しかし、私が誇る美しい風景を見てみたいなら、しかし、私の素晴らしい天然記念物・トップ9
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: 3月 30, 2026
ハイライト • 自然
翻訳者 Google •
役立つ情報 は によるものです
ハイライト • 城
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 • 湖
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
ハイライト • 山頂
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 しかし、私での。
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
excellent place to spend Sundays and holidays, have barbecues and take walks in the surrounding area
0
0
What a beautiful place. We only found one spot where you can pass through, but for bird protection reasons, you shouldn't walk along the embankment. You walk a lot around the lake on the shady paths. Unfortunately, you can't see anything from there because of the tall bushes. It's absolutely peaceful here. There's a little house with a lovely view of the lake.
1
0
by bike it's free. accessible by two paths: one short and steep and the other long and less steep. At the top there is also a bar!
0
0
Along the way you will come across some stony ground, also called Sassete, Pietraie or “Maoni” (local name), they are a peculiar phenomenon at our latitudes and at the modest altitudes reached by Monte Pisano, as they are typical forms of periglacial environment. These are mobile debris flows made up of angular blocks that are easily observable on the south-western side of the mountain and represent an ancient testimony of the last glacial (74,000-13,000 years ago). In the past they were certainly more extensive than the current outcrop areas. Their formation is linked to the type of rock that emerges, mainly green quartzites and white-pink quartzites, which tend to break into angular blocks and provide very little alteration material. Climatic factors have played a fundamental role in the formation of the Sassaie, which represent a degradation product by cryoclasm. Cryoclastism (from the Greek kryòs, ice and klastòs, broken) is the process of physical disintegration of a rock caused by the pressure caused by the increase in volume of water contained within the rock cracks when it freezes. The temperature range therefore favored the fracturing of quartzites, and the low humidity and low average temperature prevented a strong chemical alteration. Cryoclastism is a phenomenon more pronounced in regions of high altitude and latitude, and is usually associated with alpine, periglacial, subpolar maritime and polar climates, but it occurs wherever freeze-thaw cycles are present.
1
0
Exaggerated lawn for picnics or pleasant stops especially with a bit of sun
1
0
During a mountain bike ride, some beautiful views are always nice!
0
0
The faeta is always safe on clear days you have a priceless view
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しかし、私での:
無料でサインアップ