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- Q1475567 subject Q20988094.
- Q1475567 subject Q8530629.
- Q1475567 abstract "The Waalian interglacial (German: Waal-Warmzeit or Waal-Interglazial) (Zagwijn, 1960) was an interglacial in northern Europe that lasted from about 1.45 million to 1.20 million years ago. It thus lies entirely within the Old Pleistocene and is thus part of the Cenozoic. Its name is derived from a major branch of the Rhine delta, the Waal. The Waal warm period could correspond temporally to the Danube-Gunz interglacial of the northern Alpine Foreland.The warm period lies wholly within the Matuyama epoch, in which the earth's magnetic field, with a few exceptions, had a different polarity from that today: the magnetic north pole (actually corresponding to the magnetic south) lay near the geographic south pole.".
- Q1475567 wikiPageExternalLink 763.
- Q1475567 wikiPageWikiLink Q102416.
- Q1475567 wikiPageWikiLink Q1240783.
- Q1475567 wikiPageWikiLink Q1884430.
- Q1475567 wikiPageWikiLink Q20988094.
- Q1475567 wikiPageWikiLink Q216171.
- Q1475567 wikiPageWikiLink Q25546.
- Q1475567 wikiPageWikiLink Q257376.
- Q1475567 wikiPageWikiLink Q487294.
- Q1475567 wikiPageWikiLink Q5845154.
- Q1475567 wikiPageWikiLink Q6500960.
- Q1475567 wikiPageWikiLink Q842763.
- Q1475567 wikiPageWikiLink Q8530629.
- Q1475567 wikiPageWikiLink Q934.
- Q1475567 comment "The Waalian interglacial (German: Waal-Warmzeit or Waal-Interglazial) (Zagwijn, 1960) was an interglacial in northern Europe that lasted from about 1.45 million to 1.20 million years ago. It thus lies entirely within the Old Pleistocene and is thus part of the Cenozoic. Its name is derived from a major branch of the Rhine delta, the Waal.".
- Q1475567 label "Waalian interglacial".