The lake is situated in Germany, Switzerland, and Austria near the Alps. Its shorelines lie in the German states of Bavaria and Baden-Württemberg, the Austrian state of Vorarlberg, and the Swiss cantons of Thurgau, St Gallen, and Schaffhausen. The Rhine flows into the lake from the south, with its original course forming the Austro-Swiss border, and has its outflow on the "Lower Lake" where — except for Schaffhausen — it forms the German-Swiss border until the city of Basel.
Freshwater Lake Constance is central Europe's third largest, after Lake Balaton and Lake Geneva. It is 63 km (39 mi) long, and at its widest point, nearly 14 km (8.7 mi). It covers approximately 571 km2 (220 sq mi), and is 395 m (1,296 ft) above sea level. The greatest depth is 252 metres (827 ft) in the middle of the eastern part (Obersee). Its volume is approximately 10×10
^9 m3 (13×10 ^9 cu yd). The lake has four parts: the main section, called Obersee, 476 km2 (184 sq mi); the north section, Überlinger See, 61 km2 (24 sq mi); the west section, Untersee, 63 km2 (24 sq mi); and the northwest section, the Zeller See and Gnadensee. The regulated Rhine flows into the lake in the southeast, through the Obersee, the city of Konstanz and the Untersee, and flows out near Stein am Rhein. The lake itself is an important drinking water source for southwestern Germany, called Bodensee-Wasserversorgung ("Lake Constance Water Supply"). The culminating point of the lake's drainage basin is the Tödi at 3,614 metres above sea level.
Car ferries link Romanshorn to Friedrichshafen, and Konstanz to Meersburg.
Lake Constance was formed by the Rhine Glacier during the ice age and is a zungenbecken lake. After the end of the last glacial period, about 10,000 years ago, the Obersee and Untersee still formed a single lake. The downward erosion of the High Rhine caused the lake level to gradually sink and a sill, the Konstanzer Schwelle, to emerge.
The Rhine, the Bregenzer Ache, and the Dornbirner Ache carry sediments from the Alps to the lake, thus gradually decreasing the depth and coastline extension of the lake in the southeast. In antiquity the two lakes still had different names; later, for reasons which are unknown, they came to have the same name.
The Roman geographer, Pomponius Mela, was the first to mention the lake around 43 AD, calling the Lacus Venetus and the Untersee Lacus Acronius, the Rhine passing through both. Around 75 AD, The naturalist Pliny the Elder called the entire Lake Constance, Lacus Raetiae Brigantinus after the main Roman town on the lake, Brigantium (later Bregenz). This name is associated with the Celtic Brigantii who lived here, although it is not clear whether the place was named after the tribe or the inhabitants of the region were named after their main settlement. Ammianus Marcellinus later used the form Lacus Brigantiae.
The current German name of Bodensee derives from the place name Bodman, which probably originally derived from the Old High German bodamon which meant "on the soils", indicating a place on level terrain by the lake. This place, situated at the west end of Lake Überlingen (Überlinger See), had a more supraregional character for a certain period in the early Middle Ages as a Frankish imperial palace (Königspfalz), Alamannian ducal seat and mint, which is why the name may have been transferred to the lake ("lake, by which Bodman is situated" = Bodmansee). From 833/834 AD, in Latin sources, the name appears in its latinised form lacus potamicus. Therefore, the name actually derived from the Bodman Pfalz (Latinized as Potamum) was wrongly assumed by monastic scholars like Walahfrid Strabo to be derived from the Greek word potamos for "river" and meant "river lake". They may also have been influenced by the fact that the Rhine flowed through the lake.
Wolfram von Eschenbach describes it in Middle High German as the Bodemensee or Bodemsee which has finally evolved into the present German name, Bodensee. The name may be linked to that of the Bodanrück, the hill range between Lake Überlingen and the Untersee, and the history of the House of Bodman.
The German name of the lake, Bodensee, has been adopted by many other languages, for example: Dutch: Bodenmeer, Danish: Bodensøen, Norwegian: Bodensjøen, Swedish: Bodensjön, Islandic: Bodenvatn, Finnish: Bodenjärvi, Estonian: Bodeni järv, Lithuanian: Bodeno ežeras, Latvian: Bodenezers, Russian: Боденское озеро, Polish: Jezioro Bodeńskie, Czech: Bodamské jezero, Slovak: Bodamské jazero, Hungarian: Bodeni-tó, Bulgarian: Боденско езеро, Ukrainian: Боденське озеро, Croatian: Bodensko jezero, Albanian: Liqeni i Bodenit. Even in many Asiatic languages, the lake is called the Bodensee e.g. Azerbaijani: Boden gölü, Tatar: Боден күле, Marathi: बोडन से Bōdana sē, Mandarin: Chinese: 波登湖; pinyin: Bódēng-hú, Korean: 보덴 호 Boden-ho, Japanese: ボーデン湖 Bōden-ko.
After the Council of Constance in the 15th century, the alternative name Lacus Constantinus was used in the (Roman Catholic) Romance language area. This name, which had been attested as early as 1187 in the form Lacus Constantiensis, came from the town of Konstanz at the outflow of the Rhine from the Obersee, whose original name, Constantia, was in turn derived from the Roman emperor, Constantius Chlorus (around 300 AD). Hence the French: Lac de Constance, Italian: Lago di Costanza, Portuguese: Lago de Constança, Spanish: Lago de Constanza, Romanian: Lacul Constanța, Greek: Λίμνη της Κωνσταντίας – Limni tis Konstantias. The Arabic, بحيرة كونستانس buħaira Konstans and probably the Turkish, Konstanz gölü, probably go back to the French form of the name. Even in Romance-influenced English the name "Lake Constance" gained a foothold and was then exported into other languages such as Hebrew: ימת קונסטנץ yamat Konstanz and Swahili: Ziwa la Konstanz. In many languages both forms exist in parallel e.g. Romansh: Lai da Constanza and Lai Bodan, Esperanto: Konstanca Lago and Bodenlago.
The poetic name, "Swabian Sea" was adopted by authors of the early modern era and the Enlightenment from ancient authors, possibly Tacitus. However, this assumption was based on an error (similar to that of the Teutoburg Forest and the Taunus): the Romans sometimes used the name Mare Suebicum for the Baltic Sea, not Lake Constance. In times when the Romans had located the so-called "Suebi", then an Elbe Germanic tribe near a sea, this was understandable. The authors of the Early Modern Period overlooked this and adopted the name for the largest lake in the middle of the former Duchy of Swabia, which also included parts of today's Switzerland. Today the name Swabian Sea (Schwäbisches Meer) is only used jocularly as a hyperbolic term for Lake Constance.
No Paleolithic finds have been made in the immediate vicinity of the lake, because the region of Lake Constance was covered for a long time by the Rhine Glacier. The discovery of stone tools (microliths) indicate that hunters and gatherers of the Mesolithic period (Middle Stone Age, 8,000-5,500 BC) frequented the area without settling, however. Only hunting camps have been confirmed. The earliest Neolithic farmers, who belonged to the Linear Pottery culture, also left no traces behind, because the Alpine foreland lay away from the routes along which they had spread during the 6th century BC. This changed only in the middle and late Neolithic when shore settlements were established, the so-called pile dwelling and wetland settlements, which have now been uncovered mainly on Lake Überlingen, the Constance Hopper and on the Obersee. At Unteruhldingen, such a pile dwelling village has been reconstructed and is now accessible as a museum.
Grave finds from Singen am Hohentwiel date to the beginning of the Early Bronze Age and shore settlements were repeatedly built during the Neolithic Period and the Bronze Age (up to 800 BC). During the following Iron Age the settlement history is interrupted. The settlement of the shore of Lake Constance during the Hallstatt period is attested by grave mounds, which today are usually found in forests where they have been protected from the destruction by agriculture. Since the late Hallstatt period, the peoples living on Lake Constance are referred to as the Celts. During the La Tène period from 450 AD, the population density decreases, as can be deduced partly due from the fact that no more grave mounds were built. For the first time, we have written reports on Lake Constance that have survived. Thus, we learn that the Helvetians settled by the lake in the south, the Rhaetians in the area of the Alpine Rhine Valley and the Vindelici in the northeast. The most important places on the lake were Bregenz (Celtic Brigantion) and today's Constance.
In the course of the Roman Alpine campaign of 16/15 BC, the Lake Constance region was integrated into the Roman Empire. During the campaign, there was also supposed to have been a battle on Lake Constance. The geographer, Pomponius Mela, makes the first mention in 43 AD of Lake Constance as two lakes - the Lacus Venetus (Upper Lake) and the Lacus Acronius (Untersee) - with the Rhine flowing through both. Pliny the Elder referred to Lake Constance as Lacus Brigantinus for the first time. The most important Roman site was Bregenz, which soon became subject to Roman municipal law and later became the seat of the Prefect of the Lake Constance fleet. The Romans were also in Lindau, but settled only on the hills around Lindau as the lakeshore was swampy. Other Roman towns were Constantia (Constance) and Arbor Felix (Arbon).
After the borders of the Roman Empire were drawn back to the Rhine boundary in the 3rd century BC, the Alemanni gradually settled on the north shore of Lake Constance and, later, on the south bank as well. After the introduction of Christianity, the cultural significance of the region grew as a result of the founding of Reichenau Abbey and the Bishopric of Constance. Under the rule of the Hohenstaufens, Imperial Diets (Reichstage) were held by Lake Constance. In Constance, too, a treaty was drawn up between the Hohenstaufen emperor and the Lombard League. Lake Constance also played an important role as a trading post for goods being traded between German and Italian states.
During the Thirty Years' War, there were various conflicts over the control of the region during the Lake War (1632-1648).
After the War of the Second Coalition (1798-1802), which also affected the region and during which Austrian and French flotillas operated on Lake Constance, there was a reorganisation of state relationships.
Lake Constance is located in the foothills of the Alps. The shore length of both main lakes is 273 kilometres long. Of this, 173 kilometres are located in Germany (Baden-Württemberg 155 km, Bavaria 18 km), 28 kilometres run through Austria and 72 kilometres through Switzerland. If the Upper and Lower Lakes are combined, Lake Constance has a total area of 536 km², the third largest lake in Central Europe by area after Lake Balaton (594 km²) and Lake Geneva (580 km²). It is also the second largest by water volume (48.5 km³) after Lake Geneva (89 km³) and extends for over 69.2 kilometres between Bregenz and Stein am Rhein. Its catchment area is around 11,500 square kilometres, and reaching as far south as Lago di Lei in Italy.
The area of the Obersee is 473 km². It extends from Bregenz to Bodman-Ludwigshafen for over 63.3 kilometres and is 14 kilometres wide between Friedrichshafen and Romanshorn. At its deepest point between Fischbach and Uttwil it is 251.14 metres deep.
The three small bays on the Vorarlberg shore have their own names: the Bay of Bregenz, off Hard and Fußach is the Bay of Fussach and, west of that is the Wetterwinkel. Farther west, now in Switzerland, is the Bay of Rorschach. To the north, on the Bavarian side, is the Bay of Reutin. The railway embankment from the mainland to the island of Lindau and the motorway bridge over the lake border the so-called Little Lake (Kleiner See), which is located between the Lindau village of Aeschach and the island.
The northwestern, finger-shaped arm of the Obersee is called Lake Überlingen. It is usually regarded as a separate lake, the boundary between the Obersee and Lake Überlingen runs approximately along the line between the southeast tip of Bodanrück (the Hörnle, which belongs to the town of Konstanz) and Meersburg. The Constance Hopper lies between the German and Swiss shores east of Konstanz.
The Obersee and Untersee are connected by the Seerhein.
The Untersee, which is separated from the Obersee and from its north-west arm, Lake Überlingen, by the large peninsula of Bodanrück, has an area of 63 km². It is strongly characterised and divided into different areas by end moraines, various glacial snouts and medial moraines. These various areas of the lake have their own names. North of Reichenau Island is the Gnadensee. West of the island of Reichenau, between the peninsula of Höri and the peninsula of Mettnau is Lake Zell. North of the Mettnau lies the Markelfinger Winkel. The drumlins of the southern Bodanrück continue along the bed of these northern parts of the lake. South of the Reichenau, from Gottlieben to Eschenz, stretches the Rheinsee ("Rhine Lake") with strong Rhine currents in places. Previously this lake part was named Lake Bernang after the village of Berlingen. On most of the maps the name of the Rheinsee is not shown, because this place is best suited for the name of the Untersee.
The present-day shape of Lake Constance has resulted from the combination of several factors:
Like any glacial lake, Lake Constance will also become silted up by sedimentation in the near future. This process can best be observed at the mouths of the larger rivers, especially that of the Alpine Rhine. The silting up process is accelerated by ever-increasing erosion by the Rhine and the associated reduction in the level of the lake.
The main tributary of Lake Constance is the Alpine Rhine. The Alpine Rhine and the Seerhein do not mix greatly with the waters of the lake and flow through the lakes along courses that change relatively little. There are also numerous smaller tributaries (236 in all). The most important tributaries of the Obersee are (counterclockwise) the Dornbirner Ach, Bregenzer Ach, Leiblach, Argen, Schussen, Rotach, Seefelder Aach, Stockacher Aach, Salmsacher Aach, the Aach near Arbon, Steinach, Goldach and the Old Rhine. The outflow of the Obersee is the Seerhein, which in turn is the main tributary of the Untersee. The most important tributary of the Untersee is the Radolfzeller Aach.
Because the Alpine Rhine brings with it drift from the mountains and deposits this material as sediment, the Bay of Bregenz will silt up in a few centuries time. The silting up of the entire Lake Constance is estimated to take another ten to twenty thousand years.
The outflow of the Untersee is the High Rhine with the Rhine Falls at Schaffhausen. Both the average precipitation of 0.45 km³/a and evaporation which averages 0.29 km³/a cause a net change in the level of Lake Constance that is less when compared to the influence of the inflows and outflows. Further quantities of lake water are extracted by municipal waterworks around the lake and the water company of Bodensee-Wasserversorgung.
In Lake Constance there are ten islands that are larger than 2,000 m².
By far the largest is the island of Reichenau in the Untersee, which belongs to the municipality of Reichenau. The former abbey of Reichenau is a UNESCO World Heritage Site due to its three early and highly medieval churches. The island is also known for its intensive cultivation of fruit and vegetables.
The island of Lindau is located in the east of the Obersee, and is the second largest island. On it is the old town and main railway station of Lindau.
The third largest island is Mainau in the southeast of Lake Überlingen. The owners, the family of Bernadotte, have set up the island as a tourist attraction and created botanical gardens and wildlife enclosures.
Relatively large, but uninhabited and inaccessible because of their status as nature reserves, are two islands off the Wollmatinger Ried: the Triboldingerbohl which has an area of 13 ha and Mittler or Langbohl which is just 3 ha in area.
Smaller islands in the Obersee are:
In the Untersee are:
In Lake Constance there are several peninsulas which vary greatly in size:
The shores of Lake Constance consist mainly of gravel. In some places there are also sandy beaches, such as the Rohrspitz in the Austrian section of the lake, the Langenargen and Marienschlucht.
According to the data of the International Water Protection Commission for the Lake Constance, the approximate shore length is 273 km (see Coastline paradox). The inflow of water is constantly changing, mainly due to rain and the snow melt in the Alps. Its average surface area is approximately 395 m above NN (in Switzerland the absolute value is slightly higher in m above sea level). The more or less regular seasonal fluctuations in the water level also lead to slight variations in shore length and differences in the shore zone habitats (depending on high and low water).
The climate of the Lake Constance area is characterised by mild temperatures with moderate gradients, thanks to the balancing and retarding effect of the large body of water. However, due to the year-round influence of föhn winds which causes frequent fog in winter and close weather in summer, it is considered a stressful climate.
Lake Constance is also considered to be a risky and challenging lake for water sports because of the danger of gusty winds which can whip up waves as the weather changes suddenly. The most dangerous wind is the föhn, a warm down-slope wind from the Alps, which spreads out across the water, especially through the Alpine Rhine Valley and can generate waves several metres high.
Similarly dangerous for those unfamiliar with the area, are the sudden stormy gusts of wind during summer thunderstorms. They constantly claim victims from the water sports fraternity. During a thunderstorm in July 2006, waves reached heights of up to 3.50 metres.
For these reasons, there is a storm warning system in all three neighbouring countries. For storm warning purposes, Lake Constance is divided into three warning regions (west, centre and east). Warnings can be issued for each region independently. A "high winds" warning will be issued when squalls are expected of between 25 and 33 knots or registering force 6 to 8 on the Beaufort scale. A gale warning announces the likelihood of gale-force winds, i.e. those at speeds as of 34 knots or more or force 8 on the Beaufort scale. In order to issue these warnings, orange-coloured flashing lights are installed around the lake, which flash at a frequency of 40 times per minute for high winds or 90 times per minute for gales. It can happen that, due to the differently regulated responsibilities and assessments, a gale warning is issued on the Swiss side of the Obersee, but not on the German or Austrian shores, and vice-versa. Ships and ferries on Lake Constance indicate a gale warning by hoisting a Sturmballon ("storm ball") up the mast.
A one-hundred year event is the freezing over of Lake Constance, when the Untersee, Lake Überlingen and the Obersee are completely frozen over so that people can safely cross the lake on foot. The three last so-called Seegfrörne events were in 1963, 1880 and 1830.
Certain parts of the lake freeze over more frequently, mainly due to their shallow depth of water and shelter, as is the case, for example, of the so-called Markelfinger Winkel between the municipality of Markelfingen and the Mettnau peninsula.
Lake Constance is the only area in Europe where no borders exist, because there is no legally binding agreement as to where the borders lie between Switzerland, Germany and Austria. However, Switzerland holds the view that the border runs through the middle of the lake, Austria is of the opinion that the contentious area belongs to all the states on its banks, which is known as a "condominium", and Germany holds an ambiguous opinion. Legal questions pertaining to ship transport and fishing are regulated in separate treaties.
Naturally, disputes arise. One concerns a houseboat which was moored in two states (ECJ c. 224/97 Erich Ciola); another concerns the rights to fish in the Bay of Bregenz. In relation to the latter, an Austrian family was of the opinion that it alone had the right to fish in broad portions of the bay. However, this was accepted neither by the Austrian courts nor by the organs and courts of the other states.
Until the 19th century, Lake Constance was a natural lake. Since then, nature has been heavily influenced by clearing and the cultivation of much of the land around its shores. However, some near-natural areas have been largely conserved, especially in the nature reserves, or were re-naturalised. As a result, the Lake Constance region has some unusual ecological features. These include the large forested area on the Bodanrück, the occurrence of marsh gentian and orchids of the genera Dactylorhiza and Orchis in the Wollmatinger Ried, and the Siberian iris (Iris sibirica) in the Eriskircher Ried, which was therefore given its own name. One unique species among the local flora is the Lake Constance forget-me-not (Myosotis rehsteineri), whose habitat is restricted to undisturbed beaches of lime trees.
Lake Constance is also the home of numerous species of birds, many of which next in its nature reserves, such as the Wollmatinger Ried or the Mettnau peninsula. 412 species have so far been recorded..
The ten most common breeding bird species at Lake Constance according to a 2000-2003 survey in descending order are the: blackbird, chaffinch, starling, robin, chiffchaff, greenfinch, and blue tit.
In spring, the Lake Constance is an important breeding ground, especially for the coot and great crested grebe. Typical waterfowl include the: shoveler, goldeneye, goosander, pochard, grey heron, pintail, tufted duck and mallard.
In December 2014, 1,389 cormorant were counted. The International Lake Constance Fishery Association (IBF) estimates the food requirements of the cormorants on Lake Constance at 150 tonnes of fish annually.
Lake Constance is an important overwintering area for around 250,000 birds. annually. Bird species such as the dunlin, the curlew and the lapwing overwinter at Lake Constance. In the middle of December 2014 there were 56,798 heron, 51,713 coot and 43,938 pochard. In November/December are about 10,000 to 15,000 red-crested pochard and 10,000 great crested grebe on Lake Constance..
During migration in late autumn there are also numerous loon on the lake (black-throated and red-throated loon, as well as a few great northern divers). Lake Constance is also very important as a staging post during the bird migration. Bird migration is often inconspicuous and most noticeable when there are special weather conditions that make day migration obvious. Only where there is a prolonged spell of widespread low-pressure is it common to observe the congestion of large groups of migratory birds. This can often be observed in autumn on the Eriskircher Ried on the northern shore of Lake Constance. This is where broad front migration converges on the lake and birds then try to move along the shore towards the northwest. The importance of Lake Constance as an important area for resting and overwintering is underlined by the Max Planck Institute for Ornithology's Radolfzell Bird Observatory (Vogelwarte Radolfzell), which is the bird ringing centre for the German states of Bavaria, Baden-Württemberg, Berlin, Rhineland-Palatinate and the Saarland as well as for Austria, and which researches bird migration.
Around 45 species of fish live in Lake Constance. The annual haul from fishing is 1.5 million kg. Unusual species occurring here considering the location of the lake are the whitefish (Coregonus spec.) and the Arctic char (Salvelinus alpinus). Fish that are important for the fishing industry are:
The Bodenseefelchen (Coregonus wartmanni), which was named after Lake Constance due to the great numbers found there, is often prepared whole or as a fillet, in the style of the miller's wife (nach Müllerin Art), in local fish restaurants in a similar way to other trout It is also often served smoked.
The endemic species, formerly found in Lake Constance, the Bodensee-Kilch (Coregonus gutturosus) and deepwater char (Salvelinus profundus) are now assumed to be extinct.
For many years non-native species have settled in the Lake Constance ecosystem and, in some cases, endangered or threatened native flora and fauna. At Lake Constance, non-native species have been increasing annually. Several have been transported from other waterbodies as 'blind passengers' on the outside of boats, life jackets, anchor chains or ropes or diving gear. Others have immigrated from the Black Sea or the Danube since the opening of the Main-Danube Canal. Others have been deliberately introduced.
Even the rainbow trout (Oncorhynchus mykiss) is not a native fish. It was introduced into Lake Constance around 1880 for economic reasons to enhance the local fauna.
Among the foreign species of animal in Lake Constance are the zebra mussel (Dreissena polymorpha) which, since the 18th century, has spread from the Black Sea region across most of Europe and was carried into Lake Constance between 1960 and 1965. After a huge increase in numbers during the 1980s in the Rhine and large lakes, this species is now in retreat today. The zebra mussel causes problems because, among other things, it blocks water extraction pipes. In addition, the species can be a disaster for domestic shellfish, because it competes for their food. Today, according to the Institute for Lake Research (Institut für Seenforschung, ISF), the zebra mussel is also an important food for overwintering waterfowl. In fact, the number of overwinterers has more than doubled in around 30 years.
The killer shrimp (Dikerogammarus villosus) has spread since 2002 from two sections of shoreline near Hagnau and Immenstaad, over the whole Lake Überlingen (2004), the whole of the Obersee (2006) and almost the whole Lake Constance and Rheinsee shore (2007) aus. As its name implies, it is a voracious burglar of fish larvae and fish eggs.
The most recent example is the little opossum shrimp (Limnomysis benedeni), only six to eleven millimeters long, which was found in 2006 in the Vorarlberg region of Hard, and can now be found almost all over Lake Constance. It comes from the waters around the Black Sea. It was presumably first transported by ships up the Danube before it spread into the Rhine river system and entered Lake Constance. The opossum shrimp, which occurs in many places in shoals of several million in winter, are already an influential link in the food chain in Lake Constance. They consume dead animal and plant material as well as phytoplankton, but are also eaten by fish themselves.
Today, in western Lake Constance are found: the North American spinycheek crayfish (Orconectes limosus), which was introduced into European waters in the mid-19th century to increase the yield, occasionally the Chinese mitten crab (Eriocheir sinensis), and in the lake's tributaries, the signal crayfish (Pacifastacus leniusulus). As these species of large crayfish are immune to crayfish plague, but spread the pathogen, they are a great danger to native species such as noble crayfish, white-clawed crayfish or stone crayfish. The animals are often undemanding, multiply rapidly and lead predatory lives, thus also posing a threat to various small species of fish. The ISF has been systematically researching the subject since 2003.
After a collision with the Stadt Zürich in 1864 the wreck of the Jura has lain on the lake bed at a depth of 45 metres off the Swiss shore. In the early 20th century four ships were sunk in the Obersee after being taken out of service: in 1931 the Baden, formerly the Kaiser Wilhelm, in 1932 the Helvetia, in 1933 the Säntis and in 1934 the Stadt Radolfzell. The hull of the burnt-out Friedrichshafen was scuttled in 1944 off the mouth of the Argen in 100 to 150 metres of water.
The tourism and leisure industry is an important factor for this region. Overnight stays reached 17,56m visitors in 2012 with an turnover of about 1.9bn Euros. The same amount comes from the 70 million daily visitors that visit Lake Constance each year.
This region is known for sightseeing, water-sports, winter-sports like Skiing, summer-sports like Swimming (sport), Sailing and recreation. It is also one of the few places where modern Zeppelin airships operate and 12-14 people can take a trip above the lake around various points of interests.
The lake and the region around it have a substantial touristic infrastructure as well as many attractions and points of interests. Important are especially cities like Konstanz, Überlingen, Meersburg, Friedrichshafen, Lindau and Bregenz as they are the big hubs for boating tourism. The main tourism attractions are places like Rhine Falls, one of the three biggest waterfalls in Europe, the Mainau Island and Reichenau Island (UNESCO world heritage), the pilgrimage church Birnau, castles and palaces like Salem Abbey, Meersburg Castle as well as another UNESCO world heritage site, the Pfahlbaumuseum Unteruhldingen (German for 'Stilt house museum).
In the east of the lake, the Alps are reaching almost to it thus allowing a great view over the lake. The Pfänderbahn goes from top of the mountain right down, next to the lake in Bregenz.
Biking around the lake is also possible on the 261 km long trail called "Bodensee-Radweg". It brings its visitors to the most interesting sites and goes around the whole lake. Nevertheless, various shortcuts via ferries allow shorter routes and the trail is suitable for all levels. Note: There is also a trail that goes by the name "Bodensee-Rundweg". This road was intended for pedestrians so biking is sometimes not suitable or allowed.
Furthermore, Lake Constance is the location for the annual Bregenzer Festspiele, a well known arts festival that also takes place on a floating stage in Bregenz. Opera and music performances generally tend to come from popular pieces and among contributors are top music bands like the Vienna Symphony Orchestra.
From the entry of the Rhine, on the northern or right shore:
From the entry of the Rhine, on the southern or left shore:
The lake was frozen in the years 1077 (?), 1326 (partial), 1378 (partial), 1435, 1465 (partial), 1477 (partial), 1491 (partial?), 1517 (partial), 1571 (partial), 1573, 1600 (partial), 1684, 1695, 1709 (partial), 1795, 1830, 1880 (partial), and 1963.
Approximately 1,000 tonnes (1,100 short tons) of fish were caught by 150 professional fishermen in 2001 which was below the previous ten year average of 1,200 tonnes (1,300 short tons) per year. The Lake Constance trout (Salmo trutta) was almost extinct in the 1980s due to pollution, but thanks to protective measures they have made a significant return. Lake Constance is the home of the critically endangered species of trout Salvelinus profundus, and formerly also the now extinct Lake Constance whitefish (Coregonus gutturosus).