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The Saale glaciation or Saale Glaciation, sometimes referred to as the Saalian glaciation, Saale cold period (German: Saale-Kaltzeit), Saale complex (Saale-Komplex)... |
complex (MIS 21-13 ?) Elster glaciation (MIS 10, perhaps also MIS 12 ?) Holstein interglacial (MIS 9 ?) Saale glaciation (ended with MIS 6) Eem interglacial... |
Riss and Würm glaciations. The greatest ice advance into the Alpine Foreland took place during the Riss glaciation, cf. the Saale glaciation in northern... |
interglacial, which was followed Saale glaciation. The glacial period is named after the White Elster, a right tributary of the Saale. Traditionally, Elster was... |
Teltow (region) (section Saale glaciation) strata are overlain by the very thick (40 metres or more) sediments of the Saale ice age. These are usually the depositions of proglacial lakes or glacial... |
years ago and 347,000 to 128,000 years ago. It coincides with the Saale glaciation of North Germany. The name goes back to Albrecht Penck and Eduard Brückner... |
(MIS 12, Elster glaciation), pre-Neanderthals sensu lato (MIS 11–9, Holstein interglacial), early Neanderthals (MIS 7–5, Saale glaciation–Eemian), and classic... |
warm period. It followed directly after the Elster glaciation and came before the Saale glaciation, during the Middle Pleistocene. The more precise timing... |
Ice age (section Effects of glaciation) called Quaternary glaciation. Individual pulses of cold climate within an ice age are termed glacial periods (glacials, glaciations, glacial stages, stadials... |
foothills: The Saale glaciation corresponds there to the Riss glaciation; the Weichselian glaciation corresponds to the Würm glaciation. The Alps are a... |
a thin Holocene layer that overlies a thicker layer dating to the Saale glaciation, with an Upper Cretaceous layer underlying the Pleistocene layer. The... |
mammoths survived an even greater loss of habitat at the end of the Saale glaciation 125,000 years ago, and humans likely hunted the remaining populations... |
discuss] In the east of the Netherlands, remains are found of the Saale glaciation, which ended approximately 130,000 years ago. As the continental ice... |
though, it was formed in the Saale glaciation period about 150,000 years ago. During the subsequent Weichselian glaciation – only about 10,000 years ago... |
during the Saale glaciation. The structure of the valley is however clearly older and was formed by recent tectonics. In the Alpine glaciation zone of Central... |
Whilst the majority of Old Drift moraines were formed during the Saale glaciation about 130,000 to 140,000 years ago, the Young Drift moraines in Central... |
was surrounding by sandy meltwater depositions and moraines of the Saale glaciation (Pleistocene), such as the geest ridges of the Hohe Lieth to the west... |
eastern edge of the Lüneburg Heath, its appearance shaped during the Saale glaciation. Here the countryside is dominated by the ridge of the Drawehn, which... |
system located here during the Dnieper Ice Age (corresponds to the Saale glaciation in northern Central Europe). Outcrops of blue marl, a rare siliceous... |
belonged to the Elster glaciation. A covering of boulder clay was deposited over the outwash sands during the Saale glaciation, or more precisely the... |