30:
94:
344:
210:, in southeast Berlin are part of the Teltow. From a geological standpoint they certainly are, because the hills have a similar development history. However, these upland remnants are completely isolated within the Berlin Urstromtal. If the River Dahme is taken as the eastern boundary of the Teltow the Müggelberge are neither part of the Teltow geologically nor from a cultural landscape perspective.
112:
247:
is only found at a depth of 45 m (148 ft) (about 0 metres (0 ft) above NN). The gypsum hill is also of historic scientific interest, because it was here, in 1867, that the first borehole in the world to reach a depth of 1,000 metres (3,300 ft) was drilled. The
283:
have virtually no impact on the current appearance of the Teltow, the subsurface, sandy, gravelly sediments of the so-called Berlin Elbe course occur over a wide area. These deposits formed between the Elster and
Saalian ice advances, when the
31:
503:. Landesamt für Geowissenschaften und Rohstoffe Brandenburg (heute Landesamt für Bergbau, Geologie und Rohstoffe Brandenburg, LBGR) 2002, 2. Aufl., 142 S., 43 Karten,
154:
is also counted as part of the Teltow, although it has no clear boundaries. The regional border in the south is unclear, because the ground moraines here were often eroded by
315:. At several points they even break through the Weichselian deposits and are immediately on, or at least very close to, the earth's surface (for example, in Glienick near
328:
268:
532:
192:
161:
72:
490:
297:
359:
pushed southwards right over the Teltow before reaching the northern edge of the Baruth
Urstromtal, the limit of its expansion to the south.
372:
224:
57:
364:
243:. Because all the readily soluble salts have been leached out, only a solution residue has been left on the surface of the gypsum.
119:
The Teltow is not a unified region, either from a historical or a landscape perspective. The present-day term is defined by an
115:
The natural regional location of the Teltow: the plateau is highlighted by a red border, the wider region by a red dotted line
160:
processes. For example, there are many small island plateaux. The boundary of the cultural landscape is general seen as the
292:
and crossed the area of the Fläming which did not yet exist. These sediments are of great economic importance, both as
523:
508:
458:
436:
404:
576:
351:
Today's Teltow plateau in
Brandenburg-Berlin was formed around 20,000 years ago during the Brandenburg stage of
296:
conduits and for the building materials industry. But they only outcrop at a small sand pit at
Lindenberg near
131:
581:
130:
elements. Its natural northern border is defined by the range of the
Tempelhofer Berge, among them the
571:
24:
263:
to 1957 in several quarries. Other salt domes, which do not quite reach the surface, occur under
227:
hill on the northern rim of the Baruth
Urstromtal. Uniquely for Brandenburg, the hill is made of
444:
Der Kreis Teltow, seine
Geschichte, seine Verwaltung, seine Entwicklung und seine Einrichtungen.
331:
near Königs-Wusterhausen in the second half of the 19th and the first half of the 20th century,
271:
lake. For the geological structure of the Teltow, they are of secondary significance, however.
379:. To the north are ground moraines that have been deposited over a large area. Only south of
67:(1239–1245) the question of territorial lordship of the newly created heart of the expanding
53:
8:
352:
249:
77:
417:
303:
The old Elbe strata are overlain by the very thick (40 metres or more) sediments of the
52:. As an historical region, the Teltow was one of the eight territories out of which the
83:
519:
504:
454:
432:
400:
68:
41:
360:
429:
Geologische Übersichtskarte des Landes
Brandenburg 1:300.000 – Erläuterungen.
399:
Teil 4. Spreeland. Blankensee. Ullstein, Frankfurt am Main/Berlin, Ausgabe 1998,
308:
93:
62:
493:. Verlag von Karl Siegismund Königlich Sächsischer Hofbuchhändler, Berlin 1913.
151:
280:
196:
127:
82:; in addition a town immediately south of Berlin, in the present-day county of
203:
565:
547:
534:
375:. However, the line of terminal moraines is very patchy and is traces out an
304:
172:
139:
135:
380:
320:
312:
368:
293:
264:
260:
71:
was finally decided here. Between 1835 and 1952 there was also a county,
45:
332:
207:
156:
165:
376:
356:
244:
240:
236:
232:
338:
324:
176:
383:, does the contiguous ground moraine plateau of the Teltow begin.
134:
rising to 66 m (217 ft), along the southern bank of the
123:
120:
37:
343:
316:
289:
253:
239:
has pushed through all the more recent deposits here to form a
228:
188:
184:
87:
49:
473:
Brandenburgisches
Namenbuch, Teil 3, Die Ortsnamen des Teltow.
56:
was formed in the 12th and 13th centuries. As a result of the
327:
deposits are found at the surface in places. For example, in
147:
143:
424:
Verwaltungsbezirk Berlin-Steglitz (Hrsg.) 1953. (Broschüre)
285:
223:
One geological feature is the 80-metre (260 ft) high
150:
to the west. To the southwest, the countryside around the
111:
206:
hills, which are up to 115 m (377 ft) above
487:
Groß Berliner Kalender, Illustriertes Jahrbuch 1913.
288:flowed northwards from the location of present-day
213:
138:. To the east the borders are formed by the rivers
499:Werner Stackebrandt und Volker Manhenke (Hrsg.):
415:Zur quartären Schichtenfolge des Teltow-Plateaus.
563:
339:Weichsel glaciation and post-glacial development
171:The Havel river separates the Teltow from the
483:Aus der Vergangenheit des Kreises Teltow.
279:While the deeply buried sediments of the
256:/100 metres; this was also a first.
466:Steglitz in Vergangenheit und Gegenwart.
427:L. Lippstreu, N. Hermsdorf, A. Sonntag:
363:can be found there, for example, around
342:
164:. Further south is the heathland of the
110:
101:
92:
518:2. Aufl. Böhlau Verlag, Köln 2003
422:Das Bäketal in vorgeschichtlicher Zeit.
397:Wanderungen durch die Mark Brandenburg.
307:. These are usually the depositions of
564:
475:Hermann Böhlaus Nachf., Weimar, 1972.
347:Geological overview map of the Teltow
259:Sperenberg gypsum was mined from the
202:It is, however, disputed whether the
97:Typical old sand avenue in the Teltow
23:
323:the underlying sediments strongly,
274:
13:
501:Atlas zur Geologie von Brandenburg
14:
593:
449:Carsten Rasmus, Bettina Rasmus:
214:Geology, geomorphology and soils
468:Kulturbuch Verlag, Berlin 1968.
183:feature, separates it from the
453:. KlaRas-Verlag, Berlin 2002,
1:
389:
252:was found to be about 3
195:forms the boundary with the
175:to the northwest. The Nuthe-
7:
106:
10:
598:
218:
548:52.3666667°N 13.3333333°E
319:). Because the Saale ice
191:in the southwest and the
126:that consists mainly of
44:in the German states of
231:. The rising column of
36:) is both a geological
577:Regions of Brandenburg
553:52.3666667; 13.3333333
348:
116:
98:
346:
114:
102:Geography and geology
96:
21:German pronunciation:
471:Gerhard Schlimpert:
371:(Weinberg) and near
54:March of Brandenburg
582:Geography of Berlin
544: /
514:Lutz Partenheimer:
495:Zitat S. 212f.
451:Berliner Umland Süd
353:Weichsel glaciation
250:geothermal gradient
477:Zitat S. 187.
349:
199:in the northeast.
117:
99:
84:Potsdam-Mittelmark
516:Albrecht der Bär.
496:
478:
442:Adolf Hannemann:
420:Herbert Lehmann:
410:
395:Theodor Fontane:
361:Terminal moraines
193:Berlin Urstromtal
162:Baruth Urstromtal
142:, as well by the
86:, bears the name
42:historical region
25:[ˈtɛltoː]
589:
559:
558:
556:
555:
554:
549:
545:
542:
541:
540:
537:
494:
476:
409:Zitat Seite 274.
408:
309:proglacial lakes
275:Saale glaciation
81:
66:
35:
34:
33:
27:
22:
597:
596:
592:
591:
590:
588:
587:
586:
572:Teltow (region)
562:
561:
552:
550:
546:
543:
538:
535:
533:
531:
530:
481:Wilhelm Spatz:
392:
386:
355:. The Weichsel
341:
335:was extracted.
277:
221:
216:
187:plateau of the
109:
104:
75:
73:Teltow district
60:
29:
28:
20:
12:
11:
5:
595:
585:
584:
579:
574:
528:
527:
512:
497:
479:
469:
462:
447:
440:
431:Potsdam 1997,
425:
418:
413:N. Hermsdorf:
411:
391:
388:
340:
337:
281:Elster Ice Age
276:
273:
220:
217:
215:
212:
208:sea level (NN)
197:Barnim Plateau
128:ground moraine
108:
105:
103:
100:
9:
6:
4:
3:
2:
594:
583:
580:
578:
575:
573:
570:
569:
567:
560:
557:
525:
524:3-412-16302-3
521:
517:
513:
510:
509:3-9808157-0-6
506:
502:
498:
492:
491:Ernst Friedel
488:
484:
480:
474:
470:
467:
464:Max Philipp:
463:
460:
459:3-933135-10-9
456:
452:
448:
445:
441:
438:
437:3-7490-4576-3
434:
430:
426:
423:
419:
416:
412:
406:
405:3-548-24381-9
402:
398:
394:
393:
387:
384:
382:
378:
374:
370:
366:
362:
358:
354:
345:
336:
334:
330:
326:
322:
318:
314:
310:
306:
305:Saale ice age
301:
299:
295:
291:
287:
282:
272:
270:
266:
262:
257:
255:
251:
246:
242:
238:
234:
230:
226:
211:
209:
205:
200:
198:
194:
190:
186:
182:
178:
174:
173:Nauen Plateau
169:
167:
163:
159:
158:
153:
149:
145:
141:
137:
133:
129:
125:
122:
113:
95:
91:
89:
85:
79:
74:
70:
64:
59:
55:
51:
47:
43:
39:
32:
26:
18:
529:
515:
500:
486:
482:
472:
465:
450:
446:Berlin 1931.
443:
428:
421:
414:
396:
385:
381:Ludwigsfelde
350:
329:Schenkendorf
313:glacial till
302:
278:
258:
222:
201:
180:
179:Lowland, an
170:
155:
152:Pfefferfließ
118:
16:
15:
551: /
369:Luckenwalde
294:groundwater
265:Mittenwalde
261:Middle Ages
204:Müggelberge
76: [
61: [
46:Brandenburg
40:and also a
566:Categories
539:13°20′00″E
536:52°22′00″N
390:Literature
373:Sperenberg
333:brown coal
269:Blankensee
225:Sperenberg
181:urstromtal
157:urstromtal
58:Teltow War
377:ice front
365:Dobbrikow
357:ice sheet
298:Jühnsdorf
245:Rock salt
241:salt dome
233:Zechstein
132:Kreuzberg
325:Tertiary
267:and the
177:Nieplitz
107:Boundary
219:Bedrock
166:Fläming
124:plateau
121:ice age
38:plateau
522:
507:
489:Hrsg.
457:
435:
403:
321:shoved
317:Zossen
290:Torgau
229:gypsum
189:Zauche
185:sander
88:Teltow
50:Berlin
17:Teltow
235:-age
148:Nuthe
144:Havel
140:Dahme
136:Spree
80:]
69:march
65:]
520:ISBN
505:ISBN
485:In:
455:ISBN
433:ISBN
401:ISBN
286:Elbe
237:salt
146:and
48:and
367:in
311:or
568::
407:.
300:.
168:.
90:.
78:de
63:de
526:.
511:.
461:.
439:.
254:K
19:(
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
