엠네스 최고의 MTB 라이딩 경로

The drainage of the Breukelerveen and Tienhoven water board was originally carried out by two barges (built in 1649 and 1684) at the northern end of the Scheendijk-Noord in Breukelen. They discharged their water directly south of the Weersluis lock into the Vecht River. The mills were shut down in 1830 and demolished in 1840. By that time, the area of the Loosdrechtse Plassen had been created by peat extraction. In the eastern corner of Tienhoven, the land remained in agricultural use, and the farmers there suffered from significant flooding. They joined forces, established the Oostelijke Binnenpolder (Eastern Inner Polder), and had their own mill built, which discharged water into the Breukeleveen and Loosdrechtse Plassen. The necessary land was purchased in 1831, and the mill and adjacent lock were put into operation in 1833. It is suspected that an old upper house (from a demolished mill) was used in its construction. (https://www.molens.nl/ontdek-molens/alle-molens/de-trouwe-wachter-te-tienhoven)

The origin of this boulder is not entirely clear. However, you can easily test for yourself on site whether it actually bleeds when you prick it.

A truly beautiful cycle path through the heathland - a pleasure, not only when the heather is in bloom.

Wonderful piece of nature here for walking or cycling.

Beautiful route through a heathland, just driving through nature.

Behind the castle you can take a nice walk in the Hoge Vuursche forest.

Impressive country house De Hooge Vuursche with a beautiful fountain that completes the picture.

Unfortunately, large parts of the singletrack will be overgrown on July 7, 2025. To be able to cycle a bit on narrow singletracks, this is therefore not recommended in the summer.