Zierikzee (Zeeuws: Zurrikzeê) is a city in the municipality of Schouwen-Duiveland in the Dutch province of Zeeland. The city has 11,460 inhabitants (January 1, 2020) and is the capital and largest town of the municipality.
Zierikzee, a protected townscape since 1971, one of the protected town and village views in Zeeland, and is known as a monument city. For a relatively small city, Zierikzee has a large number of monuments, 568.
The Sint-Lievensmonstertoren is the most eye-catching monument in
Zierikzee. With its 62 meters it is the tallest tower in the city.
The tower is also popularly called the Fat Tower. This tower
resembles the Sint-Romboutstoren in Mechelen like two drops of
water.
Also worth seeing are the:
Nobel Gate
Noordhavenpoort
Zuidhavenpoort, with the flood monument Tested
but not broken (1970) by Ad Braat
Windmill De Hoop,
The Den
Haas windmill
new church
The Zierikzee Town Hall, from the
16th century. It was thoroughly renovated in 1772-1779. Today, the
Zierikzee Town Hall Museum is located here.
House De Haan, also
sometimes called Templar House, is a merchant's house from the 14th
century. It is one of the oldest preserved buildings in the
Netherlands.
The Gravensteen, from the 16th century
There are
several large patrician houses around the Oude Haven.
City gates
and city wall
There was a city wall in Zierikzee. The current
Nobelpoort, Noordhavenpoort and Zuidhavenpoort are the only
remaining city gates of Zierikzee, the Westpoort, Zuidwellepoort and
the Hoofdpoort were demolished in the 19th century. What is now
understood by the Slingerbos was the actual foundation of the city
wall, the canals of the city wall have been spared. However, there
are still remnants of the city wall.
The name of Zierikzee can be traced back to a composition of the personal name 'Siric' and the Old Dutch 'aa' or 'aha' which means 'water'. Siric or Sigiric is an old Germanic name, and a compound of the two parts 'sigi' (victory or victory) and 'ric' (rich, many). When the genitive -s in 'Sirics Ee' ("the Ee of Siric") was no longer recognized as such, the last part was interpreted as 'See' instead of Ee (or Aa), leading to the current spelling with - z.
Founding Legends and Early History
The origins of Zierikzee are
shrouded in legend and archaeological debate. A popular but dubious tale
claims the town was founded in 849 by Ziringus (or Zierik), son of the
Hunnic king Lalalo from Pannonia (an ancient Roman province encompassing
modern-day Hungary and Romania). According to this story, Zierik, an
explorer, settled near a creek called the Ee, giving the town its
name—Zierikzee. Lalalo is fancifully credited with inventing salt and
show business, adding to the legend's vaudeville-like flair. However,
archaeologists dismiss this as folklore, estimating the settlement dates
no earlier than the 11th century. More reliably, the area formed from
sea-deposited clay, creating high creek ridges and low-lying lakes. By
the 9th or 10th century, a small hamlet of fishermen and sheep farmers
emerged along a creek, prone to frequent floods that necessitated early
earthen dams.
The name Zierikzee first appears as "Siricasha" in a
1156 document. A tide mill is referenced as early as 1220, marking one
of the oldest watermill mentions in the Netherlands. The town received
city rights in 1248 from Count William II of Holland, spurring rapid
growth. By the late Middle Ages, it had become a strategic hub in
Zeeland, boasting more large ships than any town in Holland. Religious
orders arrived in the 13th century during the mendicant movement,
establishing monasteries occupied by begging friars like the Friars
Minor and Preachers. Around 1400, a defensive castle called Gravenhof
was built for aristocracy and protection, though it was demolished 300
years later due to neglect.
Key early landmarks include the
Zuidhavenpoort (South Harbor Gate), dating to the 13th century as the
oldest gate, and the Noordhavenpoort (North Harbor Gate) from the
13th-14th centuries, both guarding the harbor.
Medieval Period
and Economic Rise
During the medieval era, Zierikzee's economy
thrived on maritime trade. Ships sailed to distant ports like Archangel,
Saint Petersburg, Malaga, Genoa, Africa's west coast, and the Caribbean,
including involvement in the slave trade. The town joined the Hanseatic
League, enhancing its prominence. In 1304, a combined French-Dutch fleet
defeated a Flemish force in the naval Battle of Zierikzee, a pivotal
conflict affirming its strategic importance.
Construction of the
Sint-Lievensmonstertoren (Monster Tower or Fat Tower) began in 1454 in
Brabantine Gothic style, intended to reach 204 meters but halted at 62
meters in 1530 due to financial woes. The adjacent church, originally
wooden from around 950 and elevated to a Holy Roman Basilica in the 12th
century, received relics of Saint Livinus in 1463. It was rebuilt in
neo-Gothic style after fires but burned again in 1832, leading to a
neoclassical reconstruction as the Nieuwe Kerk.
The Gravensteen
prison, built in 1524 with 242,000 bricks, is Zeeland's oldest and
features carved inmate names and an escape legend.
Conflicts and
Wars
Zierikzee's location made it a frequent battleground. In the
Eighty Years' War (1568-1648) for Dutch independence, Dutch Watergeuzen
(Calvinist guerrillas) seized it from Spanish forces in 1572. The Siege
of Zierikzee (1575-1576) saw Spanish troops under Cristóbal de Mondragón
besiege the city for nine months, failing initial assaults but occupying
it after a sea battle. A mutiny over unpaid wages led to looting and
abandonment, allowing Protestant forces to regain control. This
contributed to the formation of the Dutch Republic in 1579.
The 1780s
Fourth Anglo-Dutch War brought English occupation of parts of Zeeland.
Post-Napoleon's 1813 retreat, 200 English redcoats ravaged the town.
French occupation in the early 19th century supported local Patriots but
strained finances.
During World War I, on April 30, 1917, a lost
British Royal Naval Air Service pilot mistakenly bombed Zierikzee
(neutral Dutch territory), dropping eight bombs that damaged houses and
killed a family of three, confusing it for German-held Zeebrugge.
Britain apologized and compensated.
In World War II,
Schouwen-Duiveland remained under German occupation until May 1945. In
December 1944, Germans attempted to deport men aged 17-40 for labor;
resistance stole records, but ten were executed.
Economic
Development and Decline
Zierikzee's golden age was tied to fishing
and trade. In the 17th century, it was a prominent fishing port with
warehouses like the Pakhuis (1656) and market halls (1651). However,
decline set in by the mid-18th century due to silting waterways and
wars. Population dropped from 10,000 to 6,000 in the 1780s. By the 19th
century, it was a "forgotten city" with failed commercial fishing
attempts. Industries included breweries, tanneries, and mills, but
prosperity waned. In 1735, a slave fund was created to ransom captured
sailors from Barbary pirates, lasting into the 19th century and later
funding nurseries after the 1953 flood.
A Jewish community formed in
the late 18th century, establishing a synagogue and cemetery by 1825.
Many were traders; the market day shifted to Thursday for Shabbat. Most
emigrated by the early 20th century, and remaining Jews were deported
during WWII.
Post-1953, the economy shifted to tourism, water sports,
and yachting.
Disasters and Resilience
Zierikzee has faced
repeated calamities. Fires devastated the town six times between the
15th and 19th centuries: half burned in 1414, the center in 1458, and
lightning destroyed the main church in 1466. A 17th-18th century plague
killed over three-quarters of livestock.
The North Sea flood of 1953,
a one-in-a-thousand-year event, breached dykes, killing 1,836 in the
Netherlands (including 24 in Zierikzee), flooding streets for months,
and requiring evacuations. Aid from towns like Hatfield, England,
fostered twinning.
On June 27, 2022, an F1-F2 tornado struck, killing
one, injuring nine, and damaging 300 properties.
Topography and Terrain
Zierikzee's topography is predominantly
flat and low-lying, typical of the Dutch delta landscape. The average
elevation is around 0 meters (sea level), with some areas dipping
slightly below to -1 meter, while minor variations reach up to 6 meters
in built-up zones. The island of Schouwen-Duiveland as a whole is mostly
below sea level, except for coastal dunes on the western tip that rise
to about 42 meters, providing natural barriers against the North Sea.
These dunes, such as those in the Boswachterij Westerschouwen forest
(Zeeland's largest), transition into polders—reclaimed lowlands
protected by dikes—in the interior where Zierikzee is situated.
The
terrain around Zierikzee features a mix of urban medieval structures
interspersed with agricultural polders, creeks, and meadows. The city's
core is compact, with a protected townscape including over 568
monuments, set on slightly elevated ground relative to surrounding
wetlands. To the west and north, the landscape opens into coastal plains
and nature reserves with sandy beaches, while the east and south are
dominated by estuarine mudflats and salt marshes. Hiking trails, like
the 5.7-mile Zierikzee-Schouwen-Duiveland loop, reveal gentle elevation
gains of about 47 meters, highlighting the flat, walkable nature of the
area. Overall, the topography is shaped by glacial deposits, river
sediments, and human land reclamation, resulting in a uniform, fertile
plain ideal for agriculture but vulnerable to water intrusion.
Hydrography and Water Features
Water is central to Zierikzee's
geography, reflecting Zeeland's deltaic origins. The city is connected
to the Oosterschelde (Eastern Scheldt) estuary via a canal that runs
through its harbor, primarily used today for recreational boating and
tourism. The Oosterschelde itself is a vast tidal estuary bordering
Schouwen-Duiveland to the south and east, covering about 370 km² and
serving as the Netherlands' largest national park. This body of water
features extensive mudflats, shoals (like the Roggenplaat), and salt
meadows, with tidal ranges historically around 3.4 meters, now moderated
to 3.25 meters by the Oosterscheldekering storm surge barrier—a key
component of the Delta Works completed in the 1980s.
To the north,
the Grevelingenmeer, a former estuary turned saltwater lake by the
Brouwersdam (built in 1972), offers calm waters for water sports.
Numerous creeks and ditches crisscross the island, including the
Krekengebied Ouwerkerk near Zierikzee, which are remnants of historical
floods and now form wetland habitats. The island's hydrography has been
dramatically altered by human intervention: originally four separate
islands (Schouwen, Duiveland, Dreischor, and Bommenede), they merged
through silting and dike construction, with the final link between
Schouwen and Duiveland in 1610. Connections to neighboring islands
include the Zeeland Bridge (Europe's longest at 5 km) over the
Oosterschelde and dams linking to Goeree-Overflakkee. These features
make Zierikzee a hub for maritime activities, though they also
underscore the ongoing need for flood defenses.
Climate
Zierikzee experiences a temperate maritime climate (Köppen
classification: Cfb), influenced by its proximity to the North Sea and
Oosterschelde, which moderate temperatures and bring consistent
moisture. Summers are mild and pleasant, with average highs around 18°C
(64°F) in July and August, rarely exceeding 25°C (77°F). Winters are
cool and overcast, with averages around 4.5°C (40°F) in January and
February, and occasional frosts but seldom severe cold. The annual
temperature range is about 13.6°C (24.5°F), with a yearly mean of 11.1°C
(51.9°F).
Precipitation is significant and evenly distributed,
totaling 813 mm (32 inches) annually, with no true dry season—the driest
month (April) still sees 50 mm (2 inches). Rainfall occurs on 8–10 days
per month, peaking in summer and autumn due to convective showers and
Atlantic fronts. Humidity is high, ranging from 74% in June to 84% in
November, contributing to a damp, foggy atmosphere in winter. Sunshine
averages 2,436 hours per year, with July offering up to 10 hours daily
and January only about 3.3 hours. Winds are often brisk from the
southwest, and the region is prone to storms, as evidenced by a 2022
tornado that struck Zierikzee, causing casualties.
Environmental
Features and Ecosystems
The geography around Zierikzee supports rich
biodiversity, bolstered by its estuarine position. The Oosterschelde
National Park, adjacent to the city, is a Ramsar wetland site hosting
seals, birds (e.g., avocets, curlews, plovers), and unique marine life
in its tidal zones. However, the Delta Works have altered ecosystems by
reducing tidal flows, necessitating interventions like sand
replenishment on shoals to combat erosion.
Schouwen-Duiveland boasts
over a dozen nature reserves managed by Staatsbosbeheer, many near
Zierikzee, such as the Krekengebied Ouwerkerk (creek area with
birdwatching trails), Plan Tureluur (a redshank breeding site), and
Meeuwenduinen dunes. These areas feature salt marshes, forests, and
polders that support migratory birds and endemic plants. The
Grevelingenmeer to the north adds diving and sailing opportunities in a
controlled saline environment. Environmental challenges include
sea-level rise and salinity intrusion, mitigated by ongoing dike
maintenance.
Historical Geographical Changes
Zierikzee's
geography has evolved through natural and anthropogenic forces. Founded
around 976 on the island of Schouwen, it prospered from its watery
surroundings, with islands merging via silting and dikes. The 1953 North
Sea flood devastated the area, inundating polders, damaging Zierikzee,
and prompting the Delta Works, which reshaped coastlines and created
barriers like the Brouwersdam. This transformed salty estuaries into
freshwater or controlled saline zones, enhancing flood protection but
altering habitats. Municipal mergers in 1997 formalized
Schouwen-Duiveland, consolidating the island's geography. These changes
highlight the dynamic balance between human ingenuity and natural forces
in this vulnerable delta landscape.