Bay Inútil depth map

Bay: average depth about 157 m, deepest 568 m (GEBCO_2026 grid).

Tap or scroll to load the interactive map

Sea level todayDrag the slider to lower the sea and see the land that would appear.

Sea level in metres below today’s. A simple bathtub model: it lowers the sea everywhere by the same amount and does not simulate how the water would really drain.

Key

Sea depth

  • Deeper than 6,000 m
  • 4,000 to 6,000 m
  • 2,000 to 4,000 m
  • 1,000 to 2,000 m
  • 200 to 1,000 m
  • Shallower than 200 m (the continental shelf)

Land height

  • Land up to 500 m
  • 500 to 2,000 m
  • Above 2,000 m

Drain the oceans

  • Seabed exposed when the sea is lowered A dashed white line marks today’s coast.

How to read the map. Darker blue is deeper water. Tap anywhere to see how deep the sea is there, or how high the land is, and the nearest named undersea feature. Depths come from the GEBCO_2026 grid, which in most of the deep ocean is predicted from satellite measurements of the sea surface rather than surveyed by ship, and the map’s tiles are coarser than the grid, so narrow trenches read shallower on the map than their true depth. Not for navigation.

Bay Inútil at a glance

  • 157 maverage depth
  • 127 mmedian depth
  • 568 mmaximum depth
  • 3,790 km²water area

Bay Inútil is a bay. Inside its outline the GEBCO grid has about 3,790 km² of water, with an average depth of about 157 m (the middle value is 127 m) and a maximum of 568 m, found at 54.06° S, 70.22° W.

Open the map at the deepest cell and tap to read the depth.

How deep is each part of the Bay Inútil?

The bar splits the Bay Inútil's water by depth. Each colour is a depth band, and the shares add up to 100%.

  • 0 to 200 m: 63.8%
  • 200 to 1,000 m: 36.3%
  • 1,000 to 4,000 m: 0%
  • 4,000 to 6,000 m: 0%
  • below 6,000 m: 0%

Named features near the deepest point: Hero Fracture Zone (863 km), Phoenix Ridge (891 km), Shackleton Fracture Zone (902 km), Monte Cjavals (1,121 km).

The Bay Inútil if sea level dropped

The slider on the map lowers the sea in steps. This table shows how much of the Bay Inútil's water would be land at each step.

Sea level lowered byBecomes landShare of its water
10 m168 km²4.4%
20 m333 km²8.8%
50 m1,191 km²31.4%
80 m1,496 km²39.5%
120 m1,835 km²48.4%
200 m2,416 km²63.7%
500 m3,728 km²98.4%
1,000 m3,790 km²100%
2,000 m3,790 km²100%
3,000 m3,790 km²100%
4,000 m3,790 km²100%
6,000 m3,790 km²100%

A simple bathtub model: it lowers the sea everywhere by the same amount and does not simulate how water would really drain.

Nearby seas

Nearest by the centre of each outline. All oceans and seas

Frequently asked questions

How deep is the Bay Inútil?

On average about 157 m in the GEBCO grid (the middle value is 127 m). The deepest cell inside its outline is 568 m, at 54.06° S, 70.22° W.

How big is the Bay Inútil?

About 3,790 km² of water inside its Natural Earth outline, counted from the grid cells that are below sea level.

How much of the Bay Inútil would be land if sea level dropped?

With the sea 10 m lower, about 168 km² (4.4%) of its water would be land. At 6,000 m lower, 100% would be. This is a simple bathtub model that lowers the sea evenly everywhere.

Data: depths from the GEBCO_2026 grid, statistics worked out inside the Natural Earth outline of the bay. See data sources and licences. The GEBCO Grid should NOT be used for navigation or for any other purpose involving safety at sea.

All oceans and seas · Undersea features · Drain the oceans

Embed this map

Copy this code into your web page. It is free to use. Please keep the link under the map, as it is how people find where the map comes from.