GeographieGeologie[Bearbeiten]Das A

Geographie
Geologie[Bearbeiten]
Das Alpenvorland zwischen Kalkalpen und Donau, in dem sich auch München befindet, liegt auf einem tiefen Senkungsbecken, das seit Millionen von Jahren hauptsächlich aus Abtragungen der Alpenaufgefüllt wird. Im Tertiär wurden dort überwiegend Sand- und Geröllmassen durch Flüsse aus den Alpen abgelagert. Während der nachfolgenden Eiszeiten, deren letzte vor etwa 10.000 Jahren endete, bildeten sich im Alpenbereich große Gletscher- und Schmelzwasserströme, die im Voralpenland Moränenhügel und Schotterebenen zurückließen. Die 55 km breite Münchner Ebene, welche an den Endmoränen des Isarvorlandgletschers ansetzt, ist eine schiefe Ebene mit einem Höhenunterschied von 300 Metern zwischen Holzkirchen im Süden und Moosburg im Norden, deren Oberflächenformen in erster Linie durch den würmeiszeitlichen Schotter gebildet werden. Im Süden der Ebene sind die Flüsse, insbesondere die Isar, tief eingeschnitten. Auf diesen Schotterböden findet man wie im Süden von München vermehrt Wälder, wie den Perlacher Forst und den Forstenrieder Park, auch weil der Grundwasserspiegel hier relativ tief liegt. Im Norden der Stadt dagegen, wo sich der Grundwasserspiegel nahe der Oberfläche befindet, liegen große Niedermoore, wie das Dachauer Moos im Nordwesten und das Erdinger Moos im Nordosten.

ผลลัพธ์ (อังกฤษ) 1:

GeographyGeology [edit]The alpine foothills in Munich is located between limestone Alps and Danube, lies on a deep reduction in pool, which is the Alpenaufgefüllt for millions of years of erosion. In the tertiary period there mostly sand and scree were deposited by rivers from the Alps. During the subsequent ice ages, whose letzte ended about 10,000 years ago, large glaciers and meltwater streams that are left behind in the morainic hills of foothills of the and gravel layers formed in the Alpine area. The 55-km-wide Munich plain, which attaches to the end moraines of the ISAR foreland glacier is an inclined plane with a difference of 300 metres between wooden churches in the South and Moosburg in the North, whose surface forms primarily by the würmeiszeitlichen gravel formed are. In the South of the level of the rivers, in particular the ISAR, are deeply cut. On these gravel soils, it takes one more forests, such as the Perlacher Forst and the Forstenrieder Park, and South of Munich also because the water table is relatively deep here. In the North of the city, however, where close to the water table is the surface that are large fens, like the Dachauer Moos in the Northwest and the erdinger Moos in the Northeast.

ผลลัพธ์ (อังกฤษ) 2:

Geography
Geology [edit]
The foothills between Limestone Alps and the Danube, where is also located in Munich, is located on a deep-cutting basin, which is mainly used for millions of years of erosion of the Alps populated. In the Tertiary there predominantly sand and gravel materials were deposited by rivers from the Alps. During the subsequent ice ages, the last of which ended about 10,000 years ago, formed in the Alpine region large glaciers and meltwater streams, which left in the alpine upland moraine and gravel plains. 55 km wide Munich plane which tackles the end moraines of the Isar foothills glacier, is an inclined plane with a height difference of 300 meters between wooden churches in the South and Moosburg in the north, the surface shapes are formed primarily by the würmeiszeitlichen gravel. In the south of the plane are the rivers, especially the Isar, deeply incised. On these gravel soils are found as in the south of Munich increasingly forests as the Perlacher Forst and the Forstenrieder Park, also because the groundwater level here is relatively low. In the north of the city on the other hand, where the water table is near the surface are large fens, as the Dachauer Moos in the northwest and the Erdinger Moos in the Northeast.

ผลลัพธ์ (อังกฤษ) 3:

Geography
geology[EDIT
the foothills of the Alps between Calcareous Alps and the Danube, in the Munich is located, is situated on a deep Senkungsbecken, since millions of years ago, mainly from the Alpenaufgefullt. In the Tertiary era there were predominantly sand and rubble deposited by rivers from the Alps. During the subsequent ice ages, whose last about 10.000 Years expired, formed in the Alpine region, the great glacier and Schmelzwasserstrome Schotterebenen moraine hills and left behind in the foothills of the Alps. The 55-km wide Munich level, what to the terminal moraines of the Isarvorlandgletschers approach, is an inclined plane with an altitude difference of 300 meters between Moosburg Holzkirchen in the south and in the north,The shapes in the first instance by the wurmeiszeitlichen gravel are formed. In the south of the level are the rivers, especially the river Isar, deep cut. You will find on these Schotterboden as more forests in the south of Munich, as the Perlacher Forst and the Forstenrieder Park, also because the groundwater level is relatively low here. However, in the north of the city.Where the groundwater table is located near the surface, are large blanket bogs, such as the Dachauer Moos in the north-west and the Erdinger Moos in the north-east.