Laacher See
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| Laacher See Loch Laach | |
|---|---|
 View o the caldera | |
  Laacher See Loch Laach Location in Germany | |
| Location | Ahrweiler, Rhineland-Palatinate |
| Coordinates | 50°25′N 7°16′E / 50.417°N 7.267°ECoordinates: 50°25′N 7°16′E / 50.417°N 7.267°E |
| Teep | Volcanic caldera loch |
| Primary inflows | None |
| Primar ootflows | Fulbert-Stollen (canal) |
| Basin kintras | Germany |
| Max. lenth | 1.964 km (1.220 mi) |
| Max. weenth | 1.186 km (0.737 mi) |
| 3.3 km2 (1.3 sq mi) | |
| Average deepth | 31 m (102 ft) |
| Max. deepth | 51 m (167 ft) |
| 103,000,000 m3 (0.025 cu mi) | |
| Shore lenth1 | 7.3 km (4.5 mi) |
| Surface elevation | 275 m (902 ft) |
| Islands | None |
| 1 Shore lenth is nae a weel-defined meisur. | |
Laacher See (leeterally: Loch Laach; German pronunciation: [ˈlaːxɐ ˈzeː]) is a volcanic caldera loch locatit in Rhineland-Palatinate, Germany.[1][2]
The diameter is 2 km (1.2 mi), an it is locatit 24 km (15 mi) from Koblenz, 8 km (5.0 mi) from Andernach an the Rhine river, an 37 km (23 mi) from Bonn. Its last volcanic eruption, which wis a Plinian eruption, wis aroond 11,000 B.C., wi a Volcanic Explosivity Index (VEI) o 6, havin the same magnitude as the Plinian eruption o Munt Pinatubo in 1991. It is pairt o the Eifel region, an the East Eifel Volcanic Region, which wis formed after the collision o the African an Eurasian continents millions o yeirs ago.[3][4][5] Bubbles o odorless CO2 gas called mofettas are released from the loch, which means that the volcanae is dormant. Tae the west o the loch is the Maria Laach Aibey, built in 1092 by Henry II o Laach, Coont o the Hoose o Luxembourg.
References
[eedit | eedit soorce]- ↑ Oppenheimer, Clive (2011). Eruptions that Shook the World. Cambridge University Press. pp. 216–217. ISBN 978-0-521-64112-8.
- ↑ de Klerk, Pim; et al. (2008). "Environmental impact of the Laacher See eruption at a large distance from the volcano: Integrated palaeoecological studies from Vorpommern (NE Germany)". Palaeogeography, Palaeoclimatology, Palaeoecology. 270 (1–2): 196–214. Bibcode:2008PPP...270..196D. doi:10.1016/j.palaeo.2008.09.013.
- ↑ Bogaard, Paul van den (1995). "40Ar/39Ar ages of sanidine phenocrysts from Laacher See Tephra (12,900 yr BP): Chronostratigraphic and petrological significance". Earth and Planetary Science Letters. 133 (1–2): 163–174. Bibcode:1995E&PSL.133..163V. doi:10.1016/0012-821X(95)00066-L.
- ↑ "Geo-Education and Geopark Implementation in the Vulkaneifel European Geopark/Vulkanland Eifel National Geopark". The Geological Society of America. 2011. Archived frae the original on 13 Januar 2019. Retrieved 9 Mairch 2022.
- ↑ Reinig, Frederick; Wacker, Lukas; Jöris, Olaf; Oppenheimer, Clive; Guidobaldi, Giulia; Nievergelt, Daniel; et al. "Precise date for the Laacher See eruption synchronizes the Younger Dryas".
[Measurements] firmly date the [Laacher See eruption] to 13,006 ± 9 calibrated years before present (BP; taken as AD 1950), which is more than a century earlier than previously accepted.
Freemit airtins
[eedit | eedit soorce] |
Wikimedia Commons haes media relatit tae Laacher See. |
- Continuous event display of the 10 most recent registered seismic activities measured from the Laacher See
- Apokalypse im Rheintal (Cornelia Park und Hans-Ulrich Schmincke)
- Martin Hensch, etal.: Deep low-frequency earthquakes reveal ongoing magmatic recharge beneath Laacher See Volcano (Eifel, Germany). Geophys. J. Int. (2019) 216, 2025–2036 doi:10.1093/gji/ggy532
- Michael W. Förster, Frank Sirocko: Volcanic activity in the Eifel during the last 500,000 years: The ELSA-Tephra-Stack .Global and Planetary Change (2016) (PDF)
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