George Waelbrouk, Brustbild

Signatur des Originals: S 36/F02097

Robert Burg als Escamillo, Rollenbild, in: George Bizet: Carmen

Signatur des Originals: S 36/F03272

Heinrich George, Brustbild

Signatur des Originals: S 36/F04121

George Sand, Brustbild

Signatur des Originals: S 36/F06113

George Alexander als Cross, Rollenbild, Kniestück, in: Samuel Johnson: The Idler, London: St. James's Theatre

Signatur des Originals: S 36/F08064

George Alexander als Dr. Bill, Rollenbild, Kniestück, London: St. James's Theatre

Signatur des Originals: S 36/F08065

George Meader, Szenenfoto

Signatur des Originals: S 36/F09241

George Clemont Martin, Brustbild

Signatur des Originals: S 36/F09200

Else Knott als Dortchen Lakenreißer, Szenenfoto, Brustbild, in: William Shakespeare (Robert George): König Heinrich IV., Frankfurt a. M.: Römerbergfestspiele, 1937

Signatur des Originals: S 36/F12094

Lotte Brackebusch als Frau Hurtig, Rollenbild, Brustbild, in: William Shakespeare (Robert George): König Heinrich IV, Frankfurt a. M.: Römerbergfestspiele, 1937

Signatur des Originals: S 36/F12041

Eva Bubat als Lady Percy, Rollenbild, Kniestück, in: William Shakespeare (Robert George): König Heinrich IV., Frankfurt a. M.: Römerbergfestspiele, 1937

Signatur des Originals: S 36/F12046

Hermann Schomberg als Sir John Falstaff, Rollenbild, Brustbild, in: William Shakespeare (Gobert George): König Heinrich IV., Frankfurt a. M.: Römerbergfestspiele, 1937

Signatur des Originals: S 36/F12150

Hermann Schomberg als Sir John Falstaff, Rollenbild, in: William Shakespeare (Robert George): König Heinrich IV., Frankfurt a. M.: Römerbergfestspiele, 1937

Signatur des Originals: S 36/F12152

(Table 1, page 434-435) Bulk chemical composition of S.W. Pacific island arc Mn-oxide crusts

Hydrothermal Mn-oxide crusts have been removed from the Tonga-Kermadec Ridge, the first such hydrothermal deposits to be reported in the S.W. Pacific island arc. In several respects the deposits are similar to hydrothermal Mn-crusts from oceanic spreading centre settings. They are limited in areal extent, comprise well-crystalline birnessite and generally display extreme fractionation of Mn from Fe. They are strongly depleted in many elements compared to hydrogenous Mn deposits but are comparatively enriched in Li, Zn, Mo and Cd. The Group IA and Group IIA metals show strong intercorrelations and the behaviour of Mg in the purest samples may indicate the extent to which normal seawater has influenced the composition of the deposits. Certain aspects of the deposits are not typical of hydrothermal Mn deposits. In particular at least some of the crusts have developed on a sediment or unconsolidated talus substrate. Some crusts, or specific layers within some crusts, display a chemical composition which suggests a significant input from normal seawater.

Mass balance measurements on King George Island ice cap in 2007 and 2008

The Antarctic Peninsula has been identified as a region of rapid on-going climate change with impacts on the cryosphere. The knowledge of glacial changes and freshwater budgets resulting from intensified glacier melt is an important boundary condition for many biological and integrated earth system science approaches. We provide a case study on glacier and mass balance changes for the ice cap of King George Island. The area loss between 2000 and 2008 amounted to about 20 km**2 (about 1.6% of the island area) and compares to glacier retreat rates observed in previous years. Measured net accumulation rates for two years (2007 and 2008) show a strong interannual variability with maximum net accumulation rates of 4950 mm w.e./a and 3184 mm w.e./a, respectively. These net accumulation rates are at least 4 times higher than reported mean values (1926-95) from an ice core. An elevation dependent precipitation rate of 343 mm w.e./a (2007) and 432 mm w.e./a (2008) per 100 m elevation increase was observed. Despite these rather high net accumulation rates on the main ice cap, consistent surface lowering was observed at elevations below 270 m above ellipsoid over an 11-year period. These DGPS records reveal a linear dependence of surface lowering with altitude with a maximum annual surface lowering rate of 1.44 m/a at 40 m and -0.20 m/a at 270 m above ellipsoid. These results fit well to observations by other authors and surface lowering rates derived from the ICESat laser altimeter. Assuming that climate conditions of the past 11 years continue, the small ice cap of Bellingshausen Dome will disappear in about 285 years.