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In the sequence of sediments three zones of strata were found, when the most dust was deposited in the crater lake. If these dust-laden layers correspond to the ice advances of the northern German inland ice sheet, by comparing them with the exact chronological sequence of the dust layers in the Maar
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Bernd
Zolitschka; Achim Brauer; Jörg F.W. Negendank; Hagen Stockhausen; Andreas Lang (September 2000), "Annually dated late Weichselian continental paleoclimate record from the Eifel, Germany",
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Paläoklimatische
Bedeutung laminierter Sedimente – Holzmaar (Eifel, Deutschland), Lake C2 (Nordwest-Territorien, Kanada) und Lago Grande di Monticchio (Basilicata, Italien).
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Paläoklimatische
Bedeutung laminierter Sedimente: Holzmaar (Eifel, Deutschland), Lake C2 (Nordwest-Territorien, Kanada) und Lago Grande di Monticchio (Basilicata, Italien)
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has an area of about 6.8 hectares (17 acres), a diameter of 325 metres (1,066 ft) and a depth of 21 metres (69 ft) and lies within a
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The
Holzmaar is fed by a headstream of the Sammetbach which crosses the maar. In the immediate vicinity is another maar, the
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sediments an equally accurate age for local terminal moraines may be possible at suitable locations in northern
Germany.
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238:. The sediments of the Holzmaar go back 23,200 years. This assessment was made possible by comparing the sequence and
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Natur- und
Kulturführer Vulkanlandeifel. Mit 26 Stationen der "Deutschen Vulkanstraße".
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208:, almost completely surrounded by woods. It is one of the two maars making up the
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from which give a comprehensive picture of the climate going back to the
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http://www.schweizerbart.de/publications/detail/artno/011006040
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On its south and southwest shores, the maar has silted up with
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10.1130/0091-7613(2000)28<783:ADLWCP>2.0.CO;2
41:(centre) and Holzmaar (rear). (2015 aerial photograph)
254:(GISP2), but are somewhat at odds with those of the
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chronology is in close agreement with data from the
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320:Trier und Umgebung, Sammlung geologischer Führer
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16:Body of water in Rhineland-Palatinate, Germany
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242:obtained in the maar basin with that of the
340:. Relief Boden Palaeoklima, Vol. 13, 1998.
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196:(2.5 km away to the southwest) and
387:Nature reserves in Rhineland-Palatinate
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308:Gaasterland-Verlag, Düsseldorf. 2006,
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322:, Bd. 60, 3. Auflage, Bornträger,
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318:H. Wolfgang Wagner et al., 2012:
358:Rezension zum Forschungsbericht
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377:Bogs of Rhineland-Palatinate
252:Greenland Ice Sheet Project
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256:Greenland Ice Core Project
150:325 m (1,066 ft)
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192:almost halfway between
188:in the German state of
212:, the other being the
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166:21 m (69 ft)
158:6.8 ha (17 acres)
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190:Rhineland-Palatinate
115:50.11889°N 6.87917°E
82:Rhineland-Palatinate
111: /
382:Maars of the Eifel
336:Bernd Zolitschka,
240:radiometric dating
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346:978-3-443-09013-5
328:978-3-443-15094-5
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120:50.11889; 6.87917
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236:last cold period
210:Gillenfeld Maars
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244:Meerfelder Maar
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352:External links
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186:Volcanic Eifel
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163:Average depth
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232:core samples
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184:lies in the
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176:The Holzmaar
155:Surface area
35:Hitsche Maar
392:Vulkaneifel
221:Dürres Maar
118: /
93:Coordinates
39:Dürres Maar
371:Categories
299:Literature
266:References
214:Pulvermaar
194:Gillenfeld
147:Max. width
330:, (see:)
228:sediments
106:6°52′45″E
258:(GRIP).
182:Holzmaar
103:50°7′8″N
78:Location
66:Holzmaar
37:(front)
22:Holzmaar
281:Geology
198:Eckfeld
86:Germany
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200:. The
248:varve
362:1998
342:ISBN
324:ISBN
310:ISBN
202:maar
180:The
137:Maar
132:Type
33:The
285:doi
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