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The landscape is very well served by communications. A cardioid ring motorway runs around the
Leipzig-Halle conurbation, the so-called Central German Loop (
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pits and mining facilities and their conversion into recreation areas, especially north and south of
Leipzig. By flooding some the open-cast mines many
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274:. Although open-cast mining continues in the area, it is also being developed from an environmental and tourist perspective, through the
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97:, large areas were deforested and many rivers and streams canalised or diverted. The Leipzig Bay is bounded to the north by the
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254:(federal roads) run in all directions of the compass, linking the Leipzig Bay with other parts of the country. Only
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This region was originally covered with dense forests and meandering rivers. In the course of urbanization and
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have been and are being created in the
Leipzig Basin, which are gradually changing the face of the landscape.
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The
Leipzig region is historically, culturally and economically of huge importance to
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212:, organic material was also deposited in this basin, which in turn was overlaid by
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material from the mountain ranges was deposited. As a result of the creation of
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is an important transport hub in the eastern German states. Railway lines and
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Utrata Fachwörterbuch: Geographie - Englisch-Deutsch/Deutsch-Englisch
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has no direct access to this region, although work on the unfinished
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Geologische Übersichtskarte 1 : 200,000, Sheet CC 4734 Leipzig
346:"Leipzig | History, Population, & Facts | Britannica"
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lies in the centre of the
Leipzig Bay. Other important towns are
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was formed from these deposits, which is covered by layers of
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to the west. The conurbation formed by the two cities of
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is a very flat, originally lakeless and highly fertile
371:. Bundesanstalt für Geowissenschaften und Rohstoffe
200:was formed as a compensating movement, into which
408:Leipziger Land. Kulturlandschaften Sachsens Bd. 2
335:by Jürgen Utrata (2014). Retrieved 10 Apr 2014.
8:
153:landscape and the southernmost part of the
393:Germany: A regional and economic geography
161:broken only by low eminences such as the
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184:The Leipzig Bay was formed during the
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165:and dissected by the valleys of the
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78:, anchored by the foothills of the
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157:. The landscape is essentially a
262:began in the mid 20th century.
31:Village scenery east of Leipzig
1:
395:(2nd ed.). London: Methuen.
391:Dickinson, Robert E (1964).
296:List of landscapes in Saxony
82:in the northwest and of the
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465:Geography of Saxony-Anhalt
470:Natural regions of Saxony
406:Donath, Matthias (2010).
358:Dickinson (1964), p. 37.
321:Dickinson (1964), p. 29.
45:Leipziger Tieflandsbucht
242:Mitteldeutsche Schleife
105:, to the south by the
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301:Leipzig River Network
246:Leipzig/Halle Airport
149:The Leipzig Bay is a
107:Ore Mountain Foreland
101:, to the east by the
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460:Geography of Leipzig
436:51.0000°N 13.0000°E
432: /
111:Central Saxon Hills
260:Elster-Saale Canal
155:North German Plain
86:in the southeast.
70:, in northwestern
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196:were uplifted, a
188:period. When the
74:and southeastern
16:(Redirected from
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208:and variable
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190:Ore Mountains
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163:Hohburg Hills
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84:Ore Mountains
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76:Saxony-Anhalt
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53:Saxon Lowland
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49:Leipzig Basin
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18:Leipzig Basin
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171:White Elster
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276:reclamation
151:Young Drift
115:River Saale
99:Düben Heath
37:Leipzig Bay
454:Categories
427:13°00′00″E
424:51°00′00″N
414:, Leipzig.
401:B000IOFSEQ
386:Literature
307:References
266:Importance
218:Brown coal
202:weathering
103:River Elbe
284:new lakes
214:sediments
135:Merseburg
131:Eilenburg
127:Delitzsch
93:open pit
57:Saxon Bay
374:Archived
290:See also
236:Location
210:flooding
194:Vogtland
186:Tertiary
181:rivers.
109:and the
280:lignite
278:of old
222:lignite
145:Geology
119:Leipzig
91:lignite
68:Germany
65:Central
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179:Pleiße
177:, and
95:mining
72:Saxony
41:German
230:loess
198:basin
175:Mulde
167:Saale
159:plain
139:Borna
123:Halle
61:plain
47:) or
397:ASIN
228:and
226:sand
206:bogs
192:and
137:and
121:and
35:The
244:).
220:or
63:in
55:or
51:or
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314:^
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39:(
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