Landsat 8 image of Zeebrugge

Sediment-laden waters off the Belgian port of Zeebrugge. A team of researches found that two World War II-era shipwrecks in this area leave sediment plumes during ebb and flood tides, opening the door for a new shipwreck detection method. This natural color Landsat OLI image was acquired on Sept. 11, 2015.

Feb 23, 2016 • Nearshore shipwrecks can leave telltale sediment plumes at the sea’s surface that reveal their location. Using Landsat 8 data, researchers have detected plumes extending as far as 4 kilometers (~2.5 miles) downstream from shallow shipwreck sites. This discovery demonstrates that Landsat and Landsat-like satellites can be used to locate the watery graves of coastal shipwrecks.

The planet’s oceans are littered with an estimated 3 million shipwrecks; and most maritime mishaps take place close to shore where hazards to navigation—like rocks, reefs, other submerged objects, and vessel congestion—are abundant.

While there is a romantic association of shipwrecks and buried treasure, it is desirable to know where they are located for many other practical reasons. The ships may be of historical significance, or, if the hard substrate of the ship has created a reef, of ecological significance. Modern-era shipwrecks are commonly sources of pollution, leaking onboard fuel and corroded heavy metals. And nearshore shipwrecks can be navigational hazards themselves.

A quarter of all shipwrecks may rest in the North Atlantic; within the North Sea, especially in the narrow southern end where the English coast is merely 100 miles from the shores of Belgium and the Netherlands, World War II-era shipwrecks are plentiful. Here, mines, submarines, submersibles, and warships targeted cargo ships sailing between Allied countries and Dutch and Belgian ports. The potential negative environmental impacts of these modern-era shipwrecks are substantial enough that the Council of Europe’s Parliamentary Assembly has recommended they be mapped and monitored.

MBES map of shipwreck elevations

Elevation models of the SS Sansip (A, left) and the SS Samvurn (B, right) created using a multibeam echosounder. Both of these ships left sediment plumes detectable by Landsat 8 during ebb and flood tides. Image credit: Baeye et al.

Airborne lidar can be used to detect shipwrecks close to shore and multibeam echosounders and other sound-based methods can be used anywhere deep enough for a survey vessel to sail; the former requires clear water, however, and both are too prohibitively costly to conduct exhaustive coastal surveys.

A new study published in the Journal of Archaeological Science by authors Matthias Baeye and Michael Fettweis, from the Royal Belgian Institute of Natural Sciences; Rory Quinn from Ulster University in Northern Ireland; and Samuel Deleu from Flemish Hydrography, Agency for Maritime and Coastal Services; is about to change things: the authors have found a way to use freely available Landsat data to detect ships in sediment-laden coastal waters.

Their study was conducted in a coastal area off of the Belgium port of Zeebrugge (the port city for Bruges). The coast is strewn with shipwrecks, often has sediment-laden waters and, most essentially, has a detailed multibeam echosounder survey of the wreck sites (previously conducted by the Flemish government).

launching of a US Liberty ship

The launching of a WWII Liberty Ship in 1943 (SS George Washington Carver). By 1944, wartime production of these "ugly duckling" cargo steamers took an average of 42 days. The SS Sansip was a US Liberty ship and the SS Samvurn had similar dimensions. Photo by E.F. Joseph; available from The New York Public Library, Photographs and Prints Division.

The researchers started with the known location of four fully submerged shipwrecks in their study site: The SS Sansip, which the authors explain was a 135 m (443 foot) US Liberty ship that sank after striking a mine in December 1944; the SS Samvurn, a similar ship that met the same fate the very next month; as well as the SS Nippon a ship that sank after a maritime collision in 1938; and the SS Neutron a small 51 m (167 foot) steel cargo vessel that fell victim to an uncharted navigation hazard, presumed to be the SS Sansip.

Using 21 Landsat 8 images and tidal models, the researchers mapped sediment plumes extending from the wreck locations. They found that the two ships with substantial portions of their structure unburied created sediment plumes that could be traced downstream during ebb and flood tides.

The authors postulate that the exposed structure of these ships created scour pits that then fill with fine sediments (sand, clay, organic matter, etc.) during slack tides (the period of relatively still currents between ebb and flood tides). These scour pits then serve as sediment repositories from which sediments are re-suspended during flood and ebb tides. When these sediments reach the surface, they create their telltale plumes.

This means uncharted shipwrecks could be found using this method—i.e., mapping sediment plumes during various tidal stages and then following the plumes upstream to their point of origin.

This study looked at shipwrecks in waters as deep as 15 m (50 feet); depth is an essential consideration as the re-suspended sediment plumes must reach the surface to be detected by optical satellites like Landsat.

Given that coastal waters are typically shallow, often sediment-laden, and where most shipwrecks occur, this new shipwreck detection method should prove a major discovery for marine archaeologists

Note: The authors used atmospherically corrected Landsat 8 reflectance data, specifically, that of OLI bands 4 (red) and 5 (infrared) to chart sediment plumes.
Science brief by Laura E.P. Rocchio


M. Baeye, R. Quinn, S. Deleu, M. Fettweis (2016). "Detection of shipwrecks in ocean colour satellite imagery.", Journal of Archaeological Science, pp. 1–6 DOI:

Further Reading

+ Satellites Could Help Discover Modern and Ancient Shipwrecks, Scientific American

+ Detecting shipwrecks from space, Ulster University