traffic. The wall here begins at 10–12 m and drops beyond safe recreational diving limits within metres. The reef crest on the approach from the western shore sits 0.5–1.0 m below the surface at high spring tide; at low spring water some sections break the surface. The current along the wall mirrors Grand Turk: northward on the flood, southward on the ebb, 0.3–0.5 knots on springs. There are no dive operators permanently based on Salt Cay; dive trips come by arrangement from Grand Turk or from liveaboards transiting the TCI. Whale watching is the primary draw from January through April. Humpback whales use the Turks Island Passage as a northward migration corridor and calving ground, moving through the deep water between Grand Turk and Salt Cay. Salt Cay's position at the southern entrance of the passage gives it excellent access to the whale activity. Boat-based whale watching departs from the small harbour on the northwest side of the island; flat-calm days in February and March can produce mother-calf pairs resting at the surface within 200 m of the boat. The whales are not affected by tidal phase in any practical sense — their movement is governed by calving cycle and migration timing, not water level. However, sea conditions for the boat trip depend on wind more than tide; the harbour is sheltered enough to launch a small vessel in up to 15 knots of northeast trade wind. The salt ponds in the island's interior are still connected to the sea by tidal gates and channels cut by the original salina engineers. On spring tides the gates allow a partial tidal exchange with the outer reef — seawater flows in on the flood, concentrating as it evaporates over the following weeks. The ponds produce a colour gradient visible from the air: grey-blue near the inlet gates, deepening to pink and white at the highest-salinity crystallisation pans further inland. The pink colour comes from halophilic bacteria, the same organisms that colour salt pans from Bonaire to the Camargue. At low spring tide the channels between ponds and sea are at their shallowest — accessible by wading for anyone exploring the salina infrastructure on foot. For anglers, the shallow reef platform on the east and north coasts produces bonefish and permit on the flooding tide. The flat is less developed and less visited than equivalent bonefishing grounds at Provo; anglers who reach Salt Cay by the twice-weekly ferry from Grand Turk or by private charter often find the flat unfished. The ebb tide off the west coast concentrates snapper and grouper at the reef crest edge. Families visiting Salt Cay on day trips from Grand Turk find a single small beach on the northwest side of the island, in the shelter of the harbour. The beach is narrow at high water and widens 10–15 m at low spring tide. The water is shallow — 0.5–1.0 m depth at 30 m from shore at mid-tide — and calm, protected by the outer reef. All tide predictions for Salt Cay come from the Open-Meteo Marine gridded model. Timing accuracy is ±45 minutes; height accuracy is ±0.3 m above Chart Datum.