オーバープファルツ周辺のおすすめ犬連れハイキング＆ウォーキング

ここからウェイクボーダーを眺めるのはとても良いです。 居心地の良い場所です。 そして、私は彼らがコースを回るのを見るのが大好きです。

高地湿原に関する情報資料がある興味深い場所

Lake Steinberger Lake Steinberger is part of the Upper Palatinate Lake District and, with an area of 1.84 km², is the largest lake in the Upper Palatinate. It was named after the municipality of Steinberg am See. It is 1.98 km long, 1.4 km wide, and has a maximum depth of 50 meters. The Schreckerbach stream feeds and drains the lake. After the Bavarian lignite industry ceased mining operations in the mid-1980s, the open-cast mine "Steinberger See" was flooded by reducing the water level. Remaining mining equipment was demolished and still lies on the lakebed. Two small, wooded islands also remain, which now divide the lake into a northern and a southern section. In the following decades, tourism developed at Lake Steinberger, bringing a degree of economic growth to the region. In addition to the Steinberger Yacht Club (SYC), founded in 1987, the area now boasts a sailing school, a water ski lift, a boat rental, a leisure park for families and children, a surf club, and most recently, an adventure golf course and a roughly 40-meter-high wooden "adventure sphere" with viewing platforms, an obstacle course, and a giant slide. Numerous restaurants, inns, and cafés complement the leisure offerings. A water rescue station has been established for the safety of visitors. Due to the increasing improvement in water quality and visibility in recent years, Lake Steinberger has become one of the most popular diving areas in the Upper Palatinate. Like all lakes in the Upper Palatinate Lake District, which originated from lignite mines, the water is acidic due to leaching. Because of the ongoing improvement in water quality, fish populations are steadily increasing. Perch and the occasional pike have been observed most frequently. The water is very clean; on windless days, visibility is possible to a depth of at least 10 meters. Occasionally, the tops of dead trees can be seen on the bottom. According to the ordinance issued by the Schwandorf District Office on August 8, 2002, the entire Steinberger See is open for diving. Especially in summer and winter, very good visibility (up to 20 meters) has been possible in recent years. Source: Excerpts from www.wikipedia.de

Great route for cycling

The Otterbach The Otterbach originates in the church village of Süssenbach, in the municipality of Wald in the Chams district, at approximately 477 m above sea level, through the confluence of the Weismühlbach and Steinbach streams. From there, it flows steadily southwestward, initially also called the Süssenbach, in loops that are particularly wide at the beginning. After passing through about a dozen smaller villages in Wald, it crosses the border into the Regensburg district and enters the municipality of Altenthann, passing through the village of Forstmühle there, and then flows northwest past the large, unincorporated forest area of the Forstmühle Forest. It passes successively the Altenthann hamlet of Bruckhäusl on the left bank, its church village of Heuweg on the right bank and on the heights above the valley, the village of Oberlichtenwald, which is located on the same bank as the stream, and the village of Unterlichtenwald on the right bank of the estuary in the wide floodplain. There, the most important tributary, the Sulzbach, flows along the other side of the village. Its upper reaches, together with its own course, even exceed the length of the Otterbach main branch up to this point, but contribute about a quarter less to the catchment area. From there, the St. 2145 state road uses the valley. The valley now narrows again between steep forest slopes, and the Otterbach enters the territory of Markt Donaustauf, where it successively passes the isolated villages of Neumühle and Klammer on its banks. The valley then widens into a large field bay, where it flows between the hamlets of Hammermühle and Dachsberg. Before Scheuchenberg, the stream, which ultimately flows almost southward, deviates to the right and southwest, crosses the church village of Sulzbach an der Donau, flows under the St. 2125 state road, which follows the stream, and flows into the Danube on the left after 17 kilometers. A popular hiking trail runs along the stream between Forstmühle and Hammermühle. Source: Excerpts from www.wikipedia.de

From here on it gets really adventurous

Unfortunately, there is a lack of water here too, and too little snow in winter.

As it flows, the Waldnaab grinds away granite blocks lying in the riverbed. The anvil is particularly strongly undercut in two directions: one toward the oncoming water (windward, impact side) and—at first glance surprising—also on the opposite side (leeward), i.e., downstream. On the upstream side, the grinding is easily explained by drifting debris, gravel, and sand. On the leeward side, the circulating currents collide, creating eddies that similarly erode the granite.