タラントの絶景の山頂・トップ20

It's just incredibly beautiful here 😊.

Beautiful view, especially when the rapeseed is in bloom, highly recommended.

The Bayerhöhe is located on the Baltic Sea - Saale Dam long-distance hiking trail.

with a view of Dresden, several hiking trails

Erected in 1865, made of sandstone, techn. monument

"The Götzenbüschchen (also: Götzenbusch) is a wooded hill near Oelsa in the Eastern Ore Mountains. The area consists of sandstone from the Cretaceous period and is under state protection as a natural monument because of its special geology." - https://de.wikipedia.org/wiki/G%C3%B6tzenb%C3%BCschchen A fine, small trail leads along the edge of the field. It also offers a beautiful view over the Weisseritz Valley.

The Royal Saxon Triangulation was a large-scale surveying project carried out in the Kingdom of Saxony between 1862 and 1902. The aim was to measure the country precisely and determine geographic coordinates in order to create better maps. The survey covered numerous points throughout the kingdom and 36 1st order and 122 2nd order triangulation pillars were erected, including the triangulation pillar on the Gohilg. The survey results formed the basis for the creation of the first topographical map of the Kingdom of Saxony.

"Götzenbüschchen" natural monument Dresden-Elbland 350 m On the ridge between Roter Weisseritz and Oelsabach, a copse is home to a natural monument ("geotope") that has long been known to geologists. Here is a remnant of the sandstone cover from the Cretaceous, which overlays the Ore Mountain gneiss. The special feature of this outcrop is that part of the soil formation at that time was covered by the sedimentation in the Cretaceous period and was therefore preserved. In the Cretaceous period, the climate was tropical, and this is how so-called red earth could develop, which got its red color from bivalent iron oxides. These soils are also widespread in today's tropics. This fossil soil horizon is only exposed on a very small scale, since it is either still covered or has already been removed. On the other hand, the thin-plate, also deeply weathered gneiss with a striking violet-red color is clearly visible.