Unified Germany has an area of 356,959 square kilometers. Extending 853 kilometers from its northern border with Denmark to the Alps in the south, it is the sixth largest country in Europe. At its widest, Germany measures approximately 650 kilometers from the Belgian-German border in the west to the Polish frontier in the east.
The territory of the former East Germany (divided into five new Länder in 1990) accounts for almost one-third of united Germany's territory and one-fifth of its population. After a close vote, in 1993 the Bundestag, the lower house of Germany's parliament, voted to transfer the capital from Bonn in the west to Berlin, a city-state in the east surrounded by the Land of Brandenburg. The relocation process is expected to be concluded by about the year 2000, following the transfer of the Bundestag, the Bundesrat, the Chancellory, and ten of the eighteen federal ministries.
With its irregular, elongated shape, Germany provides an excellent example of a recurring sequence of landforms found the world over. A plain dotted with lakes, moors, marshes, and heaths retreats from the sea and reaches inland, where it becomes a landscape of hills crisscrossed by streams, rivers, and valleys. These hills lead upward, gradually forming high plateaus and woodlands and eventually climaxing in spectacular mountain ranges.
As of the mid-1990s, about 37 percent of the country's area was arable; 17 percent consisted of meadows and pastures; 30 percent was forests and woodlands; and 16 percent was devoted to other uses. Geographers often divide Germany into four distinct topographic regions: the North German Lowland; the Central German Uplands; Southern Germany; and the Alpine Foreland and the Alps.
North German Lowland
The North German Lowland is a part of the Great European Plain that sweeps across Europe from the Pyrenees in France to the Ural Mountains in Russia. All of the Länder of Schleswig-Holstein, Hamburg, Bremen, Mecklenburg-Western Pomerania, Brandenburg, Berlin, most of Lower Saxony and Saxony-Anhalt, and parts of Saxony and North Rhine-Westphalia are located in this region.
Hills in the lowland only rarely reach 200 meters in height, and most of the region is well under 100 meters above sea level. The lowlands slope almost imperceptibly toward the sea. The North Sea portion of the coastline is devoid of cliffs and has wide expanses of sand, marsh, and mud flats (Watten ). The mud flats between the Elbe estuary and the Netherlands border are believed to have been above sea level during Roman history and to have been inundated when the shoreline sank during the thirteenth century. In the western area, the former line of inshore sand dunes became the East Frisian Islands. The mud flats between the islands and the shore are exposed at very low tides and are crossed by innumerable channels varying in size from those cut by small creeks to those serving as the estuaries of the Elbe and Weser rivers. The mud and sand are constantly shifting, and all harbor and shipping channels require continuing maintenance.
The offshore islands have maximum elevations of fewer than thirty-five meters and have been subject to eroding forces that have washed away whole sections during severe storms. Shorelines most subject to eroding tides were stabilized during the late nineteenth and early twentieth centuries.
Although the East Frisian Islands are strung along the coast in a nearly straight line, the North Frisian Islands are irregularly shaped and are haphazardly positioned. They were also once a part of the mainland, and a large portion of the mud flats between the islands and the coast is exposed during low tides.
The Baltic Sea coast of Schleswig-Holstein differs markedly from its North Sea coast. It is indented by a number of small, deep fjords with steep banks, which were carved by rivers when the land was covered with glacial ice. Farther to the east, the Baltic shore is flat and sandy. Rügen, Germany's largest island, lies just offshore of Stralsund.
Wherever the region's terrain is rolling and drainage is satisfactory, the land is highly productive. This is especially true of the areas that contain a very fertile siltlike loess soil, better than most German soils. Such areas, called Börden (sing., Börde ), are located along the southern edge of the North German Lowland beginning west of the Rhine near the Ruhr Valley and extending eastward and into the Leipzig Basin. The Magdeburg Börde is the best known of these areas. Other Börden are located near Frankfurt am Main, northern Baden-Württemberg, and in an area to the north of Ulm and Munich. Because the areas with loess soil also have a moderate continental climate with a long growing season, they are considered Germany's breadbasket.
Central German Uplands
The Central German Uplands are Germany's portion of the Central European Uplands; they extend from the Massif Central in France to Poland and the Czech Republic. Germany's uplands are generally moderate in height and seldom reach elevations above 1,100 meters. The region encompasses all of the Saarland, Hesse, and Thuringia; the north of Rhineland-Palatinate; substantial southern portions of North Rhine-Westphalia, Lower Saxony, and Saxony-Anhalt; and western parts of Saxony.
In the west, the Central German Uplands begin with the Rheinish Uplands, a massive rectangular block of slate and shale with a gently rolling plateau of about 400 meters in elevation and peaks of about 800 to 900 meters. The Rheinish Uplands are divided by two deep and dramatic river valleys--the Moselle and the Rhine. The high hilly area to the south of the Moselle is the Hunsrück; the one to its north is the Eifel. The Rhine separates these areas from their extensions to the east, the Taunus, and, to the north, the Westerwald. To the north and east of the Westerwald are further distinct areas of the Rheinish Uplands, most notably the small range of hills known as the Siebengebirge, across the Rhine from Bonn, and the larger hilly regions--the Siegerland, Bergishes Land, Sauerland, and the Rothaargebirge. The higher elevations of the Rheinish Uplands are heavily forested; lower-lying areas are well suited for the growing of grain, fruit, and early potatoes.
Because of the low elevations of its valleys (200 to 350 meters), the Uplands of Hesse provide an easily traveled passageway through the Central German Uplands. Although not as dramatic as the Rhine Valley, for hundreds of years this passageway--the so-called Hessian Corridor--has been an important route between the south and the north, with Frankfurt am Main at one end and Hanover at the other, and Kassel on the Weser River in its center. The headwaters of the Weser have created a number of narrow but fertile valleys. The highlands of the Uplands of Hesse are volcanic in origin. The most notable of these volcanic highlands are the Rhön (950 meters) and the Vogelsburg (774 meters).
To the north of the Uplands of Hesse lie two low ranges, the Teutoburger Wald and the Wiehengebirge, which are the northernmost fringes of the Central German Uplands. It is at the Porta Westfalica near Minden that the Weser River breaks through the latter range to reach the North German Lowland.
One of the highest points in the Central German Uplands is at Brocken (1,142 meters) in the Harz Mountains. This range is situated about forty kilometers to the northeast of Göttingen and forms the northwestern boundary of the Leipzig Basin, an extension of the North German Lowland. The Harz are still largely forested at lower levels; barren moors cover higher elevations. An important center for tourism in the 1990s, the range was once an important source for many minerals.
The Thüringer Wald, located in southwestern Thuringia, is a narrow range about 100 kilometers long, with its highest point just under 1,000 meters. Running in a northwesterly direction, it links the Central German Uplands with the Bohemian Massif of the Czech Republic and forms the southwestern boundary of the Leipzig Basin. The basin's southeastern boundary is formed by the Erzgebirge range, which extends to the northeast at a right angle to the Thüringer Wald. Part of the Bohemian Massif, the Erzgebirge range reaches 1,214 meters at its highest point.
The southeasternmost portion of the Central German Uplands consists of the Bohemian Forest and the much smaller Bavarian Forest. Both ranges belong to the Bohemian Massif. The Bohemian Forest, with heights up to 1,450 meters, forms a natural boundary between Germany and the Czech Republic.
Between the Central German Uplands and the Alpine Foreland and the Alps lies the geographical region of Southern Germany, which includes most of Baden-Württemberg, much of northern Bavaria, and portions of Hesse and Rhineland-Palatinate. The Main River runs through the northern portion of this region. The Upper Rhine River Valley, nearly 300 kilometers long and about fifty kilometers wide, serves as its western boundary. The Rhine's wide river valley here is in sharp contrast to its high narrow valley in the Rheinish Uplands. The southern boundaries of the region of Southern Germany are formed by extensions of the Jura Mountains of France and Switzerland. These ranges are separate from those of the Central German Uplands. One of these Jura ranges forms the Black Forest, whose highest peak is the Feldberg at 1,493 meters, and, continuing north, the less elevated Odenwald and Spessart hills. Another Jura range forms the Swabian Alb (see Glossary) and its continuation, the Franconian Alb. Up to 1,000 meters in height and approximately forty kilometers wide, the two albs form a long arc--400 kilometers long--from the southern end of the Black Forest to near Bayreuth and the hills of the Frankenwald region, which is part of the Central German Uplands. The Hardt Mountains in Rhineland-Palatinate, located to the west of the Rhine, are also an offshoot of the Jura Mountains.
The landscape of the Southern Germany region is often that of scarp and vale, with the eroded sandstone and limestone scarps facing to the northwest. The lowland terraces of the Rhine, Main, and Neckar river valleys, with their dry and warm climate, are suitable for agriculture and are highly productive. The loess and loam soils of the Rhine-Main Plain are cultivated extensively, and orchards and vineyards flourish. The Rhine-Main Plain is densely populated, and Frankfurt am Main, at its center, serves both as Germany's financial capital and as a major European transportation hub.
Alpine Foreland and the Alps
The Alpine Foreland makes up most of Bavaria and a good part of Baden-Württemberg. The foreland is roughly triangular in shape, about 400 kilometers long from west to east with a maximum width of about 150 kilometers north to south, and is bounded by Lake Constance and the Alps to the south, the Swabian and Franconian albs to the north, and the Bavarian Forest to the east. Elevation within the foreland rises gently from about 400 meters near the Danube, which flows along its north, to about 750 meters at the beginning of the Alpine foothills. With the exception of Munich and the small cities of Augsburg, Ingolstadt, and Ulm, the foreland is primarily rural. Soils are generally poor, with the exception of some areas with loess soil, and much of the region is pasture or is sown to hardy crops.
Germany's portion of the Alps accounts for a very small part of the country's area and consists only of a narrow fringe of mountains that runs along the country's border with Switzerland and Austria from Lake Constance in the west to Salzburg, Austria, in the east. The western section of the German Alps are the Algäuer Alps, located between Lake Constance and the Lech River. The Bavarian Alps, the central section, lie between the Lech and Inn rivers and contain Germany's highest peak, the Zugspitze (2,963 meters). The Salzburg Alps, which begin at the Inn River and encircle Berchtesgaden, make up the easternmost section of Germany's Alps.
The greater part of the country drains into the North Sea via the Rhine, Ems, Weser, and Elbe rivers, which flow in a north-northwest direction. In the east, the Oder River and its tributary, the Neisse River, flow northward into the Baltic Sea and mark the border with Poland. With the exception of the Lahn River, which flows southward before joining the Rhine, most of the tributaries of these rivers flow in a west-to-east or east-to-west direction. In an exception to the south-north pattern of major rivers, the Danube River rises in the Black Forest and flows in a southeasterly direction, traversing Bavaria before crossing into Austria at Passau on the long journey to the Black Sea. The Iller, Lech, Isar, and Inn rivers flow from the south into the Danube and drain the Alpine Foreland.
The Rhine, Germany's longest and most important river, originates in Switzerland, from where it flows into Lake Constance (actually a river basin). At the lake's west end, it begins a long course (800 kilometers) to the Netherlands, at first marking the boundary between Germany and Switzerland and later that between Germany and France. Of the Rhine's three most important tributaries, the Moselle River drains parts of the Rheinish Uplands, the Main drains areas between the Central German Uplands and the Franconian Alb, and the Neckar River drains the area between the Black Forest and the Swabian Alb. Because these rivers keep the Rhine high during the winter and because melting snow in the Alps keeps it high during the spring and summer, the river generally has a high steady flow, which accounts for its being the busiest waterway in Europe.
SOURCE: Library of Congress Country Studies/Area Handbook
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