ヴェスターラーデの湖・トップ20

The 3.7 km long trail leads along the partially wooded shore of the Herrenteich lake. The east and west banks are connected by a bridge at the "Fischhuser Damm"—north of this bridge begins the "Oberer Herrenteich" nature reserve. See: https://reinfeld-aktiv.de/tag/reinfeld/page/6/

The further you get from Bad Segeberg, the quieter and more secluded the path becomes – at least in winter. After rain or during thaws, it can sometimes be very muddy.

The Herrenteich in Reinfeld owes its existence to Cistercian monks who founded the Reynevelde monastery in the 12th century. They cleared the forest, created fish ponds and dammed the Heilsau to form the Herrenteich. Water lily - Photo: Silke Oldorff Water lily - Photo: Silke Oldorff The Herrenteich in Reinfeld, Stormarn district, owes its existence to the Cistercian monks who founded the "Reynevelde" monastery in the area of the marshy lowlands of the Heilsau in the 12th century. The Heilsau rises near today's Stockelsdorf (Ostholstein district) and flows into the Trave below Reinfeld. Count Adolf commissioned this Cistercian order in 1186 to reclaim this "place of loneliness and terror", according to contemporary witness Provost Sido from Neumünster. They cleared the forest, created small fish ponds and used the excavated material to build the dam for the Heilsau to form the Herrenteich. The monks lived in the monastery until the 16th century

With 37 hectares, the Herrenteich is the largest of a total of five freshwater ponds in Reinfeld; with its diverse bank vegetation, it offers a home to many animal species.

On hot days, the shady paths are a welcome change 😉...

The Ihlsee is located in the northwestern part of the district town of Bad Segeberg on the northern edge of the Kleinniendorf district and is part of the designated Ihlsee and Ihlwald nature reserve. The origin of the lake has not been fully investigated. Either the depression was formed after the Ice Age due to dead ice or it was created as a sinkhole by the collapse of a cave in the Segeberg salt dome. Today the lake has an area of around 29 hectares and stretches 450 m from north to south and around 850 m from west to east; the shore is 2.25 km long. Along with the Bültsee and the Garrensee, the lake is one of the few nutrient-poor lakes in Schleswig-Holstein. The lake is located in a depression and has no inflow. It is fed only by groundwater and inflowing surface water (precipitation). To the north of the bathing area is the outflow that connects the lake to the Great Segeberg Lake. The lake can be walked around, but there is no path along the lake. There is a bathing area on the eastern shore that has existed for decades. The bathing water quality is regularly monitored and in recent years has been rated as very good to good. There is a residential area on the northern shore. On the western and southern sides, the Ihlwald, a swamp forest, dominates the shoreline. From 1911 to 1961, there was a Kiel-Segeberg narrow-gauge railway station at Ihlsee, the tracks of which were removed in 1962. The Ihlsee was declared a nature reserve in 1950 because of its special features. The lake is a particularly nutrient-poor body of water, which gives rise to rare flora. Today, the lake is part of the Ihlsee and Ihlwald nature reserve and has been part of the Natura 2000 protected area network since 2006. https://de.wikipedia.org/wiki/Ihlsee

In the season you don't necessarily have to go hiking ;-)...

Beautiful hiking trail around the lake.