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Comparison of the Quaternary Stratigraphy of the Alps and Rocky Mountains 1,2

Published online by Cambridge University Press:  20 January 2017

Gerald M. Richmond*
Affiliation:
U.S. Geological Survey, Denver, Colorado

Abstract

Comparison of the glacial and periglacial deposits and soils of the Alps and Rocky Mountains suggests the following correlations. The Donau, Günz, and Mindel are correlated with the Washakie Point (Nebraskan), Cedar Ridge (Kansan), and Sacagawea Ridge (Illinoian). These glaciations are separated and followed by interglacials represented by thick deeply weathered soils, the last being the Mindel/Riss, or Sacagawea Ridge/Bull Lake (Sangamon). The Riss I (Paar) and Riss II (type Riss) Glaciations are correlated with the early and late advances of the Bull Lake Glaciation (early Altonian), and are believed to be different glaciations separated and followed by short interglacials represented by soils of intermediate development at these latitudes. The Alt-Würm period of restricted ice in the Alps is represented only by local unnamed deposits in the Rocky Mountains. In the Alps, at least three interstadial soils occur between the Riss/Würm soil and the oldest Main Würm end moraine. These coincide in time respectively with the beginning and end of the Port Talbot II interstadial and with Plum Point interstadial. The three major end moraines of the Main Würm are correlated with three or locally more end moraines of the early and middle stades of the Pinedale (Woodfordian). Moraines of the late stade of the Pinedale are equivalent to the late glacial and early postglacial moraines of post-Würm but pre-Atlantic age in the Alps.

K-Ar dating and tephrochronology in the Rockies suggest that the Washakie Point ended about 1.2 m.y. B.P., the Cedar Ridge about 700,000 B.P., the Sacagawea Ridge about 180,000 B.P., the last great interglacial about 130,000 B.P., and the interglacial separating early and late Bull Lake about 80,000 B.P. Radiocarbon dates from the Alps suggest that the Riss/Würm was about 70,000–60,000 B.P., and that Alt-Würm interstadials occurred at >50,000, 45,000–40,000, 34,000–32,000, and 28,000 B.P. Radiocarbon dates from rock shelter deposits in France indicate minor interstadials in the Main Würm at 21,000–20,000 B.P. and about 17,000 B.P. Both the Main Würm and Pinedale ended about 11,800 B.P.

Type
Research Article
Copyright
University of Washington

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Footnotes

1

Publication authorized by the Director, U.S. Geological Survey.

2

Presidential address to the VIIIth INQUA Congress, Paris, 1969. This paper has been revised since presentation on the basis of observations and discussions with colleagues in the Alps during the summer of 1969 and a review of the most recent literature.

References

Amferer, O. (1904). Studien über die Inntalterrassen. Jahrbuch Geologische Reichsanstalt 54, 91160.Google Scholar
Amferer, O. (1909). Uber die Enstehung der Inntalterrassen. Zeitschrift für Gletscherkunde 3, 5257, 111142.Google Scholar
Beck, P. (1932). Uber den eiszeitlichen Aaregletscher und die Quartärchronologie. Verhandlungen der Schweizerische Naturforschende Gesellschaft, Thun 1932, 193211.Google Scholar
Beck, P. (1938). Bericht über die ausserordentliche Frühjahrsversammlung der Schweizerischen Geologischen Gesellschaft in Thun. Eclogae Geologicae Helvetiae 31, 185191.Google Scholar
Black, R. F. (1962). Pleistocene chronology of Wisconsin (abs.). Geological Society of America Special Paper No. 68, 137.Google Scholar
Blackwelder, Eliot (1915). Post-Cretaceous history of the mountains of central western Wyoming. Journal of Geology 23, 97117, 193217, 307340.CrossRefGoogle Scholar
Blavoux, B. and Brun, A. (1966). Nouvelles données sur les terrains quaternaires de la region lémanique. Comptes Rendues Hebdomadaires des Seances de L’Académie des Sciences, Paris Series D 262, 25692572.Google Scholar
Bonifay, E. (1962). Récherches sur les terrains quaternaires dans le Sud-Est de la France. Institut Préhistorique Université Bordeaux Mémoire 2. 194 pp.Google Scholar
Bonifay, E. (1965). Stratigraphìe des loess ancièns et récents dans la Sud-Est de la France. Association Française pour l’Étude du Quaternaire Bulletin 1, No. 2, 2134.CrossRefGoogle Scholar
Bonifay, E. (1968). Climates and Quaternary sediments in southeastern France, in the Maritime Alps and along the Mediterranean coast. In “Glaciation of the Alps” (Richmond, G. M. Ed.), pp. 117132. VII INQUA Congress, Proceedings 14; University of Colorado Studies, Series in Earth Sciences 7.Google Scholar
Bonifay, E. (1969). Le Quaternaire littoral et sous-marin des côtes françaises de la Meditérranee. In “Études Françaises sur le Quaternaire,” 4355. VIII INQUA Congress, Association Française pour l’Étude du Quaternaire, Supplément Bulletin, Paris.Google Scholar
Bordes, F. (1953). Les Limons quaternaires du bassin de la Seine. Archéologique Institut Paleontologique Humaine Mémoire 26. 472 pp.Google Scholar
Bordes, F. (1969). Le loess en France. In “Etudes Françaises sur le Quaternaire,” pp. 6976. VIII INQUA Congress, Association Française pour l’Étude du Quaternaire, Supplément Bulletin, Paris.Google Scholar
Bourdier, F. (1961). “Le Bassin du Rhône au Quaternaire,”. Vol. 1. Centre National de la Récherche Scientifique, Paris.Google Scholar
Bourdier, F. (1962). “Le Bassin du Rhône au Quaternaire,”. Vol. 2. Centre National de la Récherche Scientifique, Paris Google Scholar
Brauhauser, M. (1915). “Blatt Friedrichshafen-Oberteuringen 179/174 mit Erläuterungen zur geologischen Spezialkarte von Württemberg.”. Königliches Statistisches Landesamt, Stuttgart.Google Scholar
Broecker, W. S., and Orr, P. C. (1958). Radiocarbon chronology of Lake Lahontan and Lake Bonneville. Geological Society of America Bulletin 69, 10091032.CrossRefGoogle Scholar
Broecker, W. S., and Walton, A.F. (1959). Re-evaluation of the salt chronology of several Great Basin lakes. Geological Society of America Bulletin 70, 601618.CrossRefGoogle Scholar
Brun, A. (1966). Révision de la stratigraphie des dépots quaternaires dan la basse vallée de la Dranse (Haute Savoie). Revue Géographie Physique et Dynamique 8, 399404.Google Scholar
Brunnacker, K. (1957). Die Geschichte der Böden im jüngeren Pleistozän in Bayern. Geologica Bavarica 34, 195.Google Scholar
Brunnacker, K. (1959). Zur Parallelisierung des Jungpleistozäns in den Periglazialgebieten Bayerns und seiner östlichen Nachbarländer. Geologisches Jahrbuch 76, 129150.Google Scholar
Brunnacker, K. (1964a). Böden des älteren Pleistozäns bei Regensburg. Geologica Bavarica 53, 148160.Google Scholar
Brunnacker, K. (1964b). Die Würmeiszeit in Bayern im Licht der Lössforschung. Report, VI INQUA Congress, Warsaw, 1961, 4, 441449.Google Scholar
Büdel, J. (1957). Die angebliche Zweiteilung der Würmeiszeit im Loisach-Vorland bei Murnau (Südbayern). Stuttgarter Geographische Studien 69, 121141.Google Scholar
Büdel, J. (1960). Die Gliederung der Würmkaltzeit. Würzberger Geographische Arbeiten 8, 145.Google Scholar
Christiansen, R. L., Obradovich, J. D., and Blank, R. H. Jr. (1968). Late Cenozoic volcanic stratigraphy of the Yellowstone Park region (abs.). Geological Society of America, Rocky Mountain Section, 21st Annual Meeting, Program with Abstracts, pp. 2930.Google Scholar
Dalrymple, G. B., Cox, A. and Doell, R. R. (1965). Potassium-argon age and paleomagnetism of the Bishop Tuff, California. Geological Society of America Bulletin 76, 665674.CrossRefGoogle Scholar
Dansgaard, W., Johnson, S. J., and Møller, J. (1969). One thousand centuries of climatic record from Camp Century on the Greenland Ice Sheet. Science 166, 377381.CrossRefGoogle ScholarPubMed
de Lumley, H. (1968). Correlation of Quaternary shorelines in meridional France with the Alpine glacial chronology. In “Glaciation of the Alps.” (Richmond, G. M., Ed.), pp. 133142. VII INQUA Congress, Proceedings 14; University of Colorado Studies, Series in Earth Sciences 7.Google Scholar
De Lumley, H. (1969). Civilizations préhistoriques en France. In “Études françaises sur le Quaternaire,” 151169. VIII INQUA Congress, Association française pour l’étude du Quaternaire, Supplément Bulletin, Paris.Google Scholar
Dickinson, R. G. (1966). Geology of the Cerro Summit quadrangle, Montrose County, Colorado. U.S. Geological Survey Open-file Report No. 841.CrossRefGoogle Scholar
Dreimanis, A., Terasmae, J., and McKenzie, G. D. (1966). The Port Talbot Interstade of the Wisconsin Glaciation. Canadian Journal of Earth Sciences 3, 305325.CrossRefGoogle Scholar
Eberl, B. (1930). “Die Eiszeitenfolge im Nördlichen Alpenvorlande.”. Augsburg.Google Scholar
Ebers, E. (1955). Hauptwürm, Spätwürm, Frühwürm und die Frage der älteren Würmschotter., Eiszeitalter und Gegenwart 6, 96109.Google Scholar
Ebers, E. (1960). Drumlinkerne ältere Würmschotter und das Würm-Interstadial-Profil von Hörmating/Oberbayern. Eiszeitalter und Gegenwart 11, 6476.Google Scholar
Ebers, E. (1968). Evidence of an Older Würm glacial maximum and a Middle Würm interstadial in the Alps. In “Glaciation of the Alps” (Richmond, G. M., Ed.), pp. 5577. VII INQUA Congress, Proceedings 14, University of Colorado Studies Series in Earth Sciences 7.Google Scholar
Ebers, E., Weinberger, L., and Del-Negro, W. (1966). Der Pleistozäne Salzachvorlandgletscher. Gesellschaft für Bayerische Landeskunde e. V., München 19–22, 1116.Google Scholar
Fink, J. (1954). Die fossilen Böden im österreichischen Löss. Quatär 6, 85108.Google Scholar
Fink, J. (1959). Studien zur absoluten und relativen Chronologie der fossilen Böden In Österreich I. Oberfellabrunn. Archaeologia Austriaca 25, 3965.Google Scholar
Fink, J. (1961). Die Gliederung des Jungpleistozäns in Österreich. Mitteilungen der Geologischen Gesellschaft in Wien 54, 125.Google Scholar
Fink, J. (1962). Studien zur absoluten und relativen Chronologie der fossilen Böden inÖsterreich II, Wetzleinsdorf und Stillfried. Archaeologia Austriaca 31, 118.Google Scholar
Fink, J. (1969). Le loess en Autriche. In “La Stratigraphie des Loess d’Europe,” pp. 1721. VIII INQUA Congress, Proceedings Association française pour l’étude du Quaternaire, Supplément Bulletin, Paris.Google Scholar
Franzle, O. (1960). Interstadiale Bodenbildungen in oberitalienischen Würm-Lössen. Eiszeitalter und Gegenwart 11, 196205.Google Scholar
Frechen, J., and Lippolt, H.J. (1965). Kalium-Argon-Daten zum Alter des Laacher Vulkanismus der Rheinterrassen und der Eiszeiten. Eiszeitalter und Gegenwart 16, 530.Google Scholar
Frye, J. C., Willman, H. B. and Black, R.F. (1965). Outline of glacial geology of Illinois and Wisconsin. In “The Quaternary of the United States,” (Wright, H. E. Jr., and Frey, D. G. Eds.), pp. 4362. Princeton University Press, Princeton, New Jersey.Google Scholar
Frye, J. C., Willman, H. B., Rubin, M., and Black, R. F. (1968). Definition of Wisconsinan Stage. U.S. Geological Survey Bulletin No. 1274-E 22.Google Scholar
Gotzinger, G. (1936). “Das Lössgebiet um Göttweig und Krems an der Donau. III Internationale Quartär Knoferenz; Fuhrer die Quartär-Exkursionen in Österreich, Teil I, 1–11, Wien.”. Google Scholar
Graul, H. (1962). Eine Revision der pleistozänen Stratigraphie des schwäbischen Alpenvorlandes (Mit einem bodenkundlichen Beitrag von Dr. Karl Brunnacker). Petermanns Geographische Mitteilungen 4, 253271.Google Scholar
Graul, H. (1968). Führer zur zweitägigen Exkursion im nördlichen Rheing letschergebiet August 1968. In “Beiträge zu den Exkursionen anlässlich der DEUQUA-Tagung, August 1968, in Biberach an der Riss.” Heidelberger Geographische Arbeiten 20. 1031.Google Scholar
Graul, H., Schaeffer, I., and Weidenbach, F. (1951). Quartärgeologische Exkursion durch die Riss-Lechplatte. Geologica Bavarica 6, 91177.Google Scholar
Hantke, R. (1959). Zur Altersfrage der Mittelterrassenschotter. Vierteljahrsschrift der Naturforschungs Gesellschaft in Zürich, Jahrgang 104.Google Scholar
Hantke, R. (1960). Zur Gliederung des Jungpleistozäns im Grenzbereich vom Linth-und Rhein-system. Geographica Helvetica 15, 239248.CrossRefGoogle Scholar
Heuberger, H. (1968). Die Alpengletscher im Spät-und Postglazial. Eiszeitalter und Gegenwart 19, 270275.Google Scholar
Holmes, G. W., and Moss, J. H. (1955). Pleistocene geology of the southwestern Wind River Mountains, Wyoming. Geological Society of America Bulletin 66, 629654.CrossRefGoogle Scholar
Horberg, L. (1952). Pleistocene drift sheets in the Lethbridge region, Alberta, Canada. Journal of Geology 60, 303330.CrossRefGoogle Scholar
Izett, G.A., Wilcox, R. E., Powers, H. A., and Desborough, G. A. (1970). The Bishop ash bed, a Pleistocene marker bed in the western United States. Quaternary Research 1, 121132.CrossRefGoogle Scholar
Jäckli, H. (1956). Talgeschichtliche Probleme im aargauischen Reusstal. Geographica Helvetica 11, 4658.CrossRefGoogle Scholar
Kempton, J. P. (1963). Subsurface stratigraphy of the Pleistocene deposits of central northern Illinois. Illinois State Geological Survey Circular No. 356. 43 pp.Google Scholar
Kempton, J. P., and Hackett, J. E. (1968). The late Altonian (Wisconsinan) glacial sequence in northern Illinois. In “Means of Correlation of Quaternary Successions” (Morrison, R. B. and Wright, H. E. Jr., Eds.), 535546. VII INQUA Congress, Proceedings 8; University of Utah Press, Salt Lake City, Utah.Google Scholar
Klebelsberg, R. V. (1949). “Handbuch der Gletscherkunde und Glazialgeologie Band II, Historische-Regionen Teil.”. Springer-Verlag, Wien.Google Scholar
Knauer, J. (1935). Die Ablagerungen der älteren Würm-Eiszeit (Vorrückungsphase) im süddeutschen und norddeutschen Vereisungsgebeit. Geologische Landesuntersuchungen am Bayerischen Oberbergamt Abhandlung 21, 165.Google Scholar
Knauer, J. (1938). Die Mindel-Eiszeilidie zeit grossler diluvialen Vergletscherung in Süddeuschland. Geologische Landesuntersuchungen am Buyerischen Obergant Abhandlung 29, 3545.Google Scholar
Kohl, H. (1955a). Altmoränen und Pleistozäne Schotterfluren zwischen Laudach und Krems., Oberoesterrechische Museums Verein Jahrbach 100, No. 1, 131143.Google Scholar
Kohl, H. (1955b). Die Exkursion zwischen Lambach und Enns. Verhandlungen der Geologische Bundesanstalt Sonderheft D, 4062.Google Scholar
Kohl, H. (1958). Unbekannte Altmoränen in der südwestlichen Traun-Enns-Platte. Mitteilungen der Geographischen Gesellschaft in Wien, Festschrift Hans Spreitzer, 100, No. 1–2. 131143.Google Scholar
Kohl, H. (1962). Eine unbekannte Verwitterungszone zwischen altpleistozänan Schottern bei Kremsmünster. Verhandlungen der Geologischen Bundesanstalt 2, 383386.Google Scholar
Kohl, H., and Weinberger, L. (1968). Pleistocene glaciation and its deposits at the northern margin of the Austrian Alps. In (Richmond, G. M., Ed.), 2740. Glaciation of the Apls VII INQUA Congress, Proceedings 14; University of Colorado Studies, Earth Science Series 7.Google Scholar
Kraus, E. C. (1955). Zur Zweigliederung der südbapehischen Würmeiszeit eine Inner Würm-Verwitterungsperiode. Eiszeitalter und Gegenwart 6, 7595.Google Scholar
Kraus, E. C. (1961). Die beiden interstadialen Würmböden in Südbayern. Eiszeitalter und Gegenwart 12, 4358.Google Scholar
Kraus, E. C. (1962). Herr J. Büdel und die Gliederung der Würmeiszeit. Eiszeitalter und Gegenwart 13, 227230.Google Scholar
Kukla, J. (1969). Die Fundstellen in Mähren. In “Periglazialzone, Löss und Palaeolithikum der Tschechoslowakei.” (Demek, J. and Kukla, J. Eds.), 100105. Institute of Geography, Brno, Czechoslovakia.Google Scholar
Lemée, G., and Bourdier, F. (1950). Une flore pollinique tempéré incluses dans les moraines dites wurminennes d’Armoy près de Thonon (Haute-Savoire). Comptes Rendues Hebdomadaires des Seances de I’Academic des Sciences, Paris 230, 23132315.Google Scholar
Levin, B., Ives, P. C., Oman, C. L., and Rubin, M. (1965). U.S. Survey radiocarbon dates VIII. Radiocarbon 7, 372398.CrossRefGoogle Scholar
Lona, F. (1950). Contributi alla storia della vegetazione e del clima nella val Padana—analisi pollinica del giacimento Villafranchiano di Leffe (Bergamo). Societa Italiana di Scienze Naturali Atti 89, 123178.Google Scholar
Love, J. D. (1961). Reconnaissance study of Quaternary faults in and south of Yellowstone National Park, Wyoming. Geological Society of America Bulletin 42, 17491764.CrossRefGoogle Scholar
Mackin, J. H. (1937). Erosional history of the Bighorn Basin, Wyoming. Geological Society of America Bulletin 48, 813894.CrossRefGoogle Scholar
Marr, J. W. (1967). Data on mountain environments I, Front Range, Colorado, sixteen sites, 1952–1953. University of Colorado Studies, Series in Biology 27, 110.Google Scholar
Mayr, F. (1968). Uber den Beginn der Würmeiszeit im Inntal bei Innsbruck. Zeitschrift für Geomorphologie 12, 256295.Google Scholar
Mayr, F., and Heuberger, H. (1968). Type areas of late glacial and postglacial deposits Tyrol, eastern Alps. In “Glaciation of the Alps” (Richmond, G. M. Ed.), 143165. VII INQUA Congress, Proceedings 14, University of Colorado Studies, Series in Earth Sciences 7.Google Scholar
Morrison, R. B. (1965). Quaternary stratigraphy of eastern Jordan Valley south of Salt Lake City, Utah. U.S. Geological Survey Professional Paper No. 477. 80 pp.Google Scholar
Movius, H. L. Jr. (1966). Hearths of the upper Perigordan and Aurignacian horizons at Abri Pataud, Les Eyzies (Dordogne) and their possible significance. In “Recent Studies in Paleoanthropology” (Clark, J. D. and Howell, F. C. Eds.), 296325. American Anthropologist 68, No. 2, Pt. 2.Google Scholar
Nangeroni, G. (1950a). Nuove osservazioni sul morenico Günz nella Lombardia estrema occidentale. Societa Italiana di Scienze Naturali Atti 89, 202212.Google Scholar
Nangeroni, G. (1950b). Il significato geologico delle Sabbie-ghiaie Terrazzato nella media valle dell’Olona. Societa Geologica Italiana Bollettino 69, 16.Google Scholar
Nangeroni, G. (1953). La formazione Günz nel territorio Varesino-Verbano. Geologica Bavarica 19 133140.Google Scholar
Nangeroni, G. (1958). Osservazioni su alcuni pozzi trivellati ad oriente di Varese. Societa Italiana di Scienze Naturali Atti 97, 5157.Google Scholar
Nathan, H. (1953). Ein interglazialer Schotter südlich Moosburg in Oberbayern. Geologica Bavarica 19, 315334.Google Scholar
Paschinger, V. (1959). Nachlese in den glazialen Ablagerungen der Hollenburger Senke (Sattnitz). In “Naturwissenschaftliche Beiträge zur Heimatkunde Kärntens,” Carinthia II, Jahrg 69, 2934, Klagenfurt.Google Scholar
Penck, A., and Bruckner, E. (1901–1909). “Die Alpen im Eiszeitalter,”. 3 Vols. Chr. Herm. Tauchnitz, Leipzig.Google Scholar
Richmond, G. M. (1948). Modification of Blackwelder's sequence of Pleistocene glaciation in the Wind River Mountains, Wyoming (abs.). Geological Society of America Bulletin 59, 14001401.Google Scholar
Richmond, G. M. (1957). Three pre-Wisconsin glacial stages in the Rocky Moutain region. Geological Society of America Bulletin 68, 239262.CrossRefGoogle Scholar
Richmond, G. M. (1962). Quaternary stratigraphy of the La Sal Mountains, Utah. U.S. Geological Survey Professional Paper No. 324. 135 pp.Google Scholar
Richmond, G. M. (1964a). Three pre-Bull Lake tills in the Wind River Mountains, Wyoming— a reinterpretation. In “Geological Survey Research 1964,” pp. D104D109. U.S. Geological Survey, Professional Paper, No. 501-D.Google Scholar
Richmond, G. M. (1964b). Glacial geology of the West Yellowstone Basin and adjacent parts of Yellowstone National Park. In “The Hebgen Lake, Montana, Earthquake of August 17, 1959,” pp. 223236. U.S. Geological Survey, Professional Paper No. 435.Google Scholar
Richmond, G.M. (1964c). Glaciation of Little Cottonwood and Bells Canyons, Wasatch Mountains, Utah. U.S. Geological Survey, Professional Paper No. 454-D, D1D41.Google Scholar
Richmond, G. M. (1965).Google Scholar
Glaciation of the Rocky Mountains. In “The Quaternary of the United States.” (Wright, H. E. Jr. and Frey, D. G. Eds.), pp. 217230. Princeton University Press, Princeton, New Jersey Google Scholar
Richmond, G. M. (1968). Late Pinedale and Neoglacial glaciation in the Absaroka Range, east of Yellowstone Lake, Wyoming (abs.). Geological Society of America, Rocky Mountain Section, 1968 Annual Meeting, Program with Abstracts, p. 65.Google Scholar
Richmond, G. M., Fryxell, R., Neff, G. E., and Weiss, P. L. (1965). The Cordilleran ice sheet of the northern Rocky Mountains and related Quaternary history of the Columbia Plateau. In “The Quaternary of the United States.” (Wright, H. E. Frey, D. G. Eds.), pp. 231242. Princeton University Press, Princeton, New Jersey.Google Scholar
Richmond, G. M., and Murphy, J. F. (1965). Geologic map of the Bull Lake East quadrangle, Fremont County, Wyoming. U.S. Geological Survey Geologic Quadrangle Map GQ-431.Google Scholar
Rohrer, W. L., and Leopold, E. B. (1964). Fenton Pass Formation (Pleistocene?), Bighorn Basin, Wyoming. In “Short Papers in Geology and Hydrology,” pp. C45C48. U.S. Geological Survey, Professional Paper No. 475-C.Google Scholar
Rubin, M., and Alexander, C. (1958). U.S. Geological Survey radiocarbon dates IV. Science 127, 14761487.CrossRefGoogle ScholarPubMed
Schädel, K. (1952). Die Stratigraphie des Altdiluviums im Rheingletschergebiet. Oberrheinischer Geologischer Verein Jahrbuch und Mitteilung N. F. 34, 120.Google Scholar
Schädel, K., Weidenbach, F., and Werner, J. (1961). Exkursion in das Pleistozan von Oberschwaben. In “Führer zu der Exkursion Oberrheinischer Geologischer Verein in Ulm.” Geologisch Paläontologisches Institut, Stuttgart.Google Scholar
Schädel, K., and Werner, J. (1963). Neue Gesichtspunkte zur Stratigraphie des mittleren und alteren Pleistozäns im Rheingletscherbegiet. Eiszeitalter und Gegenwart 14, 526.Google Scholar
Schaefer, I. (1953). Die donaueiszeitlichen Ablagerungen an Lech und Wertach. Geologica Bavarica 19, 1364.Google Scholar
Schaefer, I. (1956). Sur la division du Quaternaire dans l’avant-pays des Alpes en Allemagne. Actes, IV Congrès INQUA, Rome-Pisa, 1953, 2, 910914.Google Scholar
Schaefer, I. (1968). The sucession of fluvioglacial deposits in the northern Alpine foreland. In “Glaciation of the Alps” (Richmond, G. M. Ed.), pp. 914. VII INQUA Congress, Proceedings 14; University of Colorado Studies, Series in Earth Sciences 7.Google Scholar
Schmidt, M. (1913). Blatt Tettnang, 1:100,000 mit Erläuterungen der geologischen Spezialkarte von Württemberg. Königliches Statistisches Landesamt, Stuttgart.Google Scholar
Schröder, J., and Dehm, R. (1951). Die Mollusken Fauna aus der Lehm-Zwischenlage des Deckenschotters von Fischbach, Kreis Augsburg. Geologica Bavarica 6, 118120.Google Scholar
Scott, G. R. (1963). Nussbaum alluvium of Pleistocene(?) age at Pueblo, Colorado. In “Short Papers in Geology and Hydrology,” pp. 4952. U.S. Geological Survey, Professiona Paper No. 475-C. Google Scholar
Smith, G. I. (1968). Late Quaternary geologic and climatic history of Searles Lake, southeastern California. In “Means of Correlation of Quaternary Successions” (Morrison, R. B. and Wright, H. E. Jr. Eds.). pp. 293310. VII INQUA Congress, Proceedings 8, University of Utah Press, Salt Lake City, Utah.Google Scholar
Smith, P. E. L. (1966). “Le Solutréen en France.”. Institut Préhistorique Université Bordeau Publication, Mémoire 5. 449 pp.Google Scholar
Soister, P. E. (1967). Relation of Nussbaum Alluvium (Pleistocene) to the Ogallala Formation (Pliocene) and to the Platte-Arkansas divide, southern Denver basin, Colorado. In “Geological Survey Research 1967,” pp. D39D46. U.S. Geological Survey, Professional Paper, No. 575-D.Google Scholar
Stalker, A. MacS. (1963). Quaternary stratigraphy in southern Alberta. Geological Survey of Canada Paper No. 62-34. 52 pp.Google Scholar
Stearns, C. E., and Thurber, D. L. (1967). Th230/U234 dates of late Pleistocene marine fossils from the Mediterranean and Moroccan littorals. In “The Quaternary History of the Ocean Basins.” (Sears, Mary Ed.), pp. 293305. VII INQUA Congress, Proceedings 13; Progress in Oceanography 4. Pergamon Press, Oxford and New York.Google Scholar
Stromer, E., and Lebling, C. (1929). Fossilführendes Pliozän in Südbayern. Zentralblatt für Mineralogie Jahrgang 1929, Abteilung B, 307314.Google Scholar
Venzo, S. (1953). Stadi della glaciazione del “Donau” sotto al Günz nella serie lacustre di Leffe (Bergamo-Lombardia). Geologica Bavarica 19, 7493.Google Scholar
Venzo, S. (1957). Rilevamento geologico dell’ anfiteatro morenico del Garda, Parte I, Tratto occidentale. Societa Italiana di Scienze Naturali Memoirs 12 Pt. 2, 73140.Google Scholar
Venzo, S. (1961). Rilevamento geologico dell’ anfiteatro morenico del Garda, Parte II, Tratto orientale. Societa Italiana di Scienze Naturali Memoirs 13. Pt. 1, 164.Google Scholar
Venzo, S. (1965). Rilevamento geologico dell’ anfiteatro morenico frontale de Garda dal Chiese all’Adige. Societa Italiana di Scienze Naturali Memoirs 14, Pt. 1, 182.Google Scholar
Visher, S. S. (1966). “Climatic Atlas of the United States.”. Harvard University Press, Cambridge, Mass. Google Scholar
Vogel, J. C., and Waterbolk, H. T. (1963). Groningen radiocarbon dates IV. Radiocarbon 5, 163202.CrossRefGoogle Scholar
Vogel, J. C., and Waterbolk, H. T. (1967). Groningen radiocarbon dates VII. Radiocarbon 9, 107155.CrossRefGoogle Scholar
Vogel, J. C., and Zagwijn, W. H. (1967). Groningen radiocarbon dates VI. Radiocarbon 9, 63106.CrossRefGoogle Scholar
Weidenbach, F. (1936). Erläuterungen zur geologischen Spezialkarte von Württemberg, 1 :25,000. Blatt Waldsee, Stuttgart.Google Scholar
Weidenbach, F. (1937). Erläuterungen zur geologischen Spezialkarte von Württemberg, 1 :25,000. Blatt Biberach, Stuttgart.Google Scholar
Weidenbach, F. (1940). Erläuterungen zur geologischen Spezialkarte von Württemberg, 1 :25,000. Blatt ochsenhausen, Stuttgart.Google Scholar
Weinberger, L. (1950). Gliederung der Altmoränen des Salzachgletschersöstlich der Salzach. Zeitschrift für Gletscherkunde und Glazialgeologie (Innsbruck) 1, 176186.Google Scholar
Weinberger, L. (1955). Exkursion durch dasösterreichische Salzachgletschergebiet und die Moränengurtel der Irrsee und Atterseezweige des Traungletschers. In “Beiträge zur Pleistozänforschung in Österreich, Exkursionen Zwischen Salzach und March,” pp. 734. Verhandlungen der Geologischen Bundesanstalt Sanderheft D.Google Scholar
Welton, M. and Oescher, H. (1957). Erste Ergebnisse von C-14-Altersbestimmungen zur Vegetationsgeschichte der Schweiz. Verhandlungen der Schweizerischen Naturforschenden Gesellschaft, Neuenburg, 8890.Google Scholar
Wilcox, R. E. (1965). Volcanic-ash chronology. In “The Quaternary of the United States,” (Wright, H. E. and Frey, D. G. Eds.), pp. 807816. Princeton University Press, Princeton, New Jersey.Google Scholar