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The summit of the Brocken, showing the transmitters
|Elevation||1,141 m (3,743 ft)|
|Prominence||856 m (2,808 ft)|
The summit of the Brocken, showing the transmitters
|Elevation||1,141 m (3,743 ft)|
|Prominence||856 m (2,808 ft)|
The Brocken, also sometimes referred to as the Blocksberg, is the highest peak of the Harz mountain range and also the highest peak of Northern Germany; it is located near Schierke in the German state of Saxony-Anhalt between the rivers Weser and Elbe. Although its altitude of 1,141 metres (3,743 ft) is below alpine dimensions, its microclimate resembles that of mountains of about 2,000 m (6,600 ft). The peak above the tree line tends to have a snow cover from September to May, and mists and fogs shroud it up to 300 days of the year. The mean annual temperature is only 2.9 °C (37.2 °F). It is the easternmost mountain in northern Germany; travelling east in a straight line, the next prominent elevation would be in the Ural Mountains in Russia.
The Brocken has always played a role in legends and has been connected with witches and devils; Johann Wolfgang von Goethe took up the legends in his play Faust. The Brocken spectre is a common phenomenon on this misty mountain, where a climber's shadow cast upon fog creates eerie optical effects.
Today the Brocken is part of the Harz National Park and hosts a historic botanical garden of about 1,600 alpine mountain plants. A narrow gauge steam railway, the Brocken Railway, takes visitors to the railway station at the top on 1,125 m (3,691 ft).
FM-radio and television broadcasting make major use of the Brocken. The old television tower, the Sender Brocken, is now used as hotel and restaurant. It also has an observation deck, open to tourists.
The Brocken rises over the Harz National Park in the borough of Wernigerode, whose main town lies about 12 kilometres east-northeast of the mountain. The state boundary with Lower Saxony runs past the Brocken some 2 km to the west. At the southeastern foot of the Brocken lies the spa resort of Schierke.
Somewhat to the north below the summit of the Brocken is a reservoir, the Brockenteich, constructed in 1744. On or near the mountain are the source areas of the rivers Bode, Ecker, Ilse and Oder. The rounded summit of the Brocken is treeless, but vegetated with dwarf shrubs.
Before 1989 the height of the Brocken was recorded in almost all the relevant maps and books as . A survey of the summit at the beginning of the 1990s based on the current reference system, however, gave the height as just . In order to provide a reference point for the old data, in the mid-1990s granite boulders were set on the highest point of the Brocken, which not only matched the old given height, but exceeded it by about a metre. A bench mark of "1142 m" was recorded on the summit stone. This height on the upper plate refers to the line on the lower plate.
From a geological point of view the Brocken and its surrounding terrain, the Brocken massif, consists mainly of granite (called Brocken granite), an igneous rock. The granitic plutons of the Harz - the Brocken, Ramberg and Oker plutons - emerged towards the end of the Harz mountain-building phase of the Upper Carboniferous, about 300 million years ago. First, alkaline magma intruded into the overlying sediments, crystallized out and formed gabbro and diorite massifs, such as the Harzburg gabbro. A little later, silica-rich granitic magma rose, some intruding into voids and gaps in the older rocks, but most being created by the melting of existing sediments. On the boundary between granite and host rock, the so-called contact zone, a great variety of transitions may be seen. For example, the summit of the Achtermannshöhe consists of contact-metamorphosed hornfels of the contact zone that, here, lies over the Brocken granite. The subsequent erosion of the Harz mountains that followed the uplifting of the Harz during the Upper Cretaceous saw the disappearance of the protective hornfels summit, thus exposing the granite that had crystallized underground during the Upper Carboniferous. The alleged hardness of Brocken granite is not the reason for the height of the mountain, but the geological fact that it was well protected by its weather-resistant hornfels crest for a long time before erosion set in.
Only in recent geological times, since the tertiary period, did the typical, rounded, spheroidal weathering of granite outcrops and granite boulders of the Brocken take place. Such blockfields are very rare in Central Europe outside the Alps and are subject to conservation measures. They originated mainly under periglacial conditions, i.e. during the course of the ice ages, and their retreat. Today's blockfields of Brocken granite, as well as other rocks in the Harz National Park, particularly in the Oder valley, are therefore at least 10,000 years old. Physical weathering, such as frost shattering, has played a key role in their formation, resulting in giant piles of loosely-stacked rocks. In 2006, the granite blockfields of the Brocken, together with 76 other interesting geotopes, were designated as a "National Geotope".
The Brocken is a place of extreme weather conditions. Due to its exposed location in the north of Germany its peak lies above the natural tree line. The climate on the Brocken is like that of an alpine location or even that of Iceland's 1,600 – 2,200 m zone. This is due to its short summers and very long winters, with many months of continuous snow cover, strong storms and low temperatures even in summer.
Due to its significant height difference compared with the surrounding terrain the Brocken has the highest precipitation of any point in northern central Europe, with an average annual precipitation (1961–1990) of 1,814 millimetres. Its average annual temperature is 2.9 °C.
The Brocken weather station has recorded the following extreme values:
The harsh climate of the Brocken makes it a habitat for rare species. The mountain's summit is a subalpine zone with flora and fauna almost comparable to those of north Scandinavia and the Alps. The Brocken is the only mountain in Germany's Central Uplands whose summit lies above the treeline, so that only very small spruce grow there and much of it is covered by a dwarf shrub heathland. In the Brocken Garden, established in 1890, flora is nurtured by National Park employees and visitors are allowed to view it as part of regular guided tours. The garden does not just display plants from the Brocken, but also high mountain flora from other regions and countries.
Amongst the typical species of the Brocken that are rarely if ever found elsewhere in North Germany and which occur above about Alpine Pasqueflower known as the Brocken flower or Brocken anemone (Pulsatilla alpina subsp. alba), hawkweeds like the Brocken Hawkweed (Hieracium negrescens) and the Alpine Hawkweed (Hieracium alpinum), vernal grasses (Anthoxanthum), the Lady's Mantle (Alchemilla), the Tormentil (Potentilla tormentilla), the Alpine Clubmoss (Diphasiastrum alpinum), the lichens, Iceland Moss (Cetraria islandica) and Reindeer Lichen (Cladonia rangiferina). The Crowberry is also referred to here as the Brocken Myrtle (Brockenmyrte).are the variant of the
The Viviparous Lizard occurs on the Brocken in a unique, dark-colored variant, Lacerta vivipara aberr. negra. The common frog (Rana temporaria) can also be found here. Insects are very numerous. There are many beetles including ground beetles such as Amara Erratica, and hundreds of species of butterfly. The Cabbage White here only produces one generation per year compared with two in the lowlands.
The first ascent of the Brocken was documented in 1572 by the physician and botanist, Johannes Thal from Stolberg, who in his book Sylva Hercynia described the flora of the mountain area. In 1736 Count Christian Ernst of Stolberg-Wernigerode had the Wolkenhäuschen ("Clouds Cabin") erected at the summit, a small refuge that is still preserved. He also had a mountain lodge built at the southern slope, named Heinrichshöhe after his son Henry (Heinrich) Ernest. The first inn on the Brocken summit was built around 1800.
Between 1821 and 1825 Carl Friedrich Gauss used the line-of-sight to the Inselsberg within the Thuringian Forest and the Hoher Hagen mountain near Göttingen for triangulation in the course of the geodesic survey of the Kingdom of Hanover. A measurement carried out by the military staff of Prussia in 1850 found the Brocken's height to be at its present level of 1141.1 metres. After the first Brocken lodge had been destroyed by a fire, a new hotel opened in 1862. The Brocken Garden, a botanical garden, was laid out in 1890 by Professor Albert Peter of Göttingen University on an area of 4,600 m2 (50,000 sq ft) granted by Count Otto of Stolberg-Wernigerode. It was Germany's first Alpine garden.
The narrow gauge Brocken Railway was opened on 27 March 1899. Brocken station is one of the highest railway stations in Germany lying at a height of . Its gauge is 1000 mm. In 1935 the Deutsche Reichspost made the first television broadcast from the Brocken using a mobile transmitter and, in the following year, the first television tower in the world was built on the mountain; carrying the first live television broadcast of the Summer Olympics in Berlin. The tower continued functioning until September 1939, when the authorities suspended broadcasting on the outbreak of World War II.
During an air attack by the U.S. Air Force on 17 April 1945 the Brocken Hotel and the weather station were destroyed by bombing. The television tower, however, survived. From 1945 until April 1947, the Brocken was occupied by US troops. As part of the exchange of territorial (specified at the Yalta Conference) the mountain was transferred to the Soviet occupation zone. Before the Americans left the Brocken in 1947, however, they disabled the rebuilt weather station and the television tower.
The ruins of the Brocken Hotel were blown up in 1949. From 1948 to 1959 part of the Brocken was reopened to tourists. Although a pass was required, these were freely issued. From August 1961 the Brocken, which lay in East Germany's border zone, immediately adjacent to West Germany, was declared an out-of-bounds area and was therefore not open to the public. Extensive military installations were built on and around the summit was exploited. The security of the area was the responsibility of the border guards of the 7th Schierke Border Company, which was stationed in platoon strength on the summit. For accommodation, they used Brocken railway station. The Soviet Red Army also used a large portion of territory. In 1987, the goods traffic on the Brocken Railway ceased due to poor track conditions.
The Brocken was extensively used for surveillance and espionage purposes. On the summit were two large and powerful listening posts. One belonged to Soviet military intelligence, the GRU and was also the westernmost outpost of Moscow; the other was Department III of the Ministry for State Security in the GDR. The listening posts were codenamed "Yenisei" and "Urian". Between 1973 to 1976 a new modern television tower was built for the second channel of the GDR-TV. Today it is used by the public Zweites Deutsches Fernsehen (ZDF) television network. The Stasi (East German secret police) used the old tower until 1985, when they moved to a new building – now a museum. To seal the area, the entire Brocken plateau was then surrounded by a concrete wall, built from 2,318 sections, each one 2.4 tons in weight and 3.60 metres high. The whole area was not publicly accessible until December 3, 1989. The wall has since been dismantled, as have the Russian barracks and the domes of their listening posts. Today the old tower beside the lodge again is home to a weather station of the Deutscher Wetterdienst.
After the fall of the Berlin Wall on 3 December 1989 the Brocken was again open to the public during a demonstration walk. With German reunification there was a gradual reduction in border security facilities and military installations from 1990. The last Russian soldier left the Brocken on 30 March 1994. The Brocken summit was renaturalised at a cost of millions of euros. It is now a popular tourist destination for visitors to the Harz.
As a protected area since 1939 and due to the decades of restricted access the unique climate of the Brocken provided outstanding conditions. The massif is partly still covered with primary forest extremely rare in Germany. It provides perfect conditions for endangered and nearly extinct species like the Eurasian Lynx, Wildcats and Capercaillies. The Brocken was therefore declared part of a national park in 1990.
The widespread use of the name "Brocken" did not occur until towards the end of the Middle Ages. Hitherto the region had just been described as the Harz. This was primarily because, until then, the focus had been mining. The first record of a placename that resembles the present name of the mountain goes back, however, to the year 1176 when it is referred to as broke in the Saxon World Chronicle (Sächsische Weltchronik). Another early written reference to the mountain, this time as the Brackenberg, appears in 1490 in a letter from Count Henry of Stolberg. Other early documented names of the Brocken were, in 1401, the Brockenberg, in 1424 the Brocberg, in 1495 mons ruptus (Latin), in 1511 the Brogken and Brockin, in 1531 the Brogken, in 1540 the Brokenberg and, in 1589, the Brackenberg. In Old Saxon-Germanic times, a large portrait of Wodin is supposed to have been found on the Brocken. In addition, animal and human sacrifices were offered by the Saxons to their supreme god, Odin, on the blockfields of the summit until they renounced them as part of their baptismal vows when Christianity spread to the region under Charles the Great.
As far as the origin of the name is concerned, there are several interpretations: In the town records (Stadtbuch) of Osterwieck an entry for the Brocken was found in the year 1495 under the Latin name of mons ruptus, which means "broken hill". Its Low German name, broken, as the mountain had become named in 1176 in the Saxon World Chronicle and also in English, means "broken". On the one hand, this explanation of its meaning can be attributed to the fact that the two mountains, "Kleiner Brocken" and "Großer Brocken", were formed by the breakup of a single massif. On the other hand, its meaning may refer to the serious erosion of the mountain. In other words it refers to the fact that the Brocken was eroded or "broken down" to its present size.
But the most likely derivation of the name comes from the shape of the mountain as a whole. A Brocken in German is a large, shapeless mass. The size of the Brocken may thus have given it its name. Since the term "block" has a similar meaning, this could also be the derivation of its alternative name, the Blocksberg. The true origin of the name Blocksberg, however, should not be seen as "block" in the sense of "mass", but rather the German word Block (as in block of wood) in witchcraft.
Another theory holds that the name "Brocken" is derived from Bruch, a word used in northern Germany for bog or moor, which commonly used to be spelt as Bruoch or Brok. It is however doubtful that this fact was primarily responsible for its name. Another possibility is that its name is derived from the fields of boulders strewn over the summit and the slopes of the mountain. This derivation for the name Brocken is, however, unlikely because such blockfields are also found on other mountains in the Harz. Moreover, the regions concerned were hardly known at the time when the term was used. Another presumption is based on the reference in a letter written in 1490 by Count Henry of Stolberg-Wernigerode, where he uses the term Brackenberg. However the suggestion that this referred to old, unusable timber, which was called Bracken, is disputed.
At the summit is the Brockenhaus with a museum on the history of the mountain and the Brocken Garden (a botanical garden), which is managed by the Harz National Park. In addition there are restaurants and the Brocken Hotel, which is run by the Brocken publican (Brockenwirt), Hans Steinhoff. Important publicans in the past included Johann Friedrich Gerlach from 1801 to 1834, Carl Eduard Nehse between 1834 and 1850, who brought out a map of the Brocken in 1849 and the Brocken Register (Brockenstammbuch) in 1850, as well as Rudolf Schade from 1908 to 1927, who considerably increased the repute and the size of guest facilities on the Brocken.
The area around the Brocken is especially popular with hikers. The Goethe Way (Goetheweg) is a well known trail that leads to the summit of the Brocken. It is named after Johann Wolfgang von Goethe, who more-or-less followed this route in 1777. Many paths lead to the local towns of Schierke, Braunlage and Sankt Andreasberg. The 100 km long Harz Witches' Path also runs from the Brocken eastwards to Thale and westwards via Torfhaus and Altenburg to Osterode. The "Bad Harzburg Devil's Path" runs from the Brocken to Bad Harzburg. Mountain bikers also use the trails.
From Schierke from a metalled road leads to the summit, which is used by horse-drawn wagons, as well as touring and racing cyclists. Because of the situation in the National Park, vehicles with internal combustion engines are only allowed with special permission.
Worthy of special mention is the bearer of the Badge of Honour of Saxony-Anhalt, Benno Schmidt (b. 1932) - also known Brocken Benno - of Wernigerode, who has climbed the mountain since 1989, almost daily, with more than 6,000 ascents (as at 21 May 2010) and whose feat has been registered in the Guinness Book of World Records.
Two well-known running events pass over the Brocken: the Ilsenburg Brocken Run (beginning of September, 26 kilometres, of which 12 kilometres uphill, has taken place since the 1920s) and the Brocken Marathon which is part of the Harz Mountain Run with its start and finish south of Wernigerode. Both start in the valley, climb the Brocken and return. The most challenging part in each case is the last four kilometres to the Brocken summit, for which in both races, a separate mountains classification is given. This section is a concrete slab track with a steady incline of about 20% and the runners are exposed above the tree line, often to a sharp, icy wind. Of the just under 1,000 people who usually achieve it, only 50 negotiate this section without stopping to walk.
Since 2004, the Brocken Challenge, an ultra marathon 84 kilometres long from Göttingen to the Brocken summit, has been staged in February each year. The proceeds from this event go to charity. The runs are conducted in accordance with the rules of the National Park.
The 87 kilometre-long "Brocken Climb" from Göttingen to the Brocken has taken place annually since 2003. More than 300 people take part in these two-day hikes in June.
In early May each year the Brunswick-Brocken Ultra Run takes place with 2x75 km legs spread over two days. The participants run from Brunswick to Schierke, cross the Brocken, overnight in Schierke and run back again the next day. Overall, it is therefore a 150 kilometre race.
Since the 1930s various radio and television transmitters have been erected on the Brocken, see Brocken Transmitter.
Brocken House (Brockenhaus), the modern information centre for the Harz National Park, is located in the converted "Stasi Mosque" (Stasi-Moschee), a former surveillance installation for the Ministry for State Security. The historic antenna equipment in the dome may be visited. Behind the building is checkpoint no. 9 on the Harzer Wandernadel hiking trail network.
The extreme weather conditions of the Brocken are of special meteorological interest. From 1836 the Brockenwirt, who also ran the guest house and restaurant, kept meteorological records. The first weather station on the Brocken was built in 1895. Technically poor and too small, it was partially demolished in 1912 and replaced with a large stone construction, the Hellman Observatory, that was not completed until the First World War. In 1917 the academic and nature lover, George Grobe, took over the running of the observation post, his daughter supporting him until his death in 1935. Today's weather station started life in 1939. Measurements were interrupted at the end of the Second World War as a result of military bombardment, but began again in 1947. On 16 March 2010 the Brocken Weather Station became a climate reference station to provide uninterrupted, long-term climatic observations.
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