place

Hochfirst Tower

Towers completed in 1890
Hochfirstturm
Hochfirstturm

The Hochfirst Tower (German: Hochfirstturm) is a 25-metre-high lattice observation tower on the Hochfirst mountain near Titisee-Neustadt at 47°54'04" N and 8°11'03" E. It was built in 1890 as the replacement for a wooden observation tower. Several observation decks may be accessed by the winding corrugated metal staircase, and the top deck provides panoramic views of the distant Swiss Alps and the Titisee-Neustadt valley. The tower is accessible from the Freiburg-Lake Constance Black Forest Trail and is near the small village of Saig. Currently, Hochfirst Tower is used for directional radio and mobile phone services as well as for observation purposes. Hochfirst Tower has been further reinforced to withstand the strong valley winds.

Excerpt from the Wikipedia article Hochfirst Tower (License: CC BY-SA 3.0, Authors, Images).

Hochfirst Tower
Auf dem Hochfirst, Titisee-Neustadt

Geographical coordinates (GPS) Address External links Nearby Places
placeShow on map

Wikipedia: Hochfirst TowerContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 47.901111111111 ° E 8.1841666666667 °
placeShow on map

Address

Hochfirstturm

Auf dem Hochfirst
79822 Titisee-Neustadt, Neustadt im Schwarzwald
Baden-Württemberg, Germany
mapOpen on Google Maps

linkWikiData (Q880481)
linkOpenStreetMap (1436366070)

Hochfirstturm
Hochfirstturm
Share experience

Nearby Places

Windgfällweiher
Windgfällweiher

The Windgfällweiher is a reservoir between the Titisee and the Schluchsee in the south of Baden-Württemberg, Germany. It is located within the High Black Forest and lies in a hollow formed by ice age glaciation between the villages of Altglashütten, Falkau and Aha on the territory of the municipality of Lenzkirch. The lake lies in a trough that runs from the Seebach valley in the northwest to the Schluchsee in the southeast and thus crosses the generally northeastward-running streams in the area. This remnant of a former valley is followed by the Three Lakes Railway that was built between 1920 and 1926 and by the transfer channel (Überleitungskanal), built in 1932 and belonging to the Schluchseewerk, which takes water from the Seebach valley via the Haslach valley to the Schluchsee Basin. North of the low-lying watershed in this trough, between the Haslach in the north and the Ahabach in the south, now drowned by the impounded Schluchsee, the glacier of the last ice age carved out a basin, in which a small bog lake formed, the natural precursor to today's reservoir. This was enlarged in 1895 by the former Falkau Screw Works (Schraubenfabrik Falkau) with a dam in the north and the water surface raised by about 6 metres. At the same time the lake, which had only hitherto been fed from the east by the Kähnerbächle, was given another inflow in the form of a small leat (Hangkanal) from the southwest. Since 1932 the Windgfällweiher has been incorporated into the transfer of water from the Seebach to the Schluchsee (covered leat) and drained since then in the opposite direction i.e. to the south. The water is led via a ditch over the low watershed, initially as the Windgefällbach and later, the Schwarzach, into the Schluchsee. Since 1950 the lake has been protected. In 2002 an angling and fish consumption ban was announced, because PCB had been discovered in the sediment depositions on the bottom of the lake.On the wooded eastern shore of the Windgfällweiher, a lake barely touched by the streams of visitors to the area, lies a rather less picturesque bathing beach with a listed building.The Windgfällweiher, together with the Schluchsee and Titisee, contributed to the name of the Three Lakes Railway.