Dubrow Mountains
| Dubrow Mountains | ||
|---|---|---|
 Dubrow Mountains from the southwest |
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| Highest peak | nameless elevation ( 150 m above sea level ) | |
| location | Langewahl ( Brandenburg , Germany ) | |
| part of | Beeskower plate | |
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| Coordinates | 52 ° 19 ′ N , 14 ° 7 ′ E | |
| Type | Compression moraine | |
| rock | predominantly glacial material ( sand , gravel , bedload and boulders , boulder clay ), interspersed with late Tertiary clods and periglacial deposits | |
| Age of the rock | Saale Ice Age (approx. 140,000 years), overformed in the Vistula Ice Age (approx. 20,000 years), tertiary rocks older than 5 million years | |
The Dubrow Mountains are an elevation ( terminal moraine ) formed during the Ice Age in the state of Brandenburg . They are located about six kilometers southeast of Fürstenwalde / Spree in the Oder-Spree district in the triangle between the municipality of Langewahl , the district of Alt Golm of the municipality of Rietz-Neuendorf and the district of Neu Golm of the municipality of Bad Saarow .
The name is derived from the Sorbian "dub" for oak .
The Dubrow Mountains are well connected to both Berlin and Frankfurt / Oder via the A12 motorway just two kilometers to the north .
A radio tower was erected at its highest point (150 meters above sea level).
The extensive forest and the varied terrain of the Dubrow Mountains and the surrounding area are used by tourists for hiking and cycling. The Easter spring can be found in the Dubrow Mountains near the village of Langewahl.
See also
Web links
Individual evidence
- ↑ SOTA reference list: Summit table ( Memento of the original from February 22, 2014 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice.
