The Kathammer or Katwouder Mill

The Kathammer or Katwoudermolen is a striking feature in the open landscape near Volendam. This national monument, dating from 1896, not only grinds using wind power, but also houses an electric pumping station. The mill operates regularly and can only be visited by groups by appointment.

The Kathammer or Katwoudermolen. Photo: Harry Schuitemaker

Katwoude Polder

The Kathammer or Katwoudermolen drains the eastern part of the Katwoude polder, which covers approximately 520 hectares. The name of the mill is derived from aspects of the landscape: KAT means bumpy peatland, and HAM stands for uitham in the sea (Zuiderzee).

From the polder (1.95 m below sea level), the water is metre at least 1.7 metre and then discharged into the Markermeer via a drainage sluice. The polder consists of raised bogs. Over the centuries, the soil slowly subsided due to the compaction and oxidation of the peat. This made it increasingly difficult to discharge the water naturally (from high to low) into the Zuiderzee at low tide. In 1650, a paddle wheel mill was built to pump the water upwards, the Hogendijkse Molen. In 1663, the Katwoude polder was cut through by the tow canal between Edam and Amsterdam. After this, the mill only drained the eastern part of the polder. For the western part of the polder, the Katwoude-Lagendijk polder, a new paddle wheel mill was built on the tow canal in 1665.

Example of a screw mill from around 1840. Collection: North Holland Archives

Fire

On December 5, 1895, the Hogendijkse Mill burned down after being struck by lightning. The mill was inhabited by the miller and his family. Unfortunately, his daughter did not survive the strike and the miller was injured. Because a steam pumping station was too expensive at the time, a new mill was built in 1896. It was erected on the eight old masonry piers (wall dams) of its predecessor, which had survived the fire. The mill was equipped with a steel screw pump, which was very modern for its time. Due to the fire hazard, the miller no longer lived in the mill, but in the newly built miller's house next door, which was still standing.

The Kathammer around 1910 with wooden lightning conductor on the roof, viewed from the east. Collection: Cultural Heritage Agency of the Netherlands, Amersfoort / Document number 237.482

In 1911, a centrifugal pump powered by an oil engine was installed in the mill. The sails were no longer needed. Later, around 1930, the hull was sawn off to the attic.

The dismantled windmill prior to demolition of the cap, circa 1917. A lightning rod on the cap. In the foreground, a locomotive with tipping wagons. This industrial railway was constructed to reinforce the sea dike, which had been severely damaged during the storm surge of 1916. Collection: Vereniging De Hollandsche Molen (Dutch Mill Association), document identification: 1926-8-6 THE CITY OF AMSTERDAM
Mill hull in 1987. Viewed from the west. Collection: Cultural Heritage Agency of the Netherlands, Amersfoort / Document number 223.538

Wind and electric propulsion

During the1980s, the tide turned for the dismantled mill. The Katwoude polder had since been absorbed into the large Waterlanden Water Board, which began a major restoration in 1987. Due to its special historical and scenic value, it was decided to rebuild the mill. The octagonal tower was extended to its original height and fitted with a new cap and sails. As a result, the mill is once again able to drain the polder using wind power.

In addition, the mill has since housed an electric screw pump. This is located under the wooden floor. The pump switches on automatically when the water level in the polder is too high. It is not possible to grind using both wind power and the electric motor at the same time.

The screw, with a diameter of 1.85 m, is visible in the mill through a glass panel. There are flood gates at the top of the screw. These gates prevent high water from flowing back into the polder.

Drainage mill via screw pump. Collection: HHNK

Mill biotope

The mill biotope is the area surrounding the mill. The biotope of the Kathammer or Katwoudermolen mill is very good. There are no tall trees or buildings in the vicinity, allowing the mill to turn effectively in the wind.

Extra

The preservation of the mill is made possible in part by the Cultural Heritage Agency of the Netherlands and the province of North Holland.

The Kathammer

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