로스톡‬에서 가장 멋진 ‪20‬개의 천연기념물

Heiligendamm에서 Kühlungsborn까지 매우 아름다운 코스입니다. 단단한 길을 걷는 것을 좋아한다면 Steilküstenweg(제방 때문에 항상 물을 볼 수 있는 것은 아님)를 이용하고, 그렇지 않다면 해변을 따라 직접 걷고, Hühnergötter(작은 돌)를 찾고 바람을 코에 맞으세요 🤩

Watch out for pedestrians. This is a relatively narrow bike path with poor visibility at some bends. Enjoy this spot and sit on one of the benches.

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The special feature of the quiet village of Kägsdorf is its fine, sandy, pristine beach in the heart of the Rieden nature reserve, which is exempt from tourist tax year-round. Here, you'll not only experience wonderful bathing days in the summer, but also experience unique natural wonders in the fall and spring. The romantic setting at the tip of the Rieden nature reserve invites couples and families to enjoy a unique picnic, complete with sunset.

A path leads along the coast with a beautiful view

Where the forest falls into the sea The impressive cliffs with their many idyllic corners and a breathtaking view of the sky and the wide sea are among the scenic highlights of the Baltic Sea resort of Nienhagen. With its spectacular, steep coastal path, this area is the ideal destination in the early morning when the sun rises over the sea. But a walk or jog in the evening sunset is of course just as romantic. The cliffs in Nienhagen are experiencing an unstoppable, constant decline due to nature. The reason for this is the phenomenon of steep slopes with high slope stability. This type of cliffs otherwise only includes cliff sections on the Bay of Lübeck, on the island of Poel, Fischland and the Wittow peninsula on Rügen: a special natural phenomenon!

Located in the middle of the beech forest are these fish ponds, which belonged to the Althof and Doberan monastery estate.

The story in brief: The glacier of the Ice Age came from Scandinavia, big, thick and fat (you can hardly imagine how fat it was!), pushed everything in front of it that stood in its way, and came to a standstill 16,000 years ago. The ice that melted flowed forward (i.e. south) and collected in large lakes. When it got warmer (15,000 years ago), the glacier crumbled and melted; the meltwater continued to flow forward (south) in channels, collected... and at some point (11,000 years ago) there was no glacier left, the surface was smooth and also lower, the direction of flow in the channels reversed... and the Warnow deepened the channel by pushing up hills (terminal moraine). Sure, everyone knows that. But seeing all this live, with a 30-40m difference in height between the chain of hills and the Warnow bed, with this story in mind, is a different matter, namely very impressive.