ロヴェレ・ヴェロネーゼの天然記念物・トップ20

Il Salto del Còvolo Tondoは、荒々しく示唆に富むValle Boragoが、24メートルの予期せぬ乗り越えられない垂直の飛躍を遂げる地点です。かつてこの渓谷が豊かで激しい古代の川によって横断されていた時代に、何百万年もの間、水の浸食によって作られた、270°で閉じた岩のニッチです。今日、渓流の川床は一般的に乾いていますが、大雨の場合には一時的に滝が発生することがあります。 Vajo Borago（そしてそれをたどる小道）は、この記念碑的な自然の壁で突然途切れるように見えますが、実際にはMontecchioの町まで続いています。Saltoは、崖にしがみつくめまいがするような金属製の梯子と、短いが急な傾斜路の連続によってのみ乗り越えることができます。 壮大な景観！

first peak

The "Vajo del Bruto" or Valle delle Buse di Sopra, more simply known as the Valle delle Sfingi, is located in the contrada del Brutto or malga Buse di Sotto in Camposilvano. It is a particular valley, about 800 meters long, which has large monoliths regularly spaced from each other and which recall the Egyptian sphinxes, from which it takes its name. These particular rocks are the result of the karst erosion of two different rock formations, the Rosso Ammonitico and the Oolite di San Vigilio. The Valle delle Sfingi is a magical place, full of stories and legends, such as the one linked to the particular mushroom-shaped rock, also known as "el sengio de l'orco". According to tradition, in fact, this mushroom was brought here by an ogre to allow the fade (magical creatures) to tie a rope end to it to hang out the laundry. Or like the "Fò della Pace", a large tree isolated from the others and so called because under its shade disputes were resolved and contracts were drawn up.

Already done it's beautiful. It's not difficult, just a little attention

Always a magical place to see

At 1,545 meters high, Corno d'Aquilino is one of the most famous peaks of the Lessini Mountains, above Verona. It borders Valpolicella to the north and its name seems to derive from the Latin "aquilus", meaning dark. On one of its slopes, it boasts one of the deepest karst abysses in the world, almost 1,000 meters.

Modest peak in Sant'Anna d'Alfaedo, which however reserves more than one surprise. We are inside the regional natural park of Lessina, where in addition to the splendid panoramas nearby it is possible to visit the Grotta del Ciabattino.

Very suggestive place due to the presence of these rock formations, typical of Lessinia (they are also seen in other parts but here they are concentrated in a particular way, with the formations that stand out from the ground giving the idea of the Sphinxes)