부티‬에서 가장 멋진 ‪9‬개의 천연기념물

Torre degli Upezzinghi, 또는 Torre di Caprona로도 알려진 이 탑은 피사현 Vicopisano 지역의 바위 돌출부에 위치한 인상적인 구조물입니다. Upezzinghi 가문이 세운 19세기 복제품이지만, 11세기 중반에 지어졌다가 1433년 피렌체인들에 의해 해체된 고대 중세 성터 위에 세워졌습니다. 이 장소는 1289년 젊은 단테 알리기에리가 참여한 유명한 전투의 현장이었던 곳으로 이탈리아 역사와 문학에서 유명하며, 그는 이후 신곡 지옥편 제21곡에서 카프로나 공성전을 명시적으로 언급했습니다.

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