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Höllental (Lower Austria)
The Höllental ("Hell Valley") in Lower Austria is a narrow valley between the steep limestone massifs of the Schneeberg and Rax through which the River Schwarza flows. It stretches for a total of 16.5 km between Schwarzau im Gebirge and Hirschwang and, because of its natural beauty, it belongs to the Natura 2000 region of Northeastern Border Alps: Hohe Wand - Schneeberg - Rax (''Nordöstliche Randalpen: Hohe Wand - Schneeberg - Rax''). It biggest side valleys are the Weich valley, the Großes Höllental (which is much smaller however), the Kesselgraben, the Nasswald and Voisbach valleys. A well-developed road, the Höllental Straße (B 27), follows the course of the river and is especially popular with motorcyclists. In the valley and its side valleys are important sources of drinking water supply (The Fuchs Pass Spring, Kaiserbrunn and Wasseralm Spring), whose water is delivered to the Austria's capital city of Vienna over the First Vienna Mountain Spring Pipeline (''I. ...
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Kayak
A kayak is a small, narrow watercraft which is typically propelled by means of a double-bladed paddle. The word kayak originates from the Greenlandic word '' qajaq'' (). The traditional kayak has a covered deck and one or more cockpits, each seating one paddler. The cockpit is sometimes covered by a spray deck that prevents the entry of water from waves or spray, differentiating the craft from a canoe. The spray deck makes it possible for suitably skilled kayakers to roll the kayak: that is, to capsize and right it without it filling with water or ejecting the paddler. ] Some modern boats vary considerably from a traditional design but still claim the title "kayak", for instance in eliminating the cockpit by seating the paddler on top of the boat ("sit-on-top" kayaks); having inflated air chambers surrounding the boat; replacing the single hull with twin hulls; and replacing paddles with other human-powered propulsion methods, such as foot-powered rotational propellers an ...
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Neunkirchen District, Austria
Bezirk Neunkirchen () is a district of the state of Lower Austria in Austria. It is located at the south of the state. Municipalities * Altendorf :Parts of the village: Altendorf, Loitzmannsdorf, Schönstadl, Syhrn, Tachenberg * Aspang-Markt *Aspangberg-Sankt Peter :Parts of the village: Großes Amt, Kleines Amt, Neustift am Alpenwald, Neuwald * Breitenau * Breitenstein *Buchbach *Bürg-Vöstenhof :Parts of the village: Bürg, Vöstenhof *Edlitz * Enzenreith :Parts of the village: Enzenreith, Hart, Hilzmannsdorf, Köttlach, Thürmannsdorf, Wörth * Feistritz am Wechsel :Parts of the village: Feistritz am Wechsel, Grottendorf, Hasleiten, Hollabrunn *Gloggnitz :Parts of the town: Abfaltersbach, Aue, Berglach, Eichberg, Gloggnitz (with Furth and Gföhl), Graben, Heufeld, Saloder, Stuppach, Weißenbach * Grafenbach-Sankt Valentin :Parts of the village: Göttschach, Grafenbach, Ober-Danegg, Penk, St. Valentin-Landschach * Grimmenstein :Parts of the village: Grimmenstein, Hochegg * Grün ...
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Rax-Schneeberg Group
The Rax-Schneeberg Group (german: Rax-Schneeberg-Gruppe) is a mountain range in the Northern Limestone Alps on the Styrian- Lower Austrian border in Austria. Location According to the official classification of the Eastern Alps by the Alpine Club ('' Alpenvereinseinteilung der Ostalpen''), the Rax-Schneeberg Group is bounded by the following divisions to neighbouring groups of mountains: * to the north by the Klostertaler Gscheid – Klausgraben – Mamauwiese – Sebastiansbach – Puchberg * to the northeast by the valley of the River Sierning as far as Ternitz * to the south by the line: Ternitz – Schwarza near Gloggnitz – Schottwien – Semmering – Mürzzuschlag – Mürz near Kapellen * to the west by the Altenberg valley – Naßkamm – Naßbach – Schwarza – Voisbach as far as the Klostertaler Gscheid. Summits The highest point in the limestone massif of the Schneeberg is the ''Klosterwappen'' at . Its nearby twin peak is known as the '' Kaisers ...
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Valleys Of Lower Austria
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. Fo ...
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Canyons And Gorges Of Austria
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ca ...
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Höllental Railway (Lower Austria)
The Lower Austrian Höllental Railway (german: Höllentalbahn) is a narrow gauge electric railway with a track gauge of , which runs from the Austrian Federal Railways (ÖBB) station of Payerbach Reichenau on the Semmering Railway for approximately five kilometres through the market town of Reichenau an der Rax to Hirschwang. History The railway opened in 1918 to serve a paper mill and was opened to passengers and general goods traffic in 1926. Apart from local commuter traffic the railway also served tourist groups as a feeder for the , the first cable car in Austria which also opened in 1926. At the beginning of the 1960s large scale investment was needed, so in 1963 passenger traffic was stopped and replaced by post office buses. The goods traffic, in particular to the paper mill in Hirschwang, continued until 1982. In 1977 the Austrian Society for Local Railways (ÖGLB) was created, and in 1979 began operating passenger trips for tourists on weekends in the summer. Sin ...
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Payerbach
Payerbach is a town in the district of Neunkirchen in the Austrian state of Lower Austria. Population References Payerbach - Kirche.JPG, Parish church St. James the Greater Payerbach-Reichenau-Bahnhof-01.jpg, Train station Payerbach-Reichenau Cities and towns in Neunkirchen District, Austria {{LowerAustria-geo-stub ...
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Rohr Im Gebirge
Rohr im Gebirge is a village in the Wiener Neustadt-Land district of Lower Austria in Austria. Geography Rohr im Gebirge is located in the Industrieviertel, the first industrialised part of Lower Austria. Of its 80.58 square kilometers, 89.95% is woodland. There are no other cadastral communities than Rohr im Gebirge. History Before the Common Era, the area was part of the Celtic kingdom of Noricum and was within the area of influence of the oppidum of Burg in Schwarzenbach on the Burgberg, which was the main settlement of the northeast part of the kingdom. Later, under the Romans, it was within the province of Pannonia. Because of its inaccessibility, the location was settled late. The Lords of Traisma are recorded as the first owners of the forests around Rohr im Gebirge. In 1194, the area passed to the Duchy of Steyr. After the construction of Burg Gutenstein (first mentioned in 1220), Rohr came under its influence; Gutenstein remained the centre of government for the re ...
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Fly Fishing
Fly fishing is an angling method that uses a light-weight lure—called an artificial fly—to catch fish. The fly is cast using a fly rod, reel, and specialized weighted line. The light weight requires casting techniques significantly different from other forms of casting. The flies may resemble natural invertebrates, bait-fish, or other food organisms. Fly fishing can be done in fresh or saltwater. North Americans usually distinguish freshwater fishing between cold-water species (trout, salmon) and warm-water species, notably bass. In Britain, where natural water temperatures vary less, the distinction is between game fishing for trout and salmon versus coarse fishing for other species. Techniques for fly fishing differ with habitat (lakes and ponds, small streams, large rivers, bays and estuaries, and open ocean.) Author Izaak Walton called fly fishing "The Contemplative Man's Recreation". Overview In fly fishing, fish are caught by using artificial flies tha ...
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Wild Water
Whitewater forms in a rapid context, in particular, when a river's gradient changes enough to generate so much turbulence that air is trapped within the water. This forms an unstable current that froths, making the water appear opaque and white. The term "whitewater" also has a broader meaning, applying to any river or creek that has a significant number of rapids. The term is also used as an adjective describing boating on such rivers, such as whitewater canoeing or whitewater kayaking. Fast rivers Four factors, separately or in combination, can create rapids: gradient, constriction, obstruction, and flow rate. Gradient, constriction, and obstruction are streambed topography factors and are relatively consistent. Flow rate is dependent upon both seasonal variation in precipitation and snowmelt and upon release rates of upstream dams. Streambed topography Streambed topography is the primary factor in creating rapids, and is generally consistent over time. Increased fl ...
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