Zur Geomorphologie von S-Dickson Land (W-Spitzbergen) mit Schwerpunkt auf die quartären Vergletscherungsgeschichte. (Geomorphology of S. Dickson Land (W. Spitsbergen) with main emphasis on the Quaternary glacial history)
L'A. traite de la glaciation actuelle et préhistorique de la presqu'île Dickson Land, du façonnage des vallées et de l'action périglaciaire. (G. Schweizer).
'S, 25° W, the proposed plate boundary) as the result of an uprising of the basement during the Late Cretaceous. We propose that the Explora Escarpment and the Andenes Escarpment have different genetic origins. - (L'A.).
The new data give more detailed insights into the structure and evolution of the Explora Escarpment. To the west (19° W) the escarpment vanishes as a topographic feature. We interpret a newly discovered structure, denominated Polarstern Bank (71° 30
Berg (L. S.) ; Biobibliographie ; Biographie ; Blodget (L.) ; Capot-Rey (R.) ; Cressey (G. B.) ; Davis (W. M.) ; Fabricius (J. A.) ; Franz (J. M.) ; Glareanus (H.) ; Grigor'ev (A.A.) ; Guyot (A. H.) ; Géographes ; Histoire de la géographie
; Jobberns (G.) ; Lencewicz (S.) ; Mitchell (T. L.) ; Mueller (F. J. H. von) ; Ormsby (H.) ; Ritter (Carl) ; Roxby (P. M.) ; Schmitthenner (H.) ; Siècle XV-XX ; Stoffler (J.) ; Vujevic (P.)
Notices concernant 20 géographes: L. S. Berg (1876-1950), L. Blodget (1823-1901), R. Capot-Rey (1897-1977), G. B. Gressey (1896-1963), W. M. Davis (1850-1934), J. A. Fabricius (1668-1736), J. M. Franz (1700-1761), H. Glareanus (1488-1563
), A. A. Grigoryev (1883-1968), A. H. Guyot (1807-1884), G. Jobberns (1895-1974), S. Lencewicz (1899-1944), T. L. Mitchell (1792-1855), F. J. H. von Mueller (1825-1896), H. Ormsby (1877-1973), C. Ritter (1779-1859), P. M. Roxby (1880-1947), H. Schmitthenner (1887
Vorkommen und Entstehung von tri-oktaedrischen Smektiten in den Basalten und Boden der Konig-Georg-Insel (S-Shetlands/West-Antarktis) (Occurrence et genèse d'une smectite tri-octoédrique dans les basaltes et les sols de King George Island (S
Both the olivine bearing tholeiite basalts of the island and the brown soils which have developed on the basalts contain 2-20 % of a Mg-rich, Fe2+ and Al-bearing tri-octahedral smectite, e. g. Mg-saponite. Due to petrographic and crystal chemical
Geology, palynology and age of a pingo remnant near Daarle, province of Overijssel, The Netherlands in Developments in physical geography. A tribute to J. I. S. Zonneveld..