Chiloé 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 18:00 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/Santiago local. Folk tradition, not a scientific forecast.

Next spring tide on Tue 12 May (range 1.1m). Next neap on Thu 07 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.

Chiloé is the second-largest island in South America after Tierra del Fuego, approximately 180 km long and 50 km wide, separated from the Chilean mainland by the Chacao Channel in the north and the Boca del Guafo strait in the south. The island faces the open Pacific on its western coast and the sheltered inner channels on the eastern coast; the tidal environments of the two coasts are markedly different. Castro, the island's largest city, sits at the inner end of a long fjord-like inlet on the eastern coast. The tidal regime at Chiloé is macrotidal semidiurnal. Spring range at the Chacao Channel narrows is approximately 5.0–6.0 m above Chart Datum; inside Castro Fjord the range is slightly lower as the fjord attenuates the tidal prism. Two nearly equal highs and two nearly equal lows occur each day. The Chacao Channel — the 2.5 km strait between Chiloé's northern tip and the mainland at Pargua — concentrates the tidal exchange between the open Pacific and the inner canal system; spring currents through the narrows run 3–5 knots, making it one of the most significant tidal current hazards on the Chilean coast. Chiloé's architecture is inseparable from the tidal regime. The palafito stilt houses of Castro and Dalcahue are built directly over the tidal flat: the wooden structures sit on piles above the high-water line, with boat access at all tide states beneath the floor level. The low-water tidal flat below the palafitos dries completely at spring low tide, exposing the mud and gravel floor beneath the structures. At high water the flat is covered and the boats float alongside. This tidal-adaptive architecture evolved over several centuries and is one of the defining cultural expressions of island Chile. The Castro palafitos, photographed extensively, are on the inner harbour; the full low-tide mud exposure beneath them is most visible on spring tides. The western coast of Chiloé — accessible by local roads from Ancud and Castro — faces the open Pacific and receives full South Pacific swell. Beaches at Cucao and Tepuhueico inside the Chiloé National Park are remote, exposed, and backed by dense valdivian temperate rainforest. Surf at Cucao is consistent and relatively powerful; the beach is accessible to 4WD in winter and by regular road in summer. The western coast tidal flats at low water expose extensive intertidal zones used for harvesting mariscos — particularly the piure (Pyura chilensis) and lapa (Patella species) limpets that are endemic to the Chilean southern coast. Ferry crossings from Pargua to Chonchi or La Arena serve the Chacao Channel; the Naviera Austral and Trans Chiloé ferries time their crossings to avoid the peak spring current through the narrows, departing within two hours of slack water. SHOA publishes specific Chacao Channel current tables in addition to tide height tables. Open-Meteo Marine provides predictions here: accuracy ±45 min / ±0.2–0.3 m. The Chiloé Archipelago's wooden churches — 16 of which are UNESCO World Heritage listed — were built from local alerce (Fitzroya cupressoides) and cypress wood by Jesuit missionaries during the 17th–18th centuries. The churches are clustered in villages connected by boat access; the Dalcahue, Achao, and Castro churches are the most visited. The building form — a distinct 'Chilote' style of wooden nave facade — was adapted for the high-rainfall, high-tidal-range environment of the islands, and many churches sit on slightly elevated ground to avoid the occasional spring-high-tide flooding of the coastal village sites. The Chiloé Archipelago's weather is the defining factor in coastal access planning beyond tidal timing. The island averages 1,800–2,500 mm of rain per year, with the western coast receiving more than the sheltered eastern coast. Fog is frequent year-round; the visibility in the Chacao Channel can drop to under 200 m in persistent fog, and the ferries operate on radar in these conditions. The combination of macrotidal range, strong tidal current, fog, and significant rainfall makes Chiloé one of the more challenging coastal environments for independent navigation in South America.