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See also:DENMARK (Danmark)
, a small See also:kingdom of See also:Europe, occupying See also:part of a See also:peninsula and a See also:group of islands dividing the Baltic and See also:North Seas, in the See also:middle latitudes of the eastern See also:coast
.
The kingdom lies between 54° 33' and 570 45' N. and between 8° 4' 54" and 120 47' 25" E., exclusive of the See also:island of See also:Bornholm, which, as will be seen, is not to be included in the Danish See also:archipelago
.
The peninsula is divided between See also:Denmark and See also:Germany (See also:Schleswig-See also:Holstein)
.
The Danish portion is the See also:northern and the greater, and is called See also:Jutland (See also:Dan
.
Jylland)
.
Its northern part is actually insular, divided from the mainland by the Limfjord or Liimfjord, which communicates with the North See also:Sea to the See also:west and the See also:Cattegat to the See also:east, but this strait, though broad and possessing lacustrine characteristics to the west, has only very narrow entrances
.
The connexion with the North Sea See also:dates from 1825
.
The See also:Skagerrack See also:bounds Jutland to the north and north-west
.
The Cattegat is divided from the Baltic by the Danish islands, between the east coast of the Cimbric peninsula in the neighbourhood of the See also:German frontier and See also:south-western See also:Sweden
.
There is little variety in the See also:surface of Denmark
.
It is uniformly See also:low, the highest See also:elevation in the whole See also:country, the Himmelbjerg near See also:Aarhus in eastern Jutland, being little more than 500 ft. above the sea
.
Denmark, however, is nowhere low in the sense in which See also: The landscape of the islands and the south-eastern part of Jutland is See also:rich in See also:beech-See also:woods, See also:corn See also:fields and meadows, and even the See also:minute islets are See also:green and fertile . In the western and northern districts of Jutland this See also:condition gives See also:place to a wide expanse of moorland, covered with heather, and ending towards the sea in low whitish-See also:grey cliffs . There is a certain See also:charm even about these monotonous tracts, and it cannot be DENMARK 23 said that Denmark is wanting in natural beauty of a quiet See also:order . Lakes, though small, are numerous; the largest are the Arreso and the Esromso in See also:Zealand, and the See also:chain of lakes in the Himmelbjerg region, which are drained by the largest See also:river in Denmark, the Gudenaa, which, however, has a course not exceeding 8o m . Many of the See also:meres, overhung with thick beech-woods, are extremely beautiful . The coasts are generally low and sandy; the whole western See also:shore of Jutland is a See also:succession of See also:sand ridges and shallow lagoons, very dangerous to See also:shipping . In many places the sea has encroached; even in the 19th See also:century entire villages were destroyed, but during the last twenty years of the century systematic efforts were made to secure the coast by groynes and embankments . A See also:belt of sand See also:dunes, from 500 yds. to 7 M. wide, stretches along the whole of this coast for about 200 M . Skagen, or the Skaw, a See also:long, low, sandy point, stretches far into the northern sea, di' iding the Skagerrack from the Cattegat . On the western See also:side the coast is bolder and less inhospitable; there are several excellent havens, especially on the islands . The coast is nowhere, however, very high, except at one or two points in Jutland, and at the eastern extremity, of Moen, where See also:limestone cliffs occur . See also:Continental Denmark is confined wholly to Jutland, the See also:geographical description of which is given under that heading .
Out of the See also:total See also:area of the kingdom, 14,829 sq. in., Jutland, including the small islands adjacent to it, covers 9753 sq. m., and the insular part of the kingdom (including Bornholm), 5076 sq. m
.
The islands may be divided into two See also:groups, consisting of the two See also:principal islands Funen and Zealand, and the lesser islands attendant on each
.
Funen (Dan
.
Fyen), in See also:form roughly an See also:oval with an See also:axis from S.E. to N.W. of 53 in., is separated from Jutland by a channel not See also:half a mile wide in the north, but averaging ro m. between the island and the Schleswig coast, and known as the Little Belt
.
Funen, geologically a part of See also:southern Jutland, has similar characteristics, a smiling landscape of fertile meadows, the typical beech-forests clothing the low hills and the presence of numerous erratic blocks, are the superficial signs of likeness
.
Several islands, none of See also:great extent, See also:lie off the west coast of Funen in the Little Belt; off the south, how-ever, an archipelago is enclosed by the long narrow islands of Aero (16 m. in length) and Langeland (32 m.), including in a triangular area of shallow sea the islands of Taasinge, Avernako, Dreio, Turo and others
.
These are generally fertile and well cultivated
.
Aeroskjobing and Rudkjobing, on Aero and Langeland respectively, are considerable ports
.
On Langeland is the great See also:castle of Tranekjaer, whose See also:record dates from the 13th century
.
The See also:chief towns of Funen itself are all coastal
.
See also:Odense is the principal See also:town, lying See also:close to a great inlet behind the peninsula of Hindsholm on the north-east, known as Odense See also:Fjord
.
See also:Nyborg on the east is the See also:port for the See also:steam-See also:ferry to See also:Korsor in Zealand; See also:Svendborg picturesquely overlooks the southern archipelago; Faaborg on the south-west lies on a fjord of the same name; Assens, on the west, a port for the See also:crossing of the Little Belt into Schleswig, still shows traces of the fortifications which were stormed by See also:
All these towns are served by See also:railways radiating from Odense
.
The strait crossed by the Nyhorg-Korsor ferry is the Great Belt which divides the Funen from the Zealand group, and is continued south by the Langelands Belt, which washes the straight eastern shore of that island, and north by the Samso Belt, named from an island 15 m. in length, with several large villages, which lies somewhat apart from the See also:main archipelago
.
Zealand, or Sealand (Dan
.
Sjaelland), measuring 82 m
.
N. to S. by 68 E. to W
.
(extremes), with its fantastic coast-See also:line indented by fjords and projecting into long spits or promontories may be considered as the See also:nucleus of the kingdom, inasmuch as it contains the See also:capital, See also:Copenhagen, and such important towns as See also:Roskilde, Slagelse, Korsor, See also:Naestved and See also:Elsinore (Helsingor)
.
Its See also:topography is described in detail under ZEALAND
.
Its attendant islands lie mainly to the south and are parts of itself, only separated by geologically See also:recent troughs
.
The eastern
coast of Moen is rocky and bold
.
It is recorded that this island formed three See also:separate isles in r coo, and the See also:village of Borre, now 2 M. inland, was the See also:object of an attack by a See also:fleet from See also:Lubeck in 1510
.
On Falster is the port of See also:Nykjobing, and from Gjedser, the extreme southern point of Denmark, communication is maintained with Warnemunde in Germany (29 m.)
.
From Nykjobing a See also:bridge nearly one-third of a mile long crosses to Laa See also:land, at the west of which is the port of See also:Nakskov; the other towns are the See also:county town of Maribo with its See also:fine See also:
The island of Bornholm lies 86 m
.
E. of the nearest point of the archipelago, and as it belongs geologically to Sweden (from which it is distant only 22 m.) must be considered to be physically an appendage rather than an See also:internal part of the kingdom of Denmark
.
See also:Geology.—The surface in Denmark is almost everywhere formed by the so-called See also:Boulder See also:Clay and what the Danish geologists See also:call the Boulder Sand
.
The former, as is well known, owes its origin to the See also:action of See also:ice on the mountains of See also:Norway in the Glacial See also:period
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It is unstratified; but by the action of See also:water on it, stratified deposits have been formed, some of clay, containing remains of See also:arctic animals, some, and very extensive ones, of sand and See also:gravel
.
This boulder sand forms almost every-where the highest hills, and besides, in the central part of Jutland, a wide expanse of See also:heath and moorland apparently level, but really sloping gently towards the west
.
The deposits of the boulder formation See also:rest generally on limestone of the Cretaceous period, which in many places comes near the surface and forms cliffs on the sea-coast
.
Much of the Danish See also:chalk, including the well-known limestone of Faxe, belongs to the highest or "Danian" subdivision of the Cretaceous period
.
In the south-western parts a succession of strata, described as the See also:
Some parts of Denmark are supposed to have been finally raised out of the sea towards the close of the Cretaceous period; but as a whole the country did not appear above the water till about the close of the Glacial period
.
The upheaval of the country, a See also:movement See also:common to a large part of the Scandinavian peninsula, still continues, though slowly, north-east of a line See also:drawn in a south-easterly direction from Nissumfjord on the west coast of Jutland, across the island of Fyen, a little south of the town of Nyborg
.
See also:Ancient sea-beaches, marked by accumulations of seaweed, rolled stones, &c., have been noticed as much as 20 ft. above the See also:present level
.
But the upheaval does not seem to affect all parts equally
.
Even in historic times it has vastly changed the aspect and configuration of the country
.
See also:Climate, See also:Flora, See also:Fauna.—The climate of Denmark does not differ materially from that of Great See also:Britain in the same See also:latitude; but whilst the summer is a little warmer, the See also:winter is colder, so that most of the evergreens which adorn an See also:English See also:garden in the winter cannot be grown in the open in Denmark
.
During See also:thirty years the See also:annual mean temperature varied from 43.88° F. to 46.22° in different years and different localities, the mean See also:average for the whole country being 45'14
.
The islands have, upon the whole, a somewhat warmer climate than Jutland
.
The mean temperatures of the four coldest months, See also:December to See also: The annual rainfall varies between 21.58 in. and 27.87 in. in different years and different localities . It is highest on the west coast of Jutland; while the small island of Anholt in the Cattegat has an annual rainfall of only 15.78 in . More than half the rainfall occurs from See also:July to See also:November, the wettest See also:month being See also:September, with an average of 2'95 in.; the driest month is See also:April, with an average of 1.14 in . Thunderstorms are frequent in the summer . South-See also:westerly winds prevail from See also:January to March, and from September to the end of the See also:year . In April the east See also:wind, which is particularly searching, is predominant, while westerly winds prevail from May to August . In the See also:district of See also:Aalborg, in the north of Jutland, a See also:cold and dry N.W. wind called skai prevails in May and June, and is exceedingly destructive to vegetation; while along the west coast of the peninsula similar effects are produced by a See also:salt mist, which carries its See also:influence from 15 to 30 M. inland . The flora of Denmark presents greater variety than might be anticipated in a country of such See also:simple See also:physical structure . The See also:ordinary forms of the north of Europe grow freely in the mild See also:air and protected See also:soil of the islands and the eastern coast; while on the heaths and along the sandhills on the See also:Atlantic side there flourish a number of distinctive See also:species . The Danish See also:forest is almost exclusively made up of beech, a See also:tree which thrives better in Denmark than in any other country of Europe . The See also:oak and ash are now rare, though in ancient times both were abundant in the Danish islands . The See also:elm is also scarce . The almost universal predominance of the beech is by no means of ancient origin, for in the first half of the 17th century the oak was still the characteristic Danish tree . No conifer grows in Denmark except under careful cultivation, which, however, is largely practised in Jutland (q.v.) . But again, abundant traces of ancient extensive forests of See also:fir and See also:pine are found in the numerous See also:peat bogs which See also:supply a large proportion of the See also:fuel locally used . In Bornholm, it should be mentioned, the flora is more like that of Sweden; not the beech, but the pine, See also:birch and ash are the most abundant trees . The See also:wild animals and birds of Denmark are those of the rest of central Europe . The larger quadrupeds are all See also:extinct; even the red See also:deer, formerly so abundant that in a single See also:hunt in Jutland in 1593 no less than 1600 See also:head of deer were killed, is now only to be met with in preserves . In the prehistoric " kitchenmiddens " (kj okkenmodding) and elsewhere, however, vestiges are found which prove that the urochs, the wild See also:boar, the See also:beaver, the See also:bear and the See also:wolf all existed subsequently to the arrival of See also:man . The usual domestic animals are abundantly found in Denmark, with the exception of the See also:goat, which is uncommon . The sea See also:fisheries are of importance . Oysters are found in some places, but have disappeared from many localities, where their abundance in ancient times is proved by their See also:shell moulds on the coast . The Gudenaa is the only See also:salmon river in Denmark . See also:Population.—The population of Denmark in 1901 was 2,449,540 . It was 929,001 in 18or, showing an increase during the century in the proportion of 1 to 2.63 . In 1901 the average See also:density of the population of Denmark was 165.2 to the square mile, but varied much in the different parts . Jutland showed an average of only 109 inhabitants per square mile, whilst on the islands, which had a total population of 1,385,537, the average stood at 272.95, owing, on the one See also:hand, to the fact that large tracts in the interior of Jutland are almost uninhabited, and on the other to the fact that the capital of the country, with its proportionately large population, is situated on the island of Zealand . The percentages of See also:urban and rural population are respectively about 38 and 62 . A notable movement of the population to the towns began about the middle of the 19th century, and increased until very near its end . It was stronger on the islands, where the rural population increased by 5.3 % only in eleven years, whereas in Jutland the increase of the rural population between 1890 and Igor amounted to 12.0% . Here, however, See also:peculiar circumstances contributed to the increase, as successful efforts have been made to render the land fruitful by artificial means . The Danes are a yellow-haired and See also:blue-eyed See also:Teutonic See also:race of middle stature, bearing traces of their kinship with the northern Scandinavian peoples . Their habits of See also:life resemble those of the North Germans even more than those of the Swedes . The in-dependent See also:tenure of the land by a vast number of small farmers, who are their own masters, gives an air of carelessness, almost of truculence, to the well-to-do Danish peasants . They are generally slow of speech and manner, and somewhat irresolute, but take an eager See also:interest in current politics, and are generally fairly educated men of extreme democratic principles . The result of a fairly equal See also:distribution of See also:wealth is a marked tendency towards equality in social intercourse . The townspeople show a See also:bias in favour of See also:French habits and fashions . The separation from the duchies of Schleswig and Holstein, which were more than half German, intensified the See also:national See also:character; the Danes are intensely patriotic; and there is no portion of the Danish dominions except perhaps in the West See also:Indian islands, where a Scandinavian See also:language is not spoken . The preponderance of the See also:female population over the male is approximately as 1052 to toe* . The male See also:sex remains in excess until about the twentieth year, from which See also:age the female sex preponderates in increasing ratio with advancing age . The percentage of See also:illegitimacy is high as a whole, although in some of the rural districts it is very low . But in Copenhagen 20 % of the births are illegitimate . Between the middle and the end of the 19th century the See also:rate of mortality decreased most markedly for all ages . During the last See also:decade of the century it ranged between 19.5 per thousand in 1891 and 15.1 in 1898 (17.4 in 1900) . See also:Emigration for some time in the 19th century at different periods, both in its See also:early part and towards its close, seriously affected the population of Denmark . But in the last decade it greatly diminished . Thus in 1892 the number of emigrants to Transatlantic places See also:rose to 10,422 but in 1900 it was only 3570 . The great bulk of them go to the See also:United States; next in favour is See also:Canada . Communications.—The roads of Denmark form an extensive and well-maintained system . The railway system is also fairly See also:complete, the See also:state owning about three-fifths of the total mileage, which amounts to some 2000 . Two lines enter Denmark from Schleswig across the frontier . The main Danish lines are as follows . From the frontier a line runs east by See also:Fredericia, across the island of Fiinen by Odense and Nyborg, to Korsor on Zealand, and thence by Roskilde to Copenhagen . The straits between Fredericia and Middelfart and between Nyborg and Korsor are crossed by powerful steam-ferries which are generally capable of conveying a limited number of railway wagons . This system is also in use on the line which runs south fromRoskilde to the island of Falster, from the southernmost point of which, Gjedser, ferry-steamers taking railway cars serve Warnemiinde in Germany . The main lines in Jutland run (a) along the eastern side north from Fredericia by See also:Horsens, Aarhus, See also:Randers, Aalborg and See also:Hjorring, to Frederikshavn, and (b) along the western side from See also:Esbjerg by Skjerne and Vemb, and thence across the peninsula by See also:Viborg to Langaa on the eastern line . The lines are generally of See also:standard See also:gauge (4 ft . 82 in.), but there is also a considerable mileage of light narrow-gauge railways . Besides the numerous steam-ferries which connect island and island, and Jutland with the islands, and the Gjedser-Warnemiinde route, a favourite passenger line from Germany is that between See also:Kiel and Korsor, while most of the German Baltic ports have See also:direct connexion with Copenhagen . With Sweden communications are established by ferries across the Sound between Copenhagen and Malmo and See also:Landskrona, and between Elsinore (Helsingor) and See also:Helsingborg . The postal See also:department maintains a See also:telegraph and See also:telephone service . See also:Industries.—The main source of wealth in Denmark is See also:agriculture, which employs about two-fifths of the entire population . Most of the land is See also:freehold and cultivated by the owner himself, and comparatively little land is let on See also:lease except very large holdings and See also:glebe farms . The See also:independent small See also:farmer (bonder) maintains a hereditary See also:attachment to his ancestral holding . There is also a class of cottar freeholders (junster) . Fully 74 % of the total area of the country is agricultural land . Of this only about one-twelfth is meadow land . The land under See also:grain crops is not far See also:short of one-half the See also:remainder, the principal crops being oats, followed by See also:barley and See also:rye in about equal quantities, with See also:wheat about one-See also:sixth that of barley and hardly one-tenth that of oats . See also:Beet is extensively grown . During the last See also:forty years of the 19th century See also:dairy-farming was greatly See also:developed in Denmark, and brought to a high degree of perfection by the application of scientific methods and the best machinery, as well as by the See also:establishment of See also:joint dairies . The Danish See also:government has assisted this development by granting See also:money for experiments and by a rigorous system of inspection for the prevention of See also:adulteration . The co-operative system plays an important part in the industries of See also:butter-making, poultry-farming and the rearing of See also:swine . Rabbits, which are not found wild in Denmark, are bred for export . Woods See also:cover fully 7% of the area, and their preservation is considered of so much importance that private owners are under strict See also:control as regards cutting of See also:timber . The woods consist mostly of beech, which is principally used for fuel, but pines were extensively planted during the 19th century . Allusion has been made already to the efforts to plant the extensive heaths in Jutland (q.v.) with pine-trees . Agriculture.—Rates and taxes on land are mostly levied ac-cording to a See also:uniform system of See also:assessment, the unit of which is called a Tonde Hartkorn . The Td . Htk., as it is usually abbreviated, has further subdivision, and is intended to correspond to the same value of land throughout the country . The Danish measure for land is a Tonde Land (Td . L.), which is equal to 1.363 See also:statute acres . Of the best ploughing land a little over 6 Td . L., or about 8 acres, go to a Td . Htk., but of unprofitable land a Td . Htk. may represent 30o acres or more . On the islands and in the more fertile part of Jutland the average is about 10 Td . L., or 131 acres . Woodland, See also:tithes, &c., are also assessed to Td . Htk. for fiscal purposes . In the island of Bornholm, the assessment is somewhat different, though the See also:general state of agricultural holdings is the same as in other parts . The selling value of land has shown a decrease in See also:modern times on account of the agricultural depression . A See also:homestead with land assessed less than 1 Td . Htk. is legally called a Huus or Sted, i.e. cottage, whilst a See also:farm assessed at 1 Td . Htk. or more is called Gaard, i.e. farm . Farms of between i and 12 Td . Htk. are called Bondergaarde, or See also:peasant farms, and are subject to the restriction that such a holding cannot lawfully be joined to or entirely merged into another . They may be subdivided, and portions may be added to another holding, but the homestead, with a certain amount of land, must be preserved as a separate holding for ever . The seats of the See also:nobility and landed gentry are called Herregaarde . The peasants hold about 73 % of all the land according to its value . As regards their See also:size about 30 % are assessed from 1 to 4 Td . Htk.; about 33% from 4 to 8 Td . Htk.; the remainder at about 8 Td . Htk . An annual sum is voted by See also:parliament out of which loans are granted to cottagers who See also:desire to See also:purchase small freehold plots . The See also:fishery along the coasts of Denmark is of some importance both on account of the supply of See also:food obtained thereby for the population of the country, and on account of the export; but the See also:good fishing grounds, not far from the Danish coast, particularly in the North Sea, are mostly worked by the fishing vessels of other nations, which are so numerous that the Danish government is obliged to keep See also:gun-boats stationed there in order to prevent encroachments on territorial See also:waters . Other Industries.—The See also:mineral products of Denmark are unimportant . It is one of the poorest countries of Europe in this particular . It is rich, however, in See also:clays, while in the island of Bornholm there are quarries of freestone and See also:marble . The factories of Denmark supply mainly See also:local needs . The largest are those engaged in the construction of engines and See also:iron See also:ships . The manufacture of woollens and See also:cotton, the domestic manufacture of See also:linen in Zealand, See also:sugar refineries, See also:paper See also:mills, breweries, and distilleries may also be mentioned . The most notable manufacture is that of See also:porcelain . The nucleus of this See also:industry was a factory started in 1772, by F . H . Milller, for the making of See also:china out of Bornholm clay . In 1779 it passed into the hands of the state, and has remained there ever since, though there are also private factories . Originally the Copenhagen potters imitated the See also:Dresden china made at See also:Meissen, but they later produced graceful See also:original designs . The creations of Thorvaldsen have been largely repeated and imitated in this See also:ware . See also:Trade-unionism flourishes in Denmark, and strikes are of frequent occurrence . See also:Commerce.—Formerly the commercial legislation of Denmark was to such a degree restrictive that imported manufactures had to be delivered to the customs, where they were sold by public See also:auction, the proceeds of which the importer received from the See also: |