903 resultados para Museum exhibits -- Colorado -- Denver


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In the Burgdorf Museum of Ethnology, a mummy rests in a coffin. According to the inventory book, it was purchased from the Cairo Egyptian museum in 1926. The coffin was now examined by Egyptologists and the mummy was radiocarbon dated and examined by Anthropologists. The aim of the study was to compare the results and to check whether mummy and coffin actually belong together. The skull was examined morphological-anthropologically and by CT as a “blank sample”. Coffin and skull imply that the individual was female. The coffin dates to the Ptolemaic period. Only skull bones are preserved, the ethmoid is damaged. CT images Show resinous substances, bone fragments and brain remnants inside the skull. The ethmoid bone was probably foraminated during the mummification process and thus ended up inside the skull. The individual was mummified between the New Kingdom and the Ptolemaic period. Due to its style, it is most probable that the coffin comes from the Gamhud necropolis. The Burgdorf museum of ethnology inventory book chronicles were largely falsified by the examinations. There is a time gap between coffin and the mummy, there are two possible interpretations: the body was mummified with older linen, or the mummy and the coffin do not belong together. The authors strongly advise further investigations.

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1865, vier Jahre vor seinem Tod, schenkt der Bieler Sammler Friedrich Schwab seine archäologischen Objekte der Stadt. Er möchte damit den Bewohnern Biels, vor allem der Jugend, einen reichen Fundus zur Verfügung stellen, der einen Einblick in den Alltag der prähistorischen Bewohner der Region bietet. Bis heute ist die Sammlung Schwab ein Studienobjekt für Archäologen geblieben und inspiriert Öffentlichkeit und Schulklassen: So sieht Friedrich Schwab seinen Willen auch nach bald 150 Jahren noch immer erfüllt. Die vorliegende Publikation erläutert die wechselvolle Geschichte des Museums Schwab und bietet gleichzeitig einen Überblick über die archäologische Erforschung der Drei-Seen-Region: von der Entdeckung der ersten Pfahlbausiedlungen bis zu ihrer Aufnahme in das UNESCO Welterbe. Sie folgt den Sammlungen eines Universalmuseums auf ihrer Odyssee, weist auf Details einer einmaligen Architektur hin und zeigt die Zusammenhänge zwischen Kulturpolitik und der aktuellen Bieler Museumslandschaft auf.

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The soils on four lithologies (basaltic conglomerates, Bohio; Andesite; volcanoclastic sediments with basaltic agglomerates, Caimito volcanic; foraminiferal limestone, Caimito marine) on Barro Colorado Island (BCI) have high exchangeable Ca concentrations and cation-exchange capacities (CEC) compared to other tropical soils on similar parent material. In the 0–10 cm layer of 24 mineral soils, pH values ranged from 5.7 (Caimito volcanic and Andesite) to 6.5 (Caimito marine), concentrations of exchangeable Ca from 134 mmolc kg− 1 (Caimito volcanic) to 585 mmolc kg− 1 (Caimito marine), and cation exchange capacities from 317 mmolc kg− 1 (Caimito volcanic) to 933 mmolc kg− 1 (Caimito marine). X-ray diffractometry of the fraction < 2 μm revealed that smectites dominated the clay mineral assemblage in soil except on Caimito volcanic, where kaolinite was the dominant clay mineral. Exchangeable Ca concentrations decreased with increasing soil depth except on Caimito marine. The weathering indices Chemical Index of Alteration (CIA), Plagioclase Index of Alteration (PIA) and Weathering Index of Parker (WIP) determined for five soils on all geological formations, suggested that in contrast to expectation the topsoil (0–10 cm) appeared to be the least and the subsoil (50–70 cm) and saprolite (isomorphically weathered rock in the soil matrix) the most weathered. Additionally, the weathering indices indicated depletion of base cations and enrichment of Al-(hydr)oxides throughout the soil profile. Tree species did not have an effect on soil properties. Impeded leaching and the related occurrence of overland flow seem to be important in determining clay mineralogy. Our results suggest that (i) edaphic conditions favor the formation of smectites on most lithologies resulting in high CEC and thus high retention capacity for Ca and (ii) that there is an external source such as dust or sea spray deposition supplying Ca to the soils.

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Smithsonian Institution ... By Cyrus Adler and I. M. Casanowicz

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S. H. Lieben

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