뉘브레히트 최고의 러닝 경로

Lively place with restaurants and Homburg Castle

A truly beautiful town center with half-timbered houses and shingle-clad houses.

Beautiful old town center with half-timbered houses and shingle-clad houses.

The shelter is currently closed because it's damaged. Forest xylophone: Great idea! Unfortunately, it doesn't play any connected notes (scales, pentatonic scales, etc.).

Beautiful little place

Beautiful park with a large playground

<< Quartzite stone formation “Dicke Steine” near Homburg Castle >> "The “Dicke Steine” gave rise to a great deal of speculation in the past about their formation and origin. Like the Wiehl stalactite cave, they are one of the geological attractions of the Homburg region. They were formed in the Tertiary period, i.e. 65 to 2 million years ago. At that time, the Bergisches Land had a warm tropical climate. The soil was characterized by the soft sandstone that still predominates today. This was deposited on the sea floor in the Paleozoic period (Devonian). In the places where the Dicken Steine are today, warm, silicic water must have flowed through the sandstone. This caused quartz particles to dissolve in the sandstone, which were then “precipitated” out of the water solution, i.e. they settled again. This formed a fine-grained, closely interlocked quartz. However, this was still surrounded by sandstone - it was only through strong leaching processes that the surrounding softer sandstone layers. The quartzite stones, however, resisted this erosion and remained as "thick stones". The fossils that are often present in the sandstone fell victim to the erosion process almost completely, but can sometimes still be seen in outline in the quartzite." (Oberberg Biological Station, 2013, created as part of the project "Hedge, Hollow Way, Homeland - Cultural Landscape Communication Analogue and Digital". A project within the framework of the LVR Environmental Network) https://www.kuladig.de/Objektansicht/O-57899-20121207-3

Very pretty town center with several cafes.