
The Calenberg is a hill in central Germany in the
Leine depression near
Pattensen
Pattensen () is a town in the district of Hanover, in Lower Saxony, Germany. It is situated approximately south of Hanover.
Geography
Pattensen is located in the historic landscape Calenberg Land between the Leine and the Deister hills. The a ...
in the municipality of Schulenburg. It lies 13 km west of the city of
Hildesheim
Hildesheim (; or ; ) is a city in Lower Saxony, in north-central Germany with 101,693 inhabitants. It is in the district of Hildesheim (district), Hildesheim, about southeast of Hanover on the banks of the Innerste River, a small tributary of t ...
in south
Lower Saxony
Lower Saxony is a States of Germany, German state (') in Northern Germany, northwestern Germany. It is the second-largest state by land area, with , and fourth-largest in population (8 million in 2021) among the 16 ' of the Germany, Federal Re ...
on the edge of the
Central Uplands
The Central UplandsDickinson (1964), p.18 ff. (N.B. In German die ''Mittelgebirge'' (plural) refers to the Central Uplands; das ''Mittelgebirge'' refers to a low mountain range or upland region (''Mittel'' = "medium" and ''-gebirge'' = "range").) ...
. It is made from a chalk marl slab (''Kalkmergelbank''), has a height of and was formed almost 100 million years ago at the beginning of the
Upper Cretaceous
The Late Cretaceous (100.5–66 Ma) is the more recent of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''cret ...
series in
Cenomanian
The Cenomanian is, in the International Commission on Stratigraphy's (ICS) geological timescale, the oldest or earliest age (geology), age of the Late Cretaceous epoch (geology), Epoch or the lowest stage (stratigraphy), stage of the Upper Cretace ...
stage. The Calenberg became historically important as a result of the fort, stronghold and castle built as the main residence of the
House of Hanover
The House of Hanover ( ) is a European royal house with roots tracing back to the 17th century. Its members, known as Hanoverians, ruled Hanover, Great Britain, Ireland, and the British Empire at various times during the 17th to 20th centurie ...
.
Etymology
The syllables ''Kal'', ''Kalen-'', ''Calen-'' in the word ''Calenberg'' are derived from the word ''kal'' in the
Middle High German
Middle High German (MHG; or ; , shortened as ''Mhdt.'' or ''Mhd.'') is the term for the form of High German, High German language, German spoken in the High Middle Ages. It is conventionally dated between 1050 and 1350, developing from Old High ...
and
Middle Low German
Middle Low German is a developmental stage of Low German. It developed from the Old Saxon language in the Middle Ages and has been documented in writing since about 1225–34 (). During the Hanseatic period (from about 1300 to about 1600), Mid ...
languages and mean ''kahl'' i.e. "bare", "stripped", "unwooded". Name formations using ''Kal'', ''Kalen'' or ''Calen'' could refer to its geological base (''rock, stone''). The syllable ''-berg'' goes back to the
Old High German
Old High German (OHG; ) is the earliest stage of the German language, conventionally identified as the period from around 500/750 to 1050. Rather than representing a single supra-regional form of German, Old High German encompasses the numerous ...
word ''berg'', to the Middle High German ''berc(g)'', to the Middle Low German ''berch'' and the colloquial word ''barch''. It can mean "mountain", "hill" or "knoll". So the word ''Calenberg'' means something like ''kahler Berg'' or "bare hill".
The syllable ''Klei'' in the word ''Klei-Kamp'' comes from the word ''klei'' in Old High German and Middle Low German and to the
dialectic word ''klaibodden'' and means: ''heavy loam soil, heavy soil, thick clay.'' The syllable ''-Kamp'' goes back to the Old High German word ''champf '' as well as the Middle Low German and dialectic word ''kamp'' and means an "enclosed piece of land". From the middle of the 17th century onwards it was also used for large plots of private land even if they were unenclosed.
The syllable ''Kälber'' in the word ''Kälber-Kamp'' comes from the word ''kalver'' in Middle Low German and the colloquial word ''kälwer'' and means "calves". Fields known as ''Kälber'' were used to graze calves.
Geography
The Calenberg lies in the protected landscape of the Calenberg Leine Valley (''Calenberger Leinetal''). It is bordered to the north by the
Leine
The Leine (; Old Saxon ''Lagina'') is a river in Thuringia and Lower Saxony, Germany. It is a left tributary of the Aller and the Weser and is long.
The river's source is located close to the town of Leinefelde in Thuringia. About downriver ...
, to the west and south by the state road, ''
Landesstraße
''Landesstraßen'' (singular: ''Landesstraße'' ) are roads in Germany and Austria that are, as a rule, the responsibility of the respective German or Austrian federal state. The term may therefore be translated as "state road". They are road ...
'' 460, and to the east by gravel ponds. Its northern slopes are used for agriculture by the Calenberg Estate (''Hausgut Calenberg'') belonging to the
House of Hanover
The House of Hanover ( ) is a European royal house with roots tracing back to the 17th century. Its members, known as Hanoverians, ruled Hanover, Great Britain, Ireland, and the British Empire at various times during the 17th to 20th centurie ...
, in the south are the ditches, ramparts and ruins of Calenburg Castle (''Burg Calenberg'') and several old workers' cottages belonging to the Calenberg Estate. The area of Calenberg Castle and the northern workers' cottages are protected as a monument and is referred to on maps as Old Calenberg (''Alt Calenberg''). In 2008 Hanover Region surveyed ''Alt Calenberg'' and its trees, each tree was numbered and marked after the estate had felled trees here in 2007-08.
South of ''Alt Calenberg'', on the state road, L 460, are the houses of
Lauenstadt. This settlement was founded in 1327 as a town, but never developed into a town. In 1613 it was ranked last in the list of towns in the
Principality of Calenberg
The Principality of Calenberg was a dynastic division of the House of Welf, Welf Duchy of Brunswick-Lüneburg established in 1432. Calenberg was ruled by the House of Hanover (from the Principality of Lüneburg) from 1635 onwards; the princes re ...
. By about 1900 markets were held north of Lauenstadt at which everyday items were sold in open stalls.
Geology
North of the moat of Calenberg Castle, in addition to the former workers' cottages, was an old quarry, which supplied stone for the foundation walls and fortifications of
Calenberg Castle. The quarry exposed four metres of the
Cenomanian
The Cenomanian is, in the International Commission on Stratigraphy's (ICS) geological timescale, the oldest or earliest age (geology), age of the Late Cretaceous epoch (geology), Epoch or the lowest stage (stratigraphy), stage of the Upper Cretace ...
rock of which the Calenberg is made. The strata consist of plate-like, gray-white
limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science) ...
, the upper layers being quite rich in
fossil
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserve ...
s. Otto Seitz identified several varieties of
ammonite
Ammonoids are extinct, (typically) coiled-shelled cephalopods comprising the subclass Ammonoidea. They are more closely related to living octopuses, squid, and cuttlefish (which comprise the clade Coleoidea) than they are to nautiluses (family N ...
(''Mantelliceras Mantelli Sow., Turrilites costatus, Lam., Schloenbachia varians'') and
inoceramid
The Inoceramidae are an extinct family (biology), family of bivalves ("clams") in the Class Mollusca. Fossils of inoceramids are found in marine sediments of Permian to latest Cretaceous in age. Inoceramids tended to live in upper bathyal and ner ...
(''Inoceramus Cripsi Ment., Inoceramus tenuis Ment''.) here. The quarry was used in the second half of the twentieth century as a landfill site and then covered with topsoil.
Archaeology
There are at least two
tumuli
A tumulus (: tumuli) is a mound of Soil, earth and Rock (geology), stones raised over a grave or graves. Tumuli are also known as barrows, burial mounds, mounds, howes, or in Siberia and Central Asia as ''kurgans'', and may be found through ...
dating to the
Bronze Age
The Bronze Age () was a historical period characterised principally by the use of bronze tools and the development of complex urban societies, as well as the adoption of writing in some areas. The Bronze Age is the middle principal period of ...
on the Calenberg. In 1840 two skulls were handed into the
Hanover Provincial Museum (now Lower Saxony State Museum in Hanover), which had been discovered in a tumulus "near the ruins of Calenberg"; the exact location of the tumulus was not given.
History

Calenberg Castle (''Burg Calenberg'') (later described as ''Schloss Calenberg'' and ''Feste Calenberg''; ruins now called ''Alt Calenberg'') was a
medieval
In the history of Europe, the Middle Ages or medieval period lasted approximately from the 5th to the late 15th centuries, similarly to the post-classical period of World history (field), global history. It began with the fall of the West ...
lowland castle
The term lowland castle or plains castle () describes a type of castle that is situated on a lowland, plain or valley floor, as opposed to one built on higher ground such as a hill spur. The classification is extensively used in Germany where ...
(''Niederungsburg''). It was built in 1292 by the
Welf duke,
Otto the Strict in the
Leine water meadows as a
water castle
A water castle, sometimes water-castle, is a castle which incorporates a natural or artificial body of water into its defences.Forde-Johnston (1979), p. 163. It can be entirely surrounded by water-filled moats (moated castle) or natural waterbo ...
on the southern part of the Calenberg.
Before the castle was built, the ''Calenberg'' hill rose some 10 metres above the water meadows between the river arms of the Leine that existed at that time It covered not just the site of Calenberg Castle, but extended a further 500 metres farther north to the River Leine. As a result the castle moats had to be cut over 10 metres deep into the layer of chalk marl. During high water the Calenberg still rises like an island in the surrounding floodwater.
The name ''Calenberg'' clearly indicates that the chalk marl stratum was not tree-covered, but stood proud of the Leine meadows as a "bare hill". The
river terrace
Fluvial terraces are elongated terraces that flank the sides of floodplains and fluvial valleys all over the world. They consist of a relatively level strip of land, called a "tread", separated from either an adjacent floodplain, other fluvial t ...
of the Leine had, in former times, laid down gravel to the north and south of the chalk marl step, that was later covered with
loess
A loess (, ; from ) is a clastic rock, clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loesses or similar deposition (geology), deposits.
A loess ...
and river loam (''Auelehm''). The builders of the water castle used this gravel, loess and loam to build the ramparts. At the start of the 16th century the water castle was converted into a manor house (''Schloss'') and then a fort (''Feste''). After the
Thirty Years War
The Thirty Years' War, fought primarily in Central Europe between 1618 and 1648, was one of the most destructive conflicts in European history. An estimated 4.5 to 8 million soldiers and civilians died from battle, famine, or disease, whil ...
''Fort Calenberg'' lost its military significance and was
slighted
Slighting is the deliberate damage of high-status buildings to reduce their value as military, administrative, or social structures. This destruction of property is sometimes extended to the contents of buildings and the surrounding landscape. It ...
. Today it is a ruin with underground vaults, surrounded by high ramparts.
Quarry, firing range and tip
East of the former labourer's houses, above the moat, was once a large quarry which was established during the construction of Calenberg Castle in order to provide building material. The
small bore shooting club, ''K.K.S.V Schulenburg/Calenberg'',
[Der ''K.K.S.V Schulenburg/Calenberg'' trägt jetzt den Name]
''K.K.S.V. "Ernst August" Schulenburg - Calenberg von 1928 e. V.''
. founded on 12 June 1928 built a
firing range
A shooting range, firing range, gun range or shooting ground is a specialized facility, sports venue, venue, or playing field, field designed specifically for firearm usage qualifications, training, practice, or shooting sport, competitions. ...
there in 1930 with a low-level target trap in a chalk pipe, and then a shooting lodge in 1932. Because the low-level trap was often under water, it was replaced in 1935/36 by a high-level trap.
On 26 April 1949 the British occupation forces blew up the range and all its facilities. The then municipality of Schulenburg/Leine continued to use the quarry as a
rubbish tip and eventually covered it with earth. Today, arable land covers the tip. Apart from the castle ruins and several old worker's houses belonging to the Calenberg estate, the Calenberg is used for agricultural purposes.
The State Office for Mining, Energy and Geology (''Landesamt für Bergbau, Energie und Geologie'') manages the current
landfill site
A landfill is a site for the disposal of waste materials. It is the oldest and most common form of waste disposal, although the systematic burial of waste with daily, intermediate and final covers only began in the 1940s. In the past, waste was ...
under the name ''Nordrand Alt Calenberg'' and under location number 2530124004. According to the department, the tip has an area of 7,570 m
2 and a volume of 21,990 m
3 and is used for building rubble, spoil, household rubbish and bulk rubbish.
References
Maps
* ''Geologische Karte von Preußen und benachbarten deutschen Ländern'' Lieferung 265: ''Blatt Elze'' Nr. 2089. Berlin 1927. Mit einem Begleitheft ''Erläuterungen zur Geologischen Karte von Preußen und benachbarten deutschen Ländern…Blatt Elze'' von Adolf Hoffmann, Berlin 1927.
* ''Flurnamenkarte'' 1:10.000 Blatt 5/3 ''Gestorf'' des Landkreises Hannover, Abt. Kartographie, o. J. (1986).
* ''Flurnamenlexikon zur Flurnamenkarte'', Hrsg. vom Landkreis Hannover. Bearb. Heinz Weber Teil 5,3: ''Gestorf''. Schriftenreihe: ''Flurnamensammlung des Landkreises Hannover.'' o. J. (1986).
* ''Flurnamenkarte'' 1:10.000 Blatt 6/3 ''Alt-Calenberg'' des Landkreises Hannover, Abt. Kartographie, o. J. (1981).
* ''Flurnamenlexikon zur Flurnamenkarte'', Hrsg. vom Landkreis Hannover. Bearb. Heinz Weber Teil 6,3: ''Alt-Calenberg''. Schriftenreihe: ''Flurnamensammlung des Landkreises Hannover.'' o. J. (1987).
External links
Landschaftsschutzgebiet "Calenberger Leinetal"(PDF-Datei; 55 kB)
{{Authority control
Hanover (region)
Hills of Lower Saxony