59 resultados para Lüneburg


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Berichtiger Abdruck aus Spangenbergs Neuem vaterländischem Archive, nebst einigen Zusätzen.

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Mode of access: Internet.

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CBEL III, 414 lists two 1824 editions within distinguishing marks.

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In Wedekind, A.C., Noten, etc. 1836. 8vo, pp. 1-98.

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Mode of access: Internet.

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1. Sammlung: 2. verb., und durch eine Zugabe verm., Aufl., 1810.

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This article introduces the genre of a digital audio game and discusses selected play interaction solutions implemented in the Audio Game Hub, a prototype designed and evaluated in the years 2014 and 2015 at the Gamification Lab at Leuphana University Lüneburg.1 The Audio Game Hub constitutes a set of familiar playful activities (aiming at a target, reflex-based reacting to sound signals, labyrinth exploration) and casual games (e.g. Tetris, Memory) adapted to the digital medium and converted into the audio sphere, where the player is guided predominantly or solely by sound. The authors will discuss the design questions raised at early stages of the project, and confront them with the results of user experience testing performed on two groups of sighted and one group of visually impaired gamers.

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Presented at DiGRA 2015 Diversity of Play, Leuphana University, Lüneburg, Germany, on the 15th of May 2015.

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An outline of the Pleistocene history of the southern Lüneburg Heide is given based on the interpretation of exposed sections and indicator-stone analysis. Locally, Elsterian sediments crop out at the surface, mainly near the Holsteinian kieselgur (diatomite), thus indicating the existence of a pre-Saalian relief. Most of the Pleistocene deposits were formed during the three Saali- an ice advances. The ground moraine (basal till) of the first advance (the main Drenthe moraine) and its outwash sands are only locally exposed and only at the margin of the Aller valley do they form a relatively extensive plain. To the north, they are overlain by outwash sands of the late Drenthe advance. Also the Uelzen end moraine consists mainly of these outwash sands. The Uelzen moraine was overridden by the same ice advance. The Warthe ice sheet left only minor traces ridge; its advance came to a final stop at the already dumped morainic material.

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Anläßlich der Tagung der Deutschen Quartärvereinigung in Lüneburg 1964 wurden während der Exkursionen in der Grube der Ziegelei Elba (Adendorf bei Lüneburg) auch die Deckschichten des Holstein-Interglazials (siehe die Arbeit von BENDA und MICHAEL im gleichen Heft) vom Verfasser interpretiert. Die obersten bestehen aus einer Flugsandserie und 37 Sandschichten, die durch Lagen humosen Sandes getrennt sind. Ihre Basis bildet ein 2-5 cm mächtiger Radizellentorf in und über einer Steinsohle mit teilweise windgeschliffenen und windpolierten nordischen Geschieben.