29 research outputs found

    Pennsylvania Folklife Vol. 15, No. 1

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    • The Year of the Rupjonjim • Pennsylvania Summer-Houses and Summer-Kitchens • Religious and Educational References in Lancaster County Wills • Genealogy and Folk-Culture • Pennsylvania German Folktales: An Annotated Bibliography • Italian Immigrant Life in Northampton County, Pennsylvania, 1890-1915 Part IIhttps://digitalcommons.ursinus.edu/pafolklifemag/1021/thumbnail.jp

    Pennsylvania Folklife Vol. 19, No. 3

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    • Cooking in Red and White • Trade Cards, Catalogs, and Invoice Heads • The Encyclopaedia Cinematographica and Folklife Studies • The Cheese was Good • Notes and Documents: Eighteenth-Century Letters from Germany • The Ephrata Wall-Charts and Their Inscriptions • Itinerants - Peddlers, Drovers, Wagoners, Gypsies, Tramps: Folk-Cultural Questionnaire No. 15 • Engravings of Pennsylvania Millshttps://digitalcommons.ursinus.edu/pafolklifemag/1039/thumbnail.jp

    Pennsylvania Folklife Vol. 9, No. 1

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    • Half-Timbering in American Architecture • The Strouse Dance • Schuylkill Boatmen and Their Ways • Some Early Phases of the Philadelphia Mummers\u27 Parade • Fantasticals • Joseph Henry Dubbs as a Folklorist • About the Authors • Horse Companies in Montgomery County • Books Not for Burninghttps://digitalcommons.ursinus.edu/pafolklifemag/1000/thumbnail.jp

    Observation of a new boson at a mass of 125 GeV with the CMS experiment at the LHC

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    Infrared Thermal Mapping of the Martian Surface and Atmosphere: First Results

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    The Viking infrared thermal mapper measures the thermal emission of the martian surface and atmosphere and the total reflected sunlight. With the high resolution and dense coverage being achieved, planetwide thermal structure is apparent at large and small scales. The thermal behavior of the best-observed areas, the landing sites, cannot be explained by simple homogeneous models. The data contain clear indications for the relevance of additional factors such as detailed surface texture and the occurrence of clouds. Areas in the polar night have temperatures distinctly lower than the CO_2 condensation point at the surface pressure. This observation implies that the annual atmospheric condensation is less than previously assumed and that either thick CO_2 clouds exist at the 20-kilometer level or that the polar atmosphere is locally enriched by noncondensable gases
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