Situ Laacher
Situ Laacher atawa Laacher See (pronunsiasi basa Jérman: [ˈlaːxɐ ˈzeː]), nyaéta hiji vulkanik situ kaldera kalayan diaméter 2km di Rhineland-Palatinate, Jerman, kira-kira 24km kalér-kuloneun Koblenz, 37km kiduleun Bonn, jeung 8km kuloneun Andernach. Éta aya di pagunungan Eifel, sareng mangrupikeun bagian tina médan vulkanik Eifel Wétan dina Volcanic Eifel anu langkung ageung. Danau ieu kabentuk ku bitukan Plinian kira-kira 13.000 taun BP kalayan Indéks Explosivity Volcanic (VEI) tina 6, dina skala anu sarua jeung Buluna Pinatubo bitu taun 1991.[1][2][3][4] turunna vulkanik bisa dititénan salaku mofetta di basisir tenggara danau mangrupa tanda. tina dormant vulkanisme.
Lokasi | Ahrweiler, Rhineland-Palatinate |
---|---|
Koordinat | 50°24′45″N 07°16′12″E / 50.41250°N 7.27000°EKoordinat: 50°24′45″N 07°16′12″E / 50.41250°N 7.27000°E |
Rupa dano | danau kaldera vulkanis |
Aliran kaluar utama | Fulbert-Stollen (kanal) |
Aya di nagara | Jerman |
Aréa paroman | 3.3 km2 |
Maksimal jero | 53 m |
Kaluhuran paroman | 275 m |
Deskripsi
éditSitu ieu wangunna lonjong jeung dikulilingan ku sisi anu luhur. Lavana digali pikeun batu kilangan ti jaman Romawi nepi ka diwanohkeunana rol besi pikeun ngaggiling siki-sikian.[5]
Di sisi kulon aya Benedictine Maria Laach Abbey (Abbatia Lacensis), diadegkeun taun 1093 ku Henry II of Laach ti House of Luxembourg, kahiji Count Palatine of the Rhine, anu kagungan puri na sabalikna ka biara luhureun sisi situ wétan.
Situ ieu teu boga jalan kaluar alam tapi digaringkeun ngaliwatan torowongan anu digali samemeh taun 1170 jeung diwangun deui sababaraha kali saenggeusna. Nu diyakinan geus ngawangun eta situ antara taun 1152–1177 nyaéta nu ngaranna Fulbert, nu mangrupa ngaran saurang abbas biara tina biara pangdeukeutna ti éta tempat.
Rujukan
édit- ↑ Oppenheimer, Clive (2011). Eruptions that Shook the World. Cambridge University Press. pp. 216–217. ISBN 978-0-521-64112-8.
- ↑ de Klerk, Pim (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. Diarsipkan dari versi asli tanggal 13 January 2019. Diakses tanggal 8 January 2013. Archived 13 Januari 2019 di Wayback Machine
- ↑ Hull, Edward (1892). Volcanoes: Past and Present (2010 ed.). Echo Library. pp. 73–74. ISBN 9781406868180. Diarsipkan dari versi asli tanggal 28 April 2022. Diakses tanggal 2 December 2021.
Tutumbu luar
éditWikimedia Commons mibanda média séjénna nu patali jeung 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)