Saba Bank in the Caribbean Netherlands is the largest submarine atoll in the Atlantic Ocean and has some of the richest diversity of marine life in the Caribbean Sea. In 2010, it was designated as Saba Bank National Park, one of the national parks of the Netherlands, and was officially recognized as such in 2012.
The national park was established to provide protection to the biodiversity of the bank. The marine life there consists of humpback whales, sea turtles, over 200 species of fish, and many kinds of sea birds. The bank is highly valued to other close reefs, acting as a source of coral larvae and fish that then spread throughout nearby coral reefs in the region. In the past, the bank has been damaged by anchors from ships and tankers while loading oil, and began to deteriorate in color and size.[1]
The Saba Bank, several kilometers to the south of the island of Saba, covers more than 2400km2 and is therefore the largest protected nature area in the Netherlands. The bank lies completely underwater and is important from both a biological and economic perspective.
The northeastern side of Saba Bank lies about 4.3km (02.7miles) southwest of the island of Saba. It is raised about above the general depths of the surrounding sea floor. With a length of 60kmto65kmkm (40milesto40mileskm) and a width of 30kmto40kmkm (20milesto30mileskm), the atoll's total surface area is approximately 2200km2, and measures from deep, 1600km2 of which is shallower than .
From northeast, the bank extends about 55km (34miles) southwest, with a least reported depth of located about 15km (09miles), southwest of Mount Scenery. A depth of lies about 16km (10miles) south of the island. The eastern side of the bank is fringed with a ridge of living coral, sand and rock, nearly 48km (30miles) in length. The depths over the ridge range from 11to. Westward of this ridge, except for a few 16.5m (54.1feet) and 18.3m (60feet) deep coral patches near the south side of the bank and a 16.4m (53.8feet) deep patch near the west end of the bank, the bottom is clear white coral sand with depths from 21.9to, gradually increasing towards the edge of the bank, but ending abruptly in depths of . In depths of under, the bottom can be distinctly seen.
In 2019, the Royal Netherlands Institute for Sea Research (NIOZ) and Wageningen Marine Research organized an expedition to the Saba Bank, close to the Dutch island of Saba. Expert researchers gathered data to acquire more knowledge about sinkholes. In 2018, the same group of researchers discovered more than 20 enormous holes ranging from 10to in depth and with diameters varying between 70and. The floor of the Saba Bank consists of a limestone deposition 1to thick. When the bank lay above water during the ice ages and the sea level was lower than it is now, flowing freshwater dissolved the limestone and created large holes. This first led to the formation of caves, which subsequently collapsed. Interestingly enough, these sinkholes that developed on land were subsequently submerged after the last ice age (20,000 years ago), when the sea level rose again. Later, researchers discovered that the sinkhole seemed to seep gas. Researchers then obtained coordinates of a purported hot-spring in one of the sinkholes that could have possibly seeped methane.
About one-third of Saba Bank lies within the Saba territorial waters, a 120NaN0[2] zone. Around it is an Exclusive Economic Zone of the Netherlands of 200nmi outside the coastal baseline, which replaced the Economic Fisheries Zone established before the dissolution of the Netherlands Antilles.