(Click on the names of cities and landmarks for more information.)
This interactive map of the Netherlands provides an overview of the Dutch Golden Age, highlighting the cultural, economic, and historical aspects of various cities, towns, and rivers. By clicking on a location, you can learn more about its significance during this period. Explore the rich history of the Netherlands in the 17th century at your own pace.
The Netherlands today has a temperate maritime climate, with mild summers, cool winters, and high humidity throughout the year. Rainfall is evenly distributed across the seasons, and the proximity to the North Sea moderates temperatures, preventing extreme heat or cold. However, during the so called Little Ice Age, which lasted from the fourteenth to the mid-nineteenth century, the Netherlands experienced significantly colder winters, with frequent freezing of canals and rivers. This period also brought more severe storms and flooding, challenging the Dutch with increased risks of water-related disasters. The cooler climate shortened growing seasons, impacting agriculture and contributing to economic difficulties. Despite these challenges, the Dutch adapted to the harsh conditions, which influenced various aspects of their culture and daily life.
The original geography of the Netherlands is deeply influenced by its location at the confluence of three major European rivers—the Rhine, the Meuse, and the Scheldt—flowing into the North Sea. This unique setting has shaped a landscape predominantly made up of a low-lying delta, characterized by extensive flat terrain where a significant portion lies below sea level. Coastal dunes and beaches line the western and northern borders, serving as natural barriers against sea encroachment and protecting the inland areas from flooding.
The interior is marked by vast peatlands1 and wetlands, formed from millennia of accumulated plant material in waterlogged conditions. These areas were initially unsuitable for agriculture but have been transformed through extensive drainage to create arable land. The network of rivers not only deposited rich sediments that enriched the soil but also supported diverse ecosystems and provided natural routes for transportation and trade, integral to the region’s economic development.
A notable feature was the Zuiderzee, a large shallow bay in the north, which was a hub of maritime activities until its reclamation in the 20th century through the construction of the Afsluitdijk. This transformed it into the IJsselmeer, altering both the geography and hydrology of the area dramatically.
"The Dutch population grew continuously during the sixteenth and the first half of the seventeenth century; by 1650 it had doubled in size. Over the one hundred years that followed, the size of the population stagnated and in many regions it actually decreased. Taking the province of Holland as an example, the urban population increased more than the rural population. At the beginning of the sixteenth century, half of the provincial population lived in cities; by 1622, this had reached fifty-nine per cent; and in 1795, sixty-three per cent. By the middle of the seventeenth century, when the population growth was less rapid, Holland was the most densely populated and most urbanized province in western Europe. The port cities of Rotterdam and Amsterdam grew more quickly—from 50,000 inhabitants (1600) to 200,000 (1650)—than the industrial cities of Haarlem, Delft, and Gouda. An exception to this was Leiden, where textiles were produced and where the population increased suddenly, by about 70,000 inhabitants, in the middle of the seventeenth century. While most of the port cities also continued to grow in the second half of the century, there was a marked reduction in the population of the industrial centres, which clearly paralleled the industrial recession."2
Over the centuries, the Dutch have masterfully engineered their landscape to manage the challenges posed by water, reclaiming land from the sea since the medieval period. By the 17th century, they had perfected the technique of creating polders (reclaimed land surrounded by dikes). During this period, an estimated 25% to 30% of territory below sea level. The majority of these areas were in the western provinces, such as Holland and Zeeland, where much of the land had been reclaimed from the sea through a system of dikes and drainage.
The construction of dikes, canals, and sophisticated drainage systems has not only reclaimed land from the sea but also safeguarded it. These human modifications have been crucial in shaping the Netherlands' current geography, turning challenges into opportunities and making the nation a leader in water management and land reclamation. This intricate relationship between natural elements and human ingenuity continues to define the Dutch approach to environmental and engineering challenges, embedding a deep cultural emphasis on planning and cooperation within Dutch society.
In the 1500s, much of the Netherlands was composed of marshes, peat bogs, and tidal areas,3 with the land constantly at risk of flooding due to the low elevation. The region was characterized by its vast wetlands, rivers, and lakes. Early Dutch communities lived on terpen (mounds),4 which were artificial mounds built to protect against rising water levels.
Land reclamation continued. and between 1590 and 1665 almost 100,000 hectares were reclaimed from the wetland areas of Holland, Zeeland and Friesland. However, land reclamation decreased significantly after the middle of the seventeenth century because the price of agricultural products began to fall, making land reclamation far less profitable in the second part of the century.5
During the seventeenth century, the Dutch excelled in the creation of polders,6 areas of land reclaimed from the sea or wetlands that were enclosed by dikes and then drained using an elaborate system of canals and windmills. These windmills became iconic symbols of Dutch ingenuity, primarily used to pump water out of the low areas, allowing for both agricultural development and urban expansion in regions that were once submerged or swampy.
The construction of extensive dijkenstelsel (dike systems) as also critical during this period. These dijken (dikes) were essential for protecting the reclaimed lands from the sea and preventing the catastrophic floods that could occur during storm surges. Alongside the dikes, the Dutch engineered a kanalenstelsel (network of canals) that facilitated not only transportation and communication across the burgeoning nation but also played a crucial role in controlling water levels and distributing freshwater. The Dutch engineered a series of sluizen (locks; in Dutch singular sluis), dikes, and drained landscapes to manage water levels and prevent flooding, which in turn facilitated the smooth operation of the trekschuit (tow bardge) routes (trevaarten in Dutch). Tow boats were pulled along canals by horses walking on trekvaarten, were an efficient and popular transport solution, pre-dating the railway era and reflecting the Dutch mastery in both hydraulic engineering and transportation. This innovation was closely tied to their sophisticated water control systems, crucial in a country where much of the land is below sea level.
Sluizen (sluices),7 or water-regulating gates, were another important invention of the time, used to manage the flow and level of water in the canals and rivers. This regulation was vital to maintaining the integrity of the polders and ensuring that these areas remained dry and habitable.
The complete study of Vermeer’s materials, artistry and painting techniques
Jonathan Janson
(painter & founder of Essential Vermeer.com)