Saalen.

/ˈzɑːlə/

Etymology: < the name of the River Saale in Germany.

Geology.

Used attributively with reference to the third (penultimate) glaciation of the Pleistocene epoch in northern Europe, equivalent to the Riss glaciation in the Alps.

ΘΚΠ

the world > the earth > structure of the earth > age or period > [adjective] > quaternary > specific glaciation periods

Kansan1894

Scanian1895

Wisconsin1895

Illinoian1896

sub-Aftonian1896

Riss1908

Würmian1927

Elster1934

Weichsel1934

Saale1937

Menapian1957

Nebraskan1966

Anglian1968

Devensian1968

Weichselian1968

Wisconsinan1968

Elsterian1969

Wolstonian1969

Würm1972

Donau1983

1937 W. B. Wright Quaternary Ice Age (ed. 2) x. 136 In several places two deposits of loess are separated from one another by glacial formations, indicating that loess formation preceded the advance of the Saale Ice-sheet.

1945 F. E. Zeuner Pleistocene Period iii. 76 The most remarkable feature of the Ukrainian succession is the moraine of the Dnjepr lobe of the Saale glaciation.

1959 Wells & Kirkaldy Outl. Hist. Geol. (ed. 4) xix. 368 The Gipping and Lowestoft Boulder Clays must be correlated with the Saale and Elster glaciations respectively.

1971 R. F. Flint Glacial & Quaternary Geol. xxiv. 628 The distribution of the extensive Saale drift is generally well defined, though in places it is not differentiated clearly from the Elster.

1979 Nature 18 Jan. 172/1 It lies between Saale glacial deposits and the sands of the Last (Weichselian) Glaciation (isotope stages 2, 3, 4 and 5a–5d).

This entry has not yet been fully updated (first published 1982; most recently modified version published online September 2018).

单词	saale
释义	Saalen. /ˈzɑːlə/ Etymology: < the name of the River Saale in Germany. Geology. Used attributively with reference to the third (penultimate) glaciation of the Pleistocene epoch in northern Europe, equivalent to the Riss glaciation in the Alps. ΘΚΠ the world > the earth > structure of the earth > age or period > [adjective] > quaternary > specific glaciation periods Kansan1894 Scanian1895 Wisconsin1895 Illinoian1896 sub-Aftonian1896 Riss1908 Würmian1927 Elster1934 Weichsel1934 Saale1937 Menapian1957 Nebraskan1966 Anglian1968 Devensian1968 Weichselian1968 Wisconsinan1968 Elsterian1969 Wolstonian1969 Würm1972 Donau1983 1937 W. B. Wright Quaternary Ice Age (ed. 2) x. 136 In several places two deposits of loess are separated from one another by glacial formations, indicating that loess formation preceded the advance of the Saale Ice-sheet. 1945 F. E. Zeuner Pleistocene Period iii. 76 The most remarkable feature of the Ukrainian succession is the moraine of the Dnjepr lobe of the Saale glaciation. 1959 Wells & Kirkaldy Outl. Hist. Geol. (ed. 4) xix. 368 The Gipping and Lowestoft Boulder Clays must be correlated with the Saale and Elster glaciations respectively. 1971 R. F. Flint Glacial & Quaternary Geol. xxiv. 628 The distribution of the extensive Saale drift is generally well defined, though in places it is not differentiated clearly from the Elster. 1979 Nature 18 Jan. 172/1 It lies between Saale glacial deposits and the sands of the Last (Weichselian) Glaciation (isotope stages 2, 3, 4 and 5a–5d). This entry has not yet been fully updated (first published 1982; most recently modified version published online September 2018). < n.1937
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