Willeskop

Polsbroekerdam is a hamlet in the Dutch province of Utrecht. It is a part of the municipality of Lopik, and is located about 10 km southeast of Gouda. The village of Polsbroek is located west of the hamlet.

Snelrewaard is a hamlet in the Dutch province of Utrecht. It is a part of the municipality of Oudewater, and lies about 2 km east of the city of Oudewater. A small part of the hamlet is in Montfoort.Snelrewaard was a separate municipality from 1817 to 1989, when it was merged with Oudewater.It was first mentioned around 1307 as Snoyelrewaert, and means "land near water belonging to Snel (polder)". Snelrewaard has place name signs. In 1840, it was home to 140 people.

Lange Linschoten is a hamlet in the Dutch province of Utrecht. It is a part of the municipality of Oudewater, and lies about 2 km northeast of the city of Oudewater. The hamlet was first mentioned in 1555 as Lange Lynschoten, and means "the long part of the Linschoten (river)". It is not a statistical entity, and the postal authorities have placed it under Snelrewaard. In 1840, Lange Linschoten was home to 144 people. Nowadays, it consists of about 120 houses.

Oudewater (Dutch pronunciation: [ˈʌudəˌʋaːtər] ) is a municipality and a town in the Netherlands.

Wulverhorst is a former municipality in the Dutch province of Utrecht. It was located south of Woerden. Wulverhorst was a separate municipality between 1818 and 1857, when it was merged with Linschoten. The area is now a part of Montfoort as well as Woerden. On the grounds there has existed a castle from the 13th century which felt into ruins and was finally demolished in 1837.

Linschoten (Dutch pronunciation: [ˈlɪnsxoːtə(n)]) is a village in the Dutch province of Utrecht. It is a part of the municipality of Montfoort, and lies about 3 km southeast of Woerden.

Vliet is a hamlet in the Dutch province of Utrecht. It is located about 1 km southwest of the city of Oudewater, on the south bank of the Hollandsche IJssel. Vliet or Ratelsvliet was a separate municipality between 1817 and 1846, when it became part of Haastrecht. During that time, the area was part of the province of South Holland.According to the 19th-century historian A.J. van der Aa, there was no hamlet in the area in the middle of the 19th century. There were just eight houses, with a population of about 50. The area used to be a manor, also called Vliet or "Ratelesvliet", and contained a castle, Te Vliet. The castle was probably built between 1250 and 1300, and existed at least until 1515. In 1647, it was already a ruin, and nowadays just one wall still exists.

Diemerbroek is a village in the Dutch province of Utrecht. It is a part of the municipality of Oudewater, and lies about 3 km (1.9 mi) north of the town of Oudewater. The statistical district "Diemerbroek", which covers the village and the surrounding countryside, has a population of around 150.

The KNMI-mast Cabauw is a 213-metre (699') high guyed mast for meteorological measurements at Cabauw, the Netherlands. In 1972 at Cabauw (06348) a 213 metre (699') high mast was specifically built for meteorological research to establish relations between the state of the atmospheric boundary layer (ABL), land surface conditions and the general weather situation for all seasons. The Cabauw mast is located in the western part of the Netherlands (51.971 °N, 4.927 °E) in a polder 0.7 metres (28") below average sealevel. This site was chosen, because it is rather representative for this part of the Netherlands and because only minor landscape developments were planned in this region. However, significant changes are the removal of the trees along a road east of the mast in 1975, and the building of houses in the village of Lopik east of the mast in more recent years. The North Sea is more than 50 km (30 miles) away to the WNW. The nearby region is agricultural, and surface elevation changes are at most a few metres (yards) over 20 km (12 miles). Within 40 km (25 miles) radius there are four major synoptic weather stations, among which is the regular radiosonde station at De Bilt (06260), ensuring a permanent supporting mesoscale network. Near the mast, the terrain is open pasture for at least 400 metres (yards) in all directions, and in the WSW direction for 2 km (1¼ miles). Farther away, the landscape is generally very open in the West sector, while the distant East sector is rather rough (windbreaks, orchards, low houses). The distant North and South sectors are mixed landscapes, much pasture and some windbreaks. So the highest mast levels have in all directions a long fetch of landscape roughness which is usefully similar to the roughness observed in the lower surface layer. On the mast itself no undisturbed measurements can be made below 20 metres (60'). Therefore, auxiliary 20 metre (60') masts are installed to the SE and the NW at sufficient distance from the mast foot building. South of the mast is a well-kept observation field for micrometeorological observations, including soil heat flux, soil temperatures and various radiation measurements; north of the mast is a spare observation field. The soil consists of 0.6 metres (2') of river-clay, overlying a thick layer of peat. The water table is about 1 metres (3') below the surface, but can be higher during wet periods. The mast is a closed cylinder of 2 metres (6') diameter, with an elevator inside. It is guyed at four levels, and carries booms at 20 metre (60') intervals in three directions. The 9.4 metre (30') booms can be swung up hydraulically, so that instruments at their ends can be handled from an upper balcony; this swivelling mounting allows much longer booms than the customary sideways-sliding construction. Permanent signal cables in the boom tubes run through the hollow swivel axis, so during boom motion they are only torsion-deformed, a more endurable load than bending. Built around the mast foot is a 200 m2 (2000 sq. ft.) streamlined building for registration and maintenance purposes. On top of the mast, a compact weather radar was installed in 2007, measuring precipitation up to a radius of 60 km (40 miles) around the mast.

Papekop is a village in the Dutch province of Utrecht. It is a part of the municipality of Oudewater, and lies about 3 km northwest of the city of Oudewater. Papekop was a separate municipality between 1818 and 1964, when it merged with Driebruggen. Between 1821 and 1989, when it became part of Oudewater, the village was located in the province of South Holland.The village was first mentioned around 1307 as Papencoip, and means "(peat) concession of Pape (probably a clergy)". In 1840, it was home to 284 people. Between 1858 and 1936, there was a railway station in Papekop.

Montfoort (Dutch pronunciation: [ˈmɔntfoːrt] (listen)) is a municipality and a city in the Netherlands, in the province of Utrecht. Montfoort received city rights in 1329.

Tienhoven is a village in the Dutch province of Utrecht. It is a part of the municipality of Vijfheerenlanden, and lies about 10 km southwest of IJsselstein. Tienhoven was a separate municipality in the province of South Holland between 1817 and 1986, when it became part of Zederik. When Zederik merged into the new municipality Vijfheerenlanden in 2019, it became a part of the province of Utrecht. The name of the town has changed to Tienhoven aan de Lek to distinguish it from Tienhoven, Stichtse Vecht, in the province of Utrecht.The village was first mentioned in 1253 as Thienhoeuen, and means "ten parcels of land". In 2019, the name was officially changed to Tienhoven aan de Lek to distinguish from the other Tienhovens. The Protestant church dates from the 12th century, and was enlarged in the 14th and 15th century. The tower dates from the 15th century. In 1840, it was home to 238 people.