Hudson Valley

Heat. Controls the rate of heating, not the temperature. The higher the setting, the faster the temperature rise. At Hudson Valley Community College, we ve had a stop put in and you can only turn the dial as far as the number 7. When it gets up to 10, you always smoke the oil. Don t do that. 

J. W. Zubrick Hudson Valley Community College April 3, 1987... 

STATISTICAL AND FLUID DYNAMIC SIMULATIONS, AND ALSO COMPUTERS HARDWARE DEVELOPMENT IN THE HUDSON VALLEY... 

The two heads of state saved their Tube Alloy discussions for the end of the conference, late September, when they retreated to Roosevelt s estate in the Hudson Valley at Hyde Park. This was another piece of black comedy, writes C. P. Snow. . .. Roosevelt surrendered without struggle to Churchill s view of Bohr. The result was a secret aide-m6moire, obviously of Churchill s composition, that misrepresented Bohr s proposals, repudiated them and recorded for the first time the Anglo-American position on the new weapon s first use ... 

Compounds asterisked have been identihed as present in either the female s abdominal tip or her effluvium. The remaining compounds have been determined as attractants or antagonists of attraction (-) by empirical screening in the field t Flight periods for the lower Hudson Valley of New York according to Chapman and Lienk (1971)... 

Waines, R. H. and Hoar, F., Upper Silurian-Lower Devonian Stratigraphic Sequence, Western Mid-Hudson Valley Region, Ulster County, New York, New York State Geological Association, Guidebook to Field Trips, Vol. 39, 1967, pp. D1-D28. 

Waines, R. H., The Quassaic Group, a Medial to Late Ordovician Arenite Sequence in the Mari-boro Mountains Outlier, Mid-Hudson Valley, New York, U.S.A., Geol. J., Vol. 21, 1986, pp. 

Among Totten s conclusions were findings that lime hydrated to a powder by sprinkling with carefully controlled amounts of water produced stronger mortar than lime made into a paste or putty by using excess water for slaking. He also concluded that New York cements were of the highest quality. This reference led to a search for the source of those cements, which were known to have come from the Town of Rosendale, in the Hudson Valley. 

FIG. 1—Map (A) showing the location of the Rosendale natural cement region in the central Hudson Valley of southeastern New York State. Dotted outline corresponds with area of larger map (B), which illustrates the relative locations of major natural cement producing locations within the Rosendale natural cement region. The trace of the Delaware and Hudson Canal in the Rosendale region follows State Route 213 and the Rondout Creek from High Falls to Eddyville. 

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