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322:) about 30 million years ago during the evolution of the Upper Rhine Graben. The Upper Rhine Graben Sea and Upper Rhine Graben Lake also covered the Hanau-Seligenstadt Basin. Debris from the local highlands caused silting up and development of a river plain during the
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In the Hanau-Seligenstadt Basin sand, gravel and clay are dug in many pits. Until the 1930s also lignite and until the 1980s
Miocene basalts were mined. The sand and gravel deposits are yielding
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Lang, Stefan (2007): Die geologische
Entwicklung der Hanau-Seligenstädter Senke (Hessen, Bayern).– Elektronische Publikationen Darmstadt (EPDA), 782, 97 S., 51 Abb., 5 Tab., Anhang.
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rivers started once again to incise into their former sediments. The individual stages of the incision history are preserved as
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the later Hanau-Seligenstadt Basin was a non-depositional region. Subsidence started latest during the
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The Hanau-Seligenstadt Basin is located in the eastern part of the Lower Main lowlands. The river
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mountains. Towards the north the graben margins converge. The basin sediments rest on top of the
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The Hanau-Seligenstadt Basin is separated from the Upper Rhine Graben to the west by a
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developed. The still relatively short river Main tapped the Upper Main in the early
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Die geologische
Entwicklung der Hanau-Seligenstädter Senke (Hessen, Bayern)
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flows over parts of the area. Still during the
Langhian, rivers started to
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427:(Ph.D. Thesis) (in German). Darmstadt: Technische Universität Darmstadt.
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mountains form its eastern margin. To the south it is bounded by the
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basin sediments reach more than 280 m in thickness. Marine,
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412:https://tuprints.ulb.tu-darmstadt.de/782/
77:Learn how and when to remove this message
326:. About 15 million years ago during the
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345:about 5 million years ago the Lower
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417:Lang, Stefan (15 February 2007).
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286:river deposits consist of sand,
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341:their former sediments. In the
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209:European Cenozoic Rift System
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460:Cenozoic rifts and grabens
172:crosses the basin between
164:Panorama view of the basin
116:Frankfurt am Main, Germany
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250:and finally terrestrial
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93:Hanau-Seligenstadt Basin
32:This article includes a
61:more precise citations.
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144:is a subbasin of the
450:Geography of Bavaria
294:, in Pliocene also
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146:Upper Rhine Graben
124:Upper Rhine Graben
34:list of references
330:volcanoes poured
266:with interbedded
178:Offenbach am Main
150:Frankfurt am Main
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455:Regions of Hesse
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196:Geologic setting
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67:January 2022
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53:Please help
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465:Upper Rhine
375:Pleistocene
365:layers and
218:block. The
59:introducing
16:River Basin
444:Categories
397:References
371:Quaternary
284:Quaternary
260:limestones
244:Quaternary
385:Resources
316:Oligocene
312:Paleogene
306:Evolution
272:Oligocene
240:Oligocene
391:aquifers
343:Pliocene
332:basaltic
328:Langhian
320:Rupelian
280:Pliocene
236:Triassic
228:Variscan
224:Odenwald
220:Spessart
202:Cenozoic
156:Location
134:Cenozoic
113:Location
367:lignite
324:Miocene
296:lignite
276:Miocene
238:rocks.
232:Permian
190:Dieburg
121:Part of
55:improve
355:gravel
288:gravel
278:. The
268:basalt
248:limnic
205:graben
339:erode
264:sands
256:marls
252:clays
216:horst
182:Hanau
101:Basin
40:, or
363:clay
359:silt
357:and
351:sand
347:Main
335:lava
292:silt
290:and
282:and
274:and
262:and
188:and
176:and
170:Main
140:The
429:urn
242:to
234:to
130:Age
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