The Calenberg is a hill in central Germany in the Leine depression near Pattensen in the municipality of Schulenburg. It lies 13 km west of the city of Hildesheim in south Lower Saxony on the edge of the Central Uplands . It is made from a chalk marl slab ( Kalkmergelbank ), has a height of 70 m above NN and was formed almost 100 million years ago at the beginning of the Upper Cretaceous series in Cenomanian 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 .
46-620: The syllables Kal , Kalen- , Calen- in the word Calenberg are derived from the word kal in the Middle High German and Middle Low German 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 word berg , to the Middle High German berc(g) , to
92-575: 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 of
138-479: 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
184-424: A possible thin layer of alluvium) is left above either a stream or river channel. These bedrock terraces are the strath terraces and are erosional in nature. Paired and unpaired terraces : Terraces of the same elevation on opposite sides of either a stream or river are called paired terraces . They occur when it downcuts evenly on both sides and terraces on one side of the river correspond in height with those on
230-432: A volume of 21,990 m and is used for building rubble, spoil, household rubbish and bulk rubbish. 52°11′54.24″N 9°47′42″E / 52.1984000°N 9.79500°E / 52.1984000; 9.79500 Middle High German Middle High German ( MHG ; endonym : diutsch or tiutsch ; New High German : Mittelhochdeutsch [ˈmɪtl̩hoːxˌdɔʏtʃ] , shortened as Mhdt. or Mhd. )
276-471: Is no standard MHG, the prestige of the Hohenstaufen court gave rise in the late 12th century to a supra-regional literary language ( mittelhochdeutsche Dichtersprache ) based on Swabian , an Alemannic dialect. This historical interpretation is complicated by the tendency of modern editions of MHG texts to use normalised spellings based on this variety (usually called "Classical MHG"), which make
322-429: Is reached and it can transport the material rather than deposit it. This equilibrium may last for a very short period, such as, after glaciation, or for a very long time if the conditions do not change. The fill terrace is created when the conditions change again and either a stream or river starts to incise into the material that it deposited in the valley. Once this occurs benches composed completely of alluvium form on
368-810: Is the opening strophe of the Nibelungenlied ( c. 1204 ). Middle High German Uns ist in alten mæren wunders vil geseit von helden lobebæren, von grôzer arebeit, von freuden, hôchgezîten, von weinen und von klagen, von küener recken strîten muget ir nu wunder hœren sagen. Modern German translation In alten Erzählungen wird uns viel Wunderbares berichtet von ruhmreichen Helden, von hartem Streit, von glücklichen Tagen und Festen, von Schmerz und Klage: vom Kampf tapferer Recken: Davon könnt auch Ihr nun Wunderbares berichten hören. River terrace Fluvial terraces are elongated terraces that flank
414-718: Is the term for the form of German spoken in the High Middle Ages . It is conventionally dated between 1050 and 1350, developing from Old High German and into Early New High German . High German is defined as those varieties of German which were affected by the Second Sound Shift ; the Middle Low German and Middle Dutch languages spoken to the North and North West, which did not participate in this sound change , are not part of MHG. While there
460-471: The Cenomanian rock of which the Calenberg is made. The strata consist of plate-like, gray-white limestone , the upper layers being quite rich in fossils . Otto Seitz identified several varieties of ammonite ( Mantelliceras Mantelli Sow., Turrilites costatus, Lam., Schloenbachia varians ) and inoceramid ( Inoceramus Cripsi Ment., Inoceramus tenuis Ment .) here. The quarry was used in the second half of
506-649: The 11th century, and all the East Central German dialects are a result of this expansion. "Judeo-German", the precursor of the Yiddish language, is attested in the 12th–13th centuries, as a variety of Middle High German written in Hebrew characters. The Middle High German period is generally dated from 1050 to 1350. An older view puts the boundary with (Early) New High German around 1500. There are several phonological criteria which separate MHG from
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#1732773024752552-493: 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
598-537: 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 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 Fort Calenberg lost its military significance and
644-542: The MHG period is characterised by a massive rise in population, terminated by the demographic catastrophe of the Black Death (1348). Along with the rise in population comes a territorial expansion eastwards ( Ostsiedlung ), which saw German-speaking settlers colonise land previously under Slavic control. Linguistically, the transition to Early New High German is marked by four vowel changes which together produce
690-557: 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
736-484: 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. The Calenberg lies in
782-435: The approximate values of /ei/ , /iə/ , /ou/ , /øy/ , /eu/ , /yə/ , /uə/ , respectively. Middle High German pronouns of the first person refer to the speaker; those of the second person refer to an addressed person; and those of the third person refer to a person or thing of which one speaks. The pronouns of the third person may be used to replace nominal phrases . These have the same genders , numbers and cases as
828-688: The example of Good King Arthur who with knightly spirit knew how to strive for praise. In his day He lived so well That he wore the crown of honour And his name still does so. The truth of this is known To his countrymen: They affirm that he still lives today: He won such fame that Although his body died His name lives on. Of sinful shame He will forever be free Who follows his example. Commentary: This text shows many typical features of Middle High German poetic language. Most Middle High German words survive into modern German in some form or other: this passage contains only one word ( jehen 'say' 14) which has since disappeared from
874-670: The exception of Thuringian, the East Central German dialects are new dialects resulting from the Ostsiedlung and arise towards the end of the period. Middle High German texts are written in the Latin alphabet . There was no standardised spelling, but modern editions generally standardise according to a set of conventions established by Karl Lachmann in the 19th century. There are several important features in this standardised orthography which are not characteristics of
920-477: The fill terraces mentioned above, but they are erosional in origin. Once the alluvium deposited in the valley has begun to erode and fill terraces form along the valley walls, cut terraces may also form below the fill terraces. As either a stream or river continues to incise into the material, multiple levels of terraces may form. The uppermost being the fill terraces and the remaining lower terraces are cut terraces. Nested fill terraces: Nested fill terraces are
966-456: The following consonant spellings: The charts show the vowel and consonant systems of classical MHG. The spellings indicated are the standard spellings used in modern editions; there is much more variation in the manuscripts. Notes: MHG diphthongs are indicated by the spellings ⟨ei⟩ , ⟨ie⟩ , ⟨ou⟩ , ⟨öu⟩ and ⟨eu⟩ , ⟨üe⟩ , ⟨uo⟩ , and they have
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#17327730247521012-458: The following vowel spellings: Grammars (as opposed to textual editions) often distinguish between ⟨ë⟩ and ⟨e⟩ , the former indicating the mid-open /ɛ/ which derived from Germanic /e/ , the latter (often with a dot beneath it) indicating the mid-close /e/ which results from primary umlaut of short /a/ . No such orthographic distinction is made in MHG manuscripts. The standardised orthography of MHG editions uses
1058-1113: The impetus for this set of social changes came largely from France, many of the new words were either loans from French or influenced by French terms. The French loans mainly cover the areas of chivalry, warfare and equipment, entertainment, and luxury goods: Two highly productive suffixes were borrowed from French in this period: The text is the opening of Hartmann von Aue 's Iwein ( c. 1200 ) Swer an rehte güete wendet sîn gemüete, dem volget sælde und êre. des gît gewisse lêre künec Artûs der guote, der mit rîters muote nâch lobe kunde strîten. er hât bî sînen zîten gelebet alsô schône daz er der êren krône dô truoc und noch sîn name treit. des habent die wârheit sîne lantliute: sî jehent er lebe noch hiute: er hât den lop erworben, ist im der lîp erstorben, sô lebet doch iemer sîn name. er ist lasterlîcher schame iemer vil gar erwert, der noch nâch sînem site vert. [1] [5] [10] [15] [20] Whoever to true goodness Turns his mind He will meet with fortune and honour. We are taught this by
1104-401: The language. But many words have changed their meaning substantially. Muot (6) means 'state of mind' (cognates with mood ), where modern German Mut means courage. Êre (3) can be translated with 'honour', but is quite a different concept of honour from modern German Ehre ; the medieval term focuses on reputation and the respect accorded to status in society. The text
1150-732: The length of either a stream or river, gradually lowering its elevation. For example, downcutting by a river can lead to increased velocity of a tributary, causing that tributary to erode toward its headwaters. Terraces can also be left behind when the volume of the fluvial flow declines due to changes in climate , typical of areas which were covered by ice during periods of glaciation , and their adjacent drainage basins. There are two basic types of fluvial terraces, fill terraces and strath terraces. Fill terraces sometimes are further subdivided into nested fill terraces and cut terraces. Both fill and strath terraces are, at times, described as being either paired or unpaired terraces based upon
1196-726: The neuter singular, is used only with prepositions : von diu , ze diu , etc. In all the other genders and in the plural it is substituted with the dative: von dëm , von dër , von dën . Middle High German nouns were declined according to four cases ( nominative , genitive , dative , accusative ), two numbers (singular and plural ) and three genders (masculine, feminine and neuter), much like Modern High German, though there are several important differences. Verbs were conjugated according to three moods ( indicative , subjunctive (conjunctive) and imperative ), three persons, two numbers (singular and plural ) and two tenses ( present tense and preterite ) There
1242-485: The original manuscripts : A particular problem is that many manuscripts are of much later date than the works they contain; as a result, they bear the signs of later scribes having modified the spellings, with greater or lesser consistency, in accord with conventions of their time. In addition, there is considerable regional variation in the spellings that appear in the original texts, which modern editions largely conceal. The standardised orthography of MHG editions uses
1288-435: The original nominal phrase. The possessive pronouns mîn, dîn, sîn, ir, unser, iuwer are used like adjectives and hence take on adjective endings following the normal rules. The inflected forms of the article depend on the number, the case and the gender of the corresponding noun. The definite article has the same plural forms for all three genders. Definite article (strong) The instrumental case , only existing in
1334-430: The other side. Paired terraces are caused by river rejuvenation . Unpaired terraces occur when either a stream or river encounters material on one side that resists erosion, leaving a single terrace with no corresponding terrace on the resistant side. Fluvial terraces can be used to measure the rate at which either a stream or river is downcutting its valley. Using various dating methods, an age can be determined for
1380-527: The phonemic system of modern German, though not all dialects participated equally in these changes: The centres of culture in the ENHG period are no longer the courts but the towns. The dialect map of Germany by the end of the Middle High German period was much the same as that at the start of the 20th century, though the boundary with Low German was further south than it now is: Central German ( Mitteldeutsch ) Upper German ( Oberdeutsch ) With
1426-560: The preceding Old High German period: Culturally, the two periods are distinguished by the transition from a predominantly clerical written culture, in which the dominant language was Latin , to one centred on the courts of the great nobles, with German gradually expanding its range of use. The rise of the Hohenstaufen dynasty in Swabia makes the South West the dominant region in both political and cultural terms. Demographically,
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1472-659: The protected landscape of the Calenberg Leine Valley ( Calenberger Leinetal ). It is bordered to the north by the Leine , to the west and south by the state road, Landesstraße 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 , in the south are the ditches, ramparts and ruins of Calenburg Castle ( Burg Calenberg ) and several old workers' cottages belonging to
1518-496: The relative elevations of the surface of these terraces. Fill terraces: Fill terraces are the result of an existing valley being filled with alluvium . The valley may fill with alluvium for many different reasons including: an influx in bed load due to glaciation or change in stream power which causes the valley, that was down cut by either a stream or river, to be filled in with material (Easterbrook). The stream or river will continue to deposit material until an equilibrium
1564-408: The remnants of earlier floodplains that existed at a time when either a stream or river was flowing at a higher elevation before its channel downcut to create a new floodplain at a lower elevation. Changes in elevation can be due to changes in the base level (elevation of the lowest point in the fluvial system, usually the drainage basin ) of the fluvial system, which leads to headward erosion along
1610-420: The result of either a stream or river downcutting through bedrock. As the flow continues to downcut, a period of valley widening may occur and expand the valley width. This may occur due to an equilibrium reached in the fluvial system resulting from: slowed or paused uplift, climate change, or a change in the bedrock type. Once downcutting continues the flattened valley bottom composed of bedrock (overlain with
1656-490: The result of the valley filling with alluvium, the alluvium being incised, and the valley filling again with material but to a lower level than before. The terrace that results for the second filling is a nested terrace because it has been “nested” into the original alluvium and created a terrace. These terraces are depositional in origin and may be able to be identified by a sudden change in alluvium characteristics such as finer material. Strath terraces: Strath terraces are
1702-501: 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 terraces, or uplands by distinctly steeper strips of land called "risers". These terraces lie parallel to and above the river channel and its floodplain. Because of the manner in which they form, fluvial terraces are underlain by fluvial sediments of highly variable thickness. River terraces are
1748-463: The sides of the valley. The upper most benches are the fill terraces. As it continues to cut down through the alluvium the fill terraces are left above the river channel (sometimes 100 m or more). The fill terrace is only the very highest terrace resulting from the depositional episode; if there are multiple terraces below the fill terrace, these are called "cut terraces". Cut terraces: Cut terraces, also called "cut-in-fill" terraces, are similar to
1794-433: 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 under the name Nordrand Alt Calenberg and under location number 2530124004. According to the department, the tip has an area of 7,570 m and
1840-708: The twentieth century as a landfill site and then covered with topsoil. There are at least two tumuli dating to the Bronze Age 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. Calenberg Castle ( Burg Calenberg ) (later described as Schloss Calenberg and Feste Calenberg ; ruins now called Alt Calenberg )
1886-407: The vowels in brackets were dropped in rapid speech. The preterite conjugation went as follows: The present tense conjugation went as follows: The vowels in brackets were dropped in rapid speech. The preterite conjugation went as follows: In the Middle High German period, the rise of a courtly culture and the changing nature of knighthood was reflected in changes to the vocabulary. Since
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1932-524: The written language appear more consistent than it actually is in the manuscripts. Scholars are uncertain as to whether the literary language reflected a supra-regional spoken language of the courts. An important development in this period was the Ostsiedlung , the eastward expansion of German settlement beyond the Elbe - Saale line which marked the limit of Old High German . This process started in
1978-409: Was slighted . Today it is a ruin with underground vaults, surrounded by high ramparts. 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 , founded on 12 June 1928 built a firing range there in 1930 with
2024-580: Was a medieval lowland castle ( Niederungsburg ). It was built in 1292 by the Welf duke, Otto the Strict in the Leine water meadows as a water castle 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
2070-427: Was a present participle, a past participle and a verbal noun that somewhat resembles the Latin gerund , but that only existed in the genitive and dative cases. An important distinction is made between strong verbs (that exhibited ablaut ) and weak verbs (that didn't). Furthermore, there were also some irregular verbs. The present tense conjugation went as follows: The bold vowels demonstrate umlaut ;
2116-536: 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 . By about 1900 markets were held north of Lauenstadt at which everyday items were sold in open stalls. 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
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