オイセルタールのおすすめ登山＆山歩きルート

地元の人々の間では、ビショフスクロイツの代わりに「ヴェッタークロイツ」と呼ばれることもよくあります。 頂上までの最後の約100mはマウンテンバイクで走破可能ですが、年配のサイクリストは、多くの木の根や石があるため、自転車を押して進む必要があるでしょう。

葉っぱ山の最高地点を示す石のピラミッドを通り過ぎる非常に美しい小道があります。しかし、ここには他にも目印があります。古代の境界石や境界マークのある岩が小道沿いに見られます。十字架はシュパイヤー司教領を表しています。

And we owe it to the formation of the Alps... they press down on the Earth's crust, which couldn't withstand the pressure... and broke apart and was pushed upwards.

You can see it from the reddish sheaf: these rocks consist, among other things, of Dandstein, a legacy of the Ice Age.

"The weather cross, consecrated in 1909 by Bishop Konrad von Busch (1847-1910) of Speyer, was created by stonemason Johann Minges and is the highest weather cross on the Haardt mountain range. Locally, it is also known as the Bishop's Cross." Source (quoted verbatim): https://www.kuladig.de/Objektansicht/KLD-272330 The following text (difficult to read) is inscribed on the base of the cross: "Behold the Cross of the Lord! // Flee, you hostile forces! // The Lion of Judah. // The Root of David has triumphed! // Alleluia, Alleluia! // (St. Anthony of Padua)" A vineyard (large vineyard area) in the Southern Palatinate is also called "Bischofskreuz" (Bishop's Cross).

These rock formations made of sand and colored stone are about 250-270 million years old.

The Palatinate Forest, which rises to about 450 meters above sea level, is, in my opinion, the most beautiful low mountain range in Germany.

Such rock formations are typical for the Palatinate Forest and make up part of its character. For those interested in geology: the sandstone formations are between 250 and 270 million years old. Incidentally, there are only 3 sandstone veins in Europe, one of which runs here.