Der Prozess [August] Rohling c/a [Josef Samuel] Bloch

Aus: Mittheilungen aus d. Verein zur Abwehr des Antisemitismus

Cantate : Psalm 45 ; [Cantate aus Anlass der Feier der silbernen Hochzeit unseres ... Kaiserpaares ... Franz Joseph I. und ... Elisabeth Amalie Eugenia ; 24te April 1854 - 1879]

[in Musik gesetzt von] J[acob] Bachmann

[Josef Salomo del Medigo]

Abraham Geiger. Hrsg. von Ludwig Geiger

Die Philosophie des Josef (Ibn) Zaddik : nach ihren Quellen, insbesondere nach ihren Beziehungen zu den Lauteren Brüdern und zu Gabirol

unters. von Max Doctor

Aus meinem Jugendleben : meine Lehrer Israel I., Josef II., Moses III., Friedrich IV.

von D. Leimdörfer

Catalogue de la bibliothèque de littérature hébra͏̈ique et orientale de feu Josef Almanzi

Samuel David Luzzatto

Tefiloth Josef : selected recitatives ; for the Synagogue

by Yosef Rosenblatt

Di wahre und tzuferlaessige lebensbešraibung des welṭberihmṭen iṭalienišen feldherrn Josef Garibaldi und di emantzipatzion der juden

[Kalaman Majlath]

Ich, Du und ER. Franz Rosenzweigs Einfluss auf die Abfassung von Ich und Du

Bekannt ist die Tatsache, dass Martin Buber und Franz Rosenzweig gemeinsam die Hebräische Bibel übersetzt haben, jedenfalls bis zu Jesaja 53, als Rosenzweig verstarb. Weniger bekannt ist die Tatsache, dass Rosenzweig auch auf die Abfassung von Bubers Hauptwerk Ich und Du Einfluss ausgeübt hat.

Glacier advances in northeastern Turkey before and during the global Last Glacial Maximum

Abstract Our study in the Başyayla Valley in northeastern Anatolia showed evidence of four glacier advances that built terminal and lateral moraines. Surface exposure dating of boulders on these moraines showed that the Maximum Ice Extent (MIE) was asynchronous with the global Last Glacial Maximum (LGM; 22.1 ± 4.3 thousand years; ka). The local {MIE} took place at least 57.0 ± 3.5 ka ago. The extent of the Başyayla Glacier during this advance is not known exactly because the boulders are only preserved on a lateral moraine. The next advance was prior to 41.5 ± 2.5 ka, and it descended down the valley to approximately 2320 m above sea level (m a.s.l.), with a glacier length of 5.3 km. During the early global LGM, the Başyayla Glacier extended for a distance of 4.9 km down to approx. 2430 m a.s.l. The last recorded advance occurred during the global LGM. This extension was 0.7 km smaller than the local {MIE} and its terminus reached 2490 m a.s.l. only. The exposure ages of boulders in a retreat position at an altitude of approx. 3045 m a.s.l. indicate that the valley has remained ice-free since the Lateglacial period. Therefore, the Lateglacial extent was limited to the cirque system in the uppermost part of the catchment. Furthermore, Holocene glacier oscillations seem to be either absent or restricted to solifluction in the whole catchment and to rock glacier movements in the southern tributary of the Başyayla Valley system.

Timing of retreat of the Reuss Glacier (Switzerland) at the end of the Last Glacial Maximum

We used cosmogenic 10Be and 36Cl to establish the timing of the onset of deglaciation after the Last Glacial Maximum of the Reuss Glacier, one of the piedmont lobes of the Alpine ice cap that reached the northern Alpine foreland in Switzerland. In this study, we sampled erratic boulders both at the frontal position in the foreland (Lenzburg and Wohlen, canton Aargau) and at the lateral Alpine border position (Seeboden moraine, Rigi, canton Schwyz). The minimum age for the beginning of retreat is 22.2 ± 1.0 ka at the frontal (terminal) position and 20.4 ± 1.0 ka at the lateral position. These ages are directly comparable with exposure ages from the other piedmont lobes in the northern Alpine foreland. Our data from the mountain called Rigi, do not support the hypothesis that boulders located external to the Seeboden moraine were deposited prior to the last glacial cycle. We present a first exposure age from an erratic boulder in a retreat position in the Alpine foreland. The Reuss Glacier was approximately 12 km behind the maximal extent no later than at 18.6 ± 0.9 ka.

Der šlezišer ger-tzedek Josef B. ... Abraham (Josef Šṭeblitzki)

J. Aduren

Schnidejoch (2756 m a.s.l., Western Bernese Alps, Switzerland). Did Holocene glacier advances close the alpine pass for human transhumance?

A series of more than 70 radiocarbon dates confirms that the Schnidejoch pass, linking the Bernese Highlands with the River Rhone valley, was in use at least from 4800–4500 BC on. The pass was of easy access when the glaciers from the nearby Wildhorn mountain range (peak on 3248 a.s.l) were in a retreating phase e.g. as is the situation today. During holocene phases of advancing glaciers the pass was blocked for humans accompanied by herding animals. The presentation reviews the publication of Grosjean et al. (Ice-borne prehistoric finds in the Swiss Alps reflect Holocene glacier fluctuations, JOURNAL OF QUATERNARY SCIENCE, 200, 22.3, 203–207) on a larger basis of radiocarbon dating and discusses the position of the pass within a system of prehistoric settlements, camp sites and passes.