Immerather Maar, Immerath, Daun, Vulkaneifel, Rhineland-Palatinate, Germanyi
| Regional Level Types | |
|---|---|
| Immerather Maar | Crater Lake |
| Immerath | Municipality |
| Daun | Collective Municipality |
| Vulkaneifel | District |
| Rhineland-Palatinate | State |
| Germany | Country |
Immerather Maar, Eifel Volcanic Fields, Germany
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Latitude & Longitude (WGS84):
50° 7' 20'' North , 6° 57' 32'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Immerath | 263 (2011) | 1.4km |
| Strotzbüsch | 370 (2016) | 2.6km |
| Strohn | 493 (2011) | 3.1km |
| Winkel | 179 (2015) | 3.1km |
| Lutzerath | 1,463 (2017) | 3.5km |
Other Languages:
German:
Immerather Maar, Immerath, Verbandsgemeinde Daun, Landkreis Vulkaneifel, Rheinland-Pfalz, Deutschland
Cebuano:
Immerather Maar, Immerath, Vulkaneifel, Rheinland-Pfalz, Alemanya
Egyptian Arabic:
بحيره ايميراثير مار, المانيا
The Immerather Maar is a maar in the municipality of Immerath in the county of Vulkaneifel in the German state of Rhineland-Palatinate. It is part of a designated nature reserve and Special Area of Conservation.
The maar was formed by volcanic activity about 40,000 to 70,000 years ago. Around 1750, the maar was drained by a maar stream and dried out so that most of it could be used as pastureland. The area of the maar was even divided into plots. Between 1914 and 1918, the stream was wild. These events led to it being blocked and the formation of a shallow maar. The height of the water surface has changed little since then.
The Immerather Maar is the smallest and shallowest of the Eifel maar lakes. It is located at a height of 368.1 metres above sea level (NN). Its surface area is about 60,000 square metres (650,000 sq ft), and its volume is about 90,000 cubic metres (3,200,000 cu ft). It has a depth of up to 2.9 metres (9 ft 6 in), the average depth being approximately 1.50 metres (4 ft 11 in). The lakebed is flat and level, and there are only obstacles, in the form of fallen trees and tree stumps, in the water near the shores. The ground drops evenly from the shore towards the middle of the maar, except in the area of the outlet where there is a step, the water depth rising from 0.6 metres to 2.8 metres over a distance of 5 metres. The turbidity of the water has reduced in recent years due to increasing plant growth and now varies between 0.25 and 2.0 metres depending on the season. The water has a renewal time of 0.3 years. The maar does not have an above-ground inflow but is fed exclusively by surface and ground water in the crater. It has a catchment of 640,000 square metres (6,900,000 sq ft). The shoreline is 800 metres (2,600 ft) long.
The Immerather Maar is mainly a recreational area. Anglers use the waters due to their abundant fish population.
Two large fish die-offs in the last few years have almost wiped out the stock of bream. The remaining fish species are rudd, perch, pike, tench, carp, and eel.
The Regierungsbezirk of Trier designated the Immerather Maar and its shore area as a nature reserve on 12 June 1979. The purpose of the protection is to preserve the typical character of the maar in its entirety, including the natural vegetation along the banks of the river, and to preserve its fauna and flora. The protected area covers an area of 61.29 hectares.
List of minerals for each chemical element
Other Databases
| Wikipedia: | https://en.wikipedia.org/wiki/Immerather_Maar |
|---|---|
| Wikidata ID: | Q1458718 |
| GeoNames ID: | 3207745 |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
- Rheno-Hercynian BeltOrogenic Belt
EuropeContinent
- Rhenish MassifMassif
Germany
- Eifel Volcanic FieldsGroup of Volcanic Fields
- West Eifel Volcanic FieldVolcanic Field
Germany/Belgium
- Eifel MountainsMountain Range
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