しかし、私の天然記念物・トップ9

ウペッツィンギ家の塔、別名カプロナの塔は、ピサ県ヴィコピサーノの自治体にある岩棚に位置する印象的な建造物です。ウペッツィンギ家によって建てられた19世紀のレプリカですが、11世紀半ばに建てられ、1433年にフィレンツェ人によって解体された古代の中世の城の跡地に建っています。この場所は、1289年の有名な戦いの舞台となったことで、イタリアの歴史と文学において有名であり、若いダンテ・アリギエーリが参加し、後に神曲の地獄篇第21歌でカプロナの包囲戦を明確に引用しました。

excellent place to spend Sundays and holidays, have barbecues and take walks in the surrounding area

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.

Nice difference in altitude

top place to refresh yourself

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!

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.

Exaggerated lawn for picnics or pleasant stops especially with a bit of sun