798 resultados para Table setting and decoration.
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[Division I. A to Cak] -- Division II. Cak to Cro -- Division III. Cro to Gri -- Division IV. Gri to Mus -- Division V. Mus to Pin -- Division VI. Pin to Ser -- Division VII. Sha to Tut -- Division VIII. Twe to Zwe.
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Mode of access: Internet.
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Includes household hints; samples of menus; some recipes include wine or liquor as an ingredient. Sample recipes: Stuffed artichokes, Macaroni à la Milanaise, Apricot and wine jelly, Cream sponge cake.
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Includes samples of menus, nutrition information, etc.
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Includes dinner recipes and sample-menus for Sunday and holidays.
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Mode of access: Internet.
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Includes recipes for wine, mead, and other liquors; illustrations of kitchen stoves using coal; illustrations of layout of dishes for multi-course meal. Sample recipes: To bake herrings, To make cream pancakes, To make a blanc-mange of isinglass, To make cowslip wine.
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Includes index.
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Catalog and promotional literature for R. Wallace & Sons Manufacturing Co., manufacturers of silver tableware.
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Advertisements at end.
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Includes section on napkin folding; cooking glossary of Czech and English language, including English pronuncation with Czech phonetics. Sample recipes: Obyčejná bramborová polévka, Potato soup, Soupe de pommes de terre; Skopová sekanina s vejci, Mutton hash with eggs, Hachis de mouton aux oeufs; Mramorový dort, Marble cake, Gâteau marbre.
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Includes samples of menus. Sample recipes: Halibut steak au gratin, Roast fillet of veal with oysters, Bordelaise sauce, Cream pudding.
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Lettered on cover: Prepared by the editors of Vogue.
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The transport of anthropogenic and natural contaminants to public-supply wells was evaluated in a part of the High Plains aquifer near York, Nebraska, as part of the U.S. Geological Survey National Water-Quality Assessment Program. The aquifer in the Eastern High Plains regional study area is composed of Quaternary alluvial deposits typical of the High Plains aquifer in eastern Nebraska and Kansas, is an important water source for agricultural irrigation and public water supply, and is susceptible and vulnerable to contamination. A six-layer, steady-state ground-water flow model of the High Plains aquifer near York, Nebraska, was constructed and calibrated to average conditions for the time period from 1997 to 2001. The calibrated model and advective particle-tracking simulations were used to compute areas contributing recharge and travel times from recharge areas to selected public-supply wells. Model results indicate recharge from agricultural irrigation return flow and precipitation (about 89 percent of inflow) provides most of the ground-water inflow, whereas the majority of ground-water discharge is to pumping wells (about 78 percent of outflow). Particle-tracking results indicate areas contributing recharge to public-supply wells extend northwest because of the natural ground-water gradient from the northwest to the southeast across the study area. Particle-tracking simulations indicate most ground-water travel times from areas contributing recharge range from 20 to more than 100 years but that some ground water, especially that in the lower confined unit, originates at the upgradient model boundary instead of at the water table in the study area and has travel times of thousands of years.