Sukeldumissügavust

Sukeldumissügavust is a term used in the field of archaeology and maritime history to describe the depth at which a shipwreck is submerged in water. This depth is crucial for understanding the preservation state of the wreck and the potential for further research. The term is derived from the Dutch word "sukkel," which means to sink or submerge, and "diepte," meaning depth.

The sukeldepth of a shipwreck can vary greatly depending on several factors, including the age of the wreck, the water depth at the site, and the rate of sedimentation. In shallow waters, shipwrecks may be partially or completely exposed at low tide, while in deeper waters, they can be submerged to great depths. For example, the wreck of the Vasa, a 17th-century ship, lies at a depth of about 35 meters in Stockholm's archipelago, while the Titanic, which sank in 1912, is located at a depth of over 3,800 meters in the North Atlantic Ocean.

The sukeldepth of a shipwreck is typically measured using sonar or other underwater surveying techniques. This information is important for archaeologists and historians, as it helps them determine the best methods for studying and preserving the wreck. In some cases, shipwrecks that are too deeply submerged may not be accessible for further research, while those that are partially exposed may be at risk of damage from weathering or human activity.

Understanding the sukeldepth of a shipwreck is also important for maritime archaeologists who are interested in the environmental conditions that existed at the time of the wreck. By analyzing the sukeldepth, they can gain insights into the water quality, currents, and other factors that may have contributed to the sinking of the ship. This information can provide valuable context for understanding the historical and cultural significance of the wreck.