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Oesterdam

The Oesterdam is the longest dam of the Delta Works, but was originally not part of the Delta Plan.

The Oesterdam separates the salty Eastern Scheldt (the Tholense Gat) from the fresh Bergsche Diep and connects Tholen and Zuid-Beveland. The Oesterdam includes the Bergse Diepsluis and is located next to the two Kreekkraksluizen.

Origin

The Oesterdam was not originally included in the Delta Plan. This is because the plan was to completely close off the Eastern Scheldt. This would eliminate the ebb and flow, turning the Eastern Scheldt into fresh water, which could be used for drinking water and agriculture. Additionally, shipping on the busy route from the Port of Rotterdam to Antwerp would no longer be affected by tides. However, closing off the Eastern Scheldt would come at the cost of nature.

It was then decided to preserve the nature in the Eastern Scheldt, while simultaneously retaining as many of the benefits of the planned freshwater reservoir as possible. To achieve this, the 'compartmentalisation works' were constructed: the Oesterdam, the Philipsdam, the Markiezaatskade, and the Bathse Spuisluis. The water basins behind these Delta Works were 'compartmentalised', meaning they were separated from the Eastern Scheldt and its tides.

These Delta Works were not built to protect against the sea, but to regulate water management in the hinterland. The Oesterdam, along with the Philipsdam, reduced the surface area of the Eastern Scheldt, thereby increasing the tidal effect and preserving the natural area. To allow for large-scale shipping, two sluices were constructed next to the dam: the Kreekkraksluizen. A sluice for recreational boats and small fishing vessels heading to Bergen op Zoom was also built within the Oesterdam itself.

The lower costs were mainly due to the use of sand to construct the Oesterdam, instead of large concrete caissons. A sand dredger pumped sand from the seabed further along and sprayed it continuously until the dam formed. This was quite a task because, as the remaining gap to be closed became smaller, the current became stronger. Therefore, precise measurements were made to determine how much sand was flowing away and how much needed to be sprayed back in. This knowledge would later be applied during the construction of the Philipsdam.

The short section towards Tholen was the last to be completed. By this point, the current was so strong that it was impossible to spray the sand against it. To make it possible, the Eastern Scheldt Storm Surge Barrier had to be temporarily closed, but it wasn't yet operational enough to allow this. In 1986, once the Eastern Scheldt Barrier was fully functional, the Oesterdam could be completed.

Space was made on the Speelmansplaten near the Bergse Diepsluis for vacation villas, events, and water sports. The N659, which runs over the Oesterdam, was opened in 1989.

Around 2010, the Oesterdam was no longer strong enough to withstand the waves it had to endure. However, instead of reinforcing the dam with the usual riprap, a large amount of sand was placed on the western side of the dam, not far from Zuid-Beveland. The sand breaks the power of the waves and simultaneously formed a new recreational beach.

The Markiezaatskade consists of two parts: a northern section between the Molenplaat and Noordland, and a western section from the Molenplaat towards the Kreekkraksluizen. Construction began in late 1980 with the spraying of sand on the northern part. Before starting on the western section, a stretch of about 800 meters was constructed in the middle as a permeable dike, which would gradually silt up over time. This gap was designed to allow a gradual transition from saltwater to freshwater in the new Markiezaatsmeer.

Work on the western section began from the south, starting at the Kreekkraksluizen, but a dike breach in March 1982 caused a setback. Part of the dike was destroyed and had to be repaired before work could continue. On March 30, 1983, the Markiezaatskade was completed.

The Markiezaatsmeer now lies in the area once described as "the drowned land of the Markiezaat of Bergen op Zoom." Today, it is a nature reserve.

The locks originally used the same system as the Philipsdam to prevent the mixing of fresh and saltwater. When the lock opened and a ship passed through, the waters would mix. However, fresh water is lighter than salt water, so once the lock was closed, the saltwater was pumped out from the bottom, or the fresh water from the top, depending on the direction of the vessel. After this process, the lock could open again, and the ship would sail away in a uniform type of water.

Since 1997, the Kreekraksluizen have operated in a different way. They now function as a pump station that, at certain times, pumps fresh water into the Antwerp Canal area (the southern side of the Kreekraksluizen). This has artificially shifted the salt-freshwater boundary further south. This method uses less energy, is more cost-effective to maintain, and reduces the waiting time for ships in the lock.

Address

Weg van de Buitenlandse Pers 5, Ouwerkerk

Opening hours

Open daily from 10:00 to 17:00. Between November 1 and March 31, the museum and bistro Vijfde Caisson are closed on Mondays.
On 23 and 30 December: open // On December 25 and January 1: closed