エルスニッツが誇る美しい風景を見てみたいなら、エルスニッツの素晴らしい天然記念物・トップ20
に行ってみましょう。あなたにぴったりの場所が見つかるよう、素晴らしい天然記念物を探索するために必要なすべての情報を集めました。次のアウトドアの冒険に出かける計画の参考にしましょう。
最終更新日: 4月 9, 2026
ハイライト • 記念碑
翻訳者 Google •
役立つ情報 は によるものです
ハイライト • 自然記念物
翻訳者 Google •
役立つ情報 は によるものです
今すぐサインアップして、こんな場所を発見しよう
最高のシングルトラック、ピーク、その他のエキサイティングなアウトドアスポットのおすすめを受け取ろう。
無料新規登録
ハイライト • 自然記念物
翻訳者 Google •
役立つ情報 は によるものです
ハイライト • 記念碑
翻訳者 Google •
役立つ情報 は によるものです
ハイライト • 自然記念物
翻訳者 Google •
役立つ情報 は によるものです
無料でサインアップして、さらに多くの自然記念物を発見しましょう エルスニッツでの。
無料新規登録
すでにアカウントをお持ちですか?
無料アカウントで今日から始めよう
次の冒険が待っています。
ログインまたは登録
エルスニッツ周辺で人気
The Wendelstein (734 m) is part of a long chain of rocky cliffs that jut sharply out of the earth. This striking rock formation begins at the "Hoher Stein" (Czech Republic), continues via the "Alter Söll" (Schöneck), the "Rehhübel," "Rinnelstein," "Großer Affenstein," "Kleiner Affenstein," "Genesenstein," "Wendelstein," and "Schwarzer Stein" (all Grünbach) to the "Bendelstein" near Auerbach. The Wendelstein, like all the others, is composed of greywacke quartzite. This is a dark gray, mostly highly consolidated sandstone composed of feldspar, chlorite, and mica, with a high proportion of slate and quartzite. About 500 million years ago, the Vogtland region was covered by a shallow sea. Sand and mud settled on the bottom, which subsequently solidified into sandstone and slate, the sedimentary rock, due to climate change and landslide. Forced upwards under enormous heat and pressure, phyllite and quartzite were formed. (https://www.gruenbach.de/freizeit_aktiv)
0
0
The Poppenstein is located on the northern shore of the Werda Dam. The Poppenstein and the neighboring small rock formations are composed of fruit or knotted slate. This clay slate, formed approximately 500 million years ago, was transformed and hardened under the influence of upwelling magmatic melt. The small pits on the rock's surface are the result of chemical weathering, where embedded minerals were dissolved out. (Information panel at the Poppenstein)
0
0
A striking viewpoint on the trail from Falkenstein to Grünbach. The Lochstein is a popular destination for both locals and visitors. A covered seating area sponsored by the town's residents always invites you to take a break, which is also greatly appreciated by hikers on Felsenweg 3b from Werda. Located in the Vogtland Geo-Environmental Park, the Lochstein is a greywacker quartzite rock – an impressive rock that can be climbed with a view of the Falkenstein town area. However, when climbing, the "Lochstein" is primarily for more experienced climbers because it has been left in its almost pristine state, which is why it is advisable to have a pair of slings, friends, or nuts handy. But even without this challenge, the Lochstein is simply beautiful in any season. (https://www.vogtland-tourismus.de/mobile/de/poi/aussichtspunkt/lochstein-bei-falkenstein-vogtland/23502738 )
0
0
The Wendelstein has been protected as a geological natural monument since November 5, 1938. A triangulation column dated 1864 was erected on the highest part of the rock, representing a second-order survey point in the course of the historic Saxon national survey. The Wendelstein is 734 m above sea level and is part of a long chain of rocky cliffs that jut steeply out of the earth. This striking rock formation begins at the "Hoher Stein" (Czech Republic), continues via the "Alter Söll" (Schöneck), the "Rehhübel," "Rinnelstein," the "Großer Affenstein" and "Kleiner Affenstein," the "Genesenstein," "Wendelstein," and the "Schwarzer Stein" (all Grünbach) to the "Bendelstein" near Auerbach. (https://www.gruenbach.de/freizeit_aktiv/gehenswertes_rund_um_gruenbach-muldenberg/wendelstein/index.php)
0
0
There is a small hut and a few benches here. Ideal for a short rest.
0
0
Beautiful rock. It's worth a detour.
0
0
At the top of the Wendelstein there is a historic triangulation column and a summit cross.
0
0
これらのガイドで、最高の洞窟を探す範囲を広げましょうエルスニッツでの:
無料でサインアップ