Kunstmapen von Osijek. Drucken 1920—1941

Wir haben hier diese chronologische Ordnundg: Wir haben hier diese chronologische Ordnundg: 1920. Šanoa, Branimir: Kr. slob. grad Osijek MCMXIX 1922. Wagner, Božo: Stari Osijek: 8 originalnih litografija 1924. Roch, Ivan: Iz starog Osijeka: 16 orig. litografija 1926. Gojković, Jovan: Iz osječke Tvrđe: 12 orig. Litografija 1932. Roch, Ivan: Grad Osijek: 20 originalnih litografija (ponavlja se 1939) 1937. Gojković, J.: Stari Osijek: u nekoliko perocrteža (I izdanje kolorirano, II crno-bijelo) (12 kom) 1939. Gojković, Jovan: Stari Osijek: 28 perocrteža (I i II izdanje) Gojković, J.: Stari Osijek 16 perocrteža Roch, I.: Grad Osijek: 20 orig. litografija (ponovljeno iz 1932. godine) 1940. Gojković, J.: Stari Osijek: u nekoliko perocrteža (nalijepljene razgledni¬ce) (15 kom) Gojković, J.: Stari Osijek (12 kom

Limits of Weierstrass points in regular smoothings of curves with two components

In the 80's D. Eisenbud and J. Harris posed the following question: "What are the limits of Weierstrass points in families of curves degenerating to stable curves not of compact type?" We answer their question for one-dimensional families of smooth curves degenerating to stable curves with just two components meeting at points in general position. In this note we treat only those families whose total space is regular. Nevertheless, we announce here our most general answer, to be presented in detail in a forthcoming submission.Comment: 7 pages, AMS-Te

Comment on `Renormalization-Group Calculation of the Dependence on Gravity of the Surface Tension and Bending Rigidity of a Fluid Interface'

It is shown that the interface model introduced in Phys. Rev. Lett. 86, 2369 (2001) violates fundamental symmetry requirements for vanishing gravitational acceleration $g$, so that its results cannot be applied to critical properties of interfaces for $g\to 0$.Comment: A Comment on a recent Letter by J.G. Segovia-L\'opez and V. Romero-Roch\'{\i}n, Phys. Rev. Lett.86, 2369 (2001). Latex file, 1 page (revtex

Montegrosso – E Pilone

Trois niveaux distincts d’occupation (IIA, IIIA, IVA) de la terrasse 2 (T2) permettent, par la nature des vestiges découverts, les datations 14C (F2 couche IV A : 1403 ± 130 apr. J.-C.) et les organisations évidentes, d’inférer une occupation en continu du xvie au xvie s. apr. J.-C. Les activités domestiques de plein air (F2 couche IV A) ou liées à un habitat probable mais non caractérisé (F1 couche III et F3 couche II A) sont attestées en particulier par les traces de cuisson des os et les c..