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Depth under cursor—
0 mreef · shelf · slope · trench7,208 m
Viewpoint7.30°N · 134.40°EPalau · Western Pacific
Depth · 0 to 7,208 m
Reef flat0–5 m
Reef slope5–30
Mesophotic30–150
Shelf break150–200
Slope200–1,800
Abyssal1,800–5,000
Palau Trench5,000 m +
Maritime zones
Territorial sea12 nm
Contiguous24 nm
EEZ200 nm
Depth bands are ecological, not evenly spaced — they mark the
reef-building limit, the mesophotic floor and the shelf break.
Vertical scale is non-linear: the top 60 m is
shown at full scale and everything below is compressed, or a 7 km trench would flatten
the reef to a sheet.Seafloor provenance: 78% of this frame comes from
GMRT's high-resolution multibeam soundings; the rest is interpolated from a coarser
background grid and is measurably smoother. The closer views sit largely on that fill
— Rock Islands 18% surveyed, Ulong Channel 2% — so fine structure there is
the model, not a survey. Depths are relative to approximately mean sea level with no
tidal reduction, so the waterline on a shallow flat is datum-dependent.
Reef structuretap a species ↗
Geomorphic zone
Terrestrial reef flat
Reef crest
Outer reef flat
Inner reef flat
Back reef slope
Sheltered reef slope
Reef slope
Plateau
Shallow lagoon
Deep lagoon
Bottom cover
Coral / algae
Seagrass
Rock
Rubble
Sand
Microalgal mats
Allen Coral Atlas, 10 m satellite-derived classification.
Mapped to roughly 30 m depth — below that the class is unmapped, not absent.
Live · reef condition
Heat stress—
Sea surface temp—
Bleaching alert—
Surface current—
Fishing effort—
NOAA Coral Reef Watch · Global Fishing Watch
Current is the ~25 km geostrophic field from altimetry — the
regional set. It does not resolve tidal flow through a reef channel, which is the flow a
diver feels and the flow that times a spawning aggregation.