1270
SECTION V. - ASTRONOMIE SPHÉRIQUE.
11254 SALMON, W.
A table for finding tbe latitude from thealtitude of the polar star, observed at anyhour in the northern hemisphere .
11255 BOILEAU, J. X. A.
À collection of tables, astronomical, meteo-rological, and magnetical, also for determi-ning the altitudes of mountains.
11 25G SANCUEZ y CEBQUERO, J.
Explicacion de las tablas de navegacion yastronomia nautica de J. de Mendoza y Rios.4°, Madrid , 1851.
11 257 DOMKE, F.
Nautische, astronomische und logarith-mische Tafeln, nebst Erklarung und Ge-brauchs-Ànweisung für die PreussischenNavigations-Schulen.
11 258 FOURNIER, C. F.
Manuel du caboteur.
8°, Paris , 1855; 4 pl. « Nouvelle édition, entiè-rement refondue, suivie des principales tablesastronomiques nécessaires aux navigateurs. »
11259 WARD, E. C.
New lunar tables, for correcting theapparent distance of the Moon from the Sun,tixed star, or planet, for the eff'ect of refrac-tion and parallax.
Voyez le n° 11 214.
Traduction.
Neue Mond-Tafeln zur Berichtigung der
scheinbaren Distanz des Mondes von derSonne, eines Fixstern oder Planeten hin-sichtlich Refraction und Parallaxe (par E. F.J. Huwald).
8°, Hamburg, 1857.
II 2GO TUXEN, G. E.
Nautiske, astronomiske og logarithmisketabeller.
8°, Kjobenhavn, 1856.
11261 * * *
Natural versed sines from 0° to 125°, andlogarithmic versed sines from 0° to 135°,or O' 1 to 9 h , used in computing lunar dis-tances for the Nautical Almanac.
112G2 SHARE, J. SI.
Tables for ascertaining a ship’s distancefrom the summit of high land, having takenits altitude above the sea horizon with asextant.
11265 LIN DS A Y, J. B.
The chrono-astrolabe, containing a full setof astronomical tables.
Il 264 CAMERON, P.
The variation and déviation of the compassrectified by azimuth and altitude tables fromthe equator to the latitude of 80 degrees;also by the azimuth and altitude tables arefound in the true position of a ship at sea,the error of the chronometer and the longi-tude; likewise a treatise on magnelism andthe déviations of the compass in iron ships,and the method of observing and correctingthem by magnets.