saalian造句

• Saalian sediments uncomfortably overlie this paleosol.
• The region is part of the Saalian glaciation meltwater valley or " urstromtal ".
• The Veluwe was formed by the Saalian glacial during the Pleistocene epoch, some 200, 000 years ago.
• The oldest occupation phases present at Veldwezelt-Hezerwater should be seen in relation to the Late Saalian rock-fall deposits.
• The basis of the terrain is largely formed from the moraines and meltwater deposits of the Saalian glaciation, the penultimate glaciation period of the pleistocene era.
• However, on stratigraphic grounds, we think that it is safe to say that they should be dated to the Late Saalian Zeifen Interstadial ( MIS 6.01 ).
• During the Saalian Stage ( 230, 000 130, 000 years ago ) the area of the present-day L黱eburg Heath was covered three times by a continental ice sheet.
• The oldest known Pleistocene sediments exposed in the southern sea cliffs of Bolshoy Lyakhovsky Island consist of Saalian sediments, which accumulated between 200, 000 and 120, 000 years ago.
• The lower part of these sediments consist of ice-rich, silty and silty-sandy sediments that accumulated as an Saalian ice complex between 200, 000 and 170, 000 years ago.
• Eemian lake sediments fill depressions, i . e . ice wedge casts and thermokarst lakes, which developed by the surficial thawing during Eemian interglacial climates of Saalian ice-wedges and other permafrost.
• The Lusatian Border Ridge and the Muskau Fold Arc consist of about 150, 000 year old shove end moraine arcs of the Warthe Stage of the Saalian glaciation, that are characterized by several parallel valleys and ridges.
• The upper part of the Saalian sediments, which lie uncomfortably on the eroded surface of the lower Saalian ice complex deposits, consists of well-sorted fine-grained sand that contains pollen characteristic of sparse grass-sedge dominated interstadial vegetation and less ground ice.
• The upper part of the Saalian sediments, which lie uncomfortably on the eroded surface of the lower Saalian ice complex deposits, consists of well-sorted fine-grained sand that contains pollen characteristic of sparse grass-sedge dominated interstadial vegetation and less ground ice.
• This phenomenon seems to play a key role at the " Lower-Sites " at Veldwezelt-Hezerwater during the Late Saalian to Eemian s . s . climatic shift ( late MIS 6 to MIS 5e ), with in general the presence of very small tools s . s.
• Although there are a few exceptions, we can state that at Veldwezelt-Hezerwater, from the Late Saalian ( late MIS 6 ) onwards, the general trend in the Middle Palaeolithic succession of lithic artefacts and tools is that they seem to increase in size through the Middle Palaeolithic.