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| China Restaurant Lee Peng
Simeonstraße 41a
54290 Trier
Anbieter auf der Karte zeigen
restaurants
Phone: 0651 - 40088
Fax: 0651 - 40088
When making a phone inquiry, please always refer to"Vacation in Rhineland-Palatinate"
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Unfortunately this offerer published non but a german text. For translation: www.google.com
china á la carte
LEE PENG
Das China-Restaurant liegt in absolut zentraler Lage in der Fußgängerzone. Neben chinesischen "á la carte"-Spezialitäten bietet das Restaurant Lee Peng jeden Tag, mit Ausnahme des Sonntags, ein großes, reichhaltiges Mittagsbuffet an, bei dem sich die Gäste aus nicht weniger als 40 Komponenten ihre kulinarischen Favoriten selbst zusammenstellen können.
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Schedule of events for
Trier |
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Moselle, Eifel |
District: Trier-Saarburg | Verbandsgemeinde: Trier
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Vacation
In the holiday region
Eifel |
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Vacation in the Eifel |
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| Tourismus am Vulkan - die Maare der Eifel |
The Eifel is a low volcanic mountain range in western Germany. It occupies parts of southwestern North Rhine-Westphalia and northwestern Rhineland-Palatinate.
The Eifel is bordered by the Moselle River in the south and the Rhine in the east. In the north it is continued by the hills of the High Venn (Hohes Venn), in the west by the Ardennes. (Ardennes and Eifel are actually the same ...
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| Tourismus am Vulkan - die Maare der Eifel |
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| Die Oberburg in Manderscheid |
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| Formel 1-Rennstrecke Nürburgring |
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| Nostalgie-Urlaub mit der Eifelquerbahn |
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The Eifel is a low volcanic mountain range in western Germany. It occupies parts of southwestern North Rhine-Westphalia and northwestern Rhineland-Palatinate.
The Eifel is bordered by the Moselle River in the south and the Rhine in the east. In the north it is continued by the hills of the High Venn (Hohes Venn), in the west by the Ardennes. (Ardennes and Eifel are actually the same geological region. They are a single volcanic field.)
In the Tertiary geological era, the Eifel was a site of extensive volcanic activity. Some of the hills are volcanic vents. The lakes of the regions are former volcanic craters (maars). The last eruptions took place around 10 000 years ago. The volcanism of the Eifel is caused by a hotspot, a place where hot material form deep in the mantle rises to the surface. Research has shown that the mantle plume is still active; the Eifel region is rising by 1-2 mm per year. Historically, the Eifel volcanoes had inactive phases of 10 000 to 20 000 years between active phases, suggesting there is a possibility of future eruptions.
Source: www.wikipedia.com
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| Holiday destinations within a radius of
5 km
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