Directory for the Pacific Coast of the United States Reported to the Superinten

U.S. Coast And Geodetic Survey

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28m. ; and of the stand, Oh. 33m. The average difference between the corrected establishments of the a. M. And p. M. Tides of the same day is Ih. 02wi. For high water and Oh. 52m. For low water. The differences when the moon's declination is greatest ~ Named hv Vancouver in 1792.
Till: I'M II. H MA IKS COAST SUIIVEY. '. >"> , . L^iii. And l/i. L"i;ii. Respectively. Tlio average difference in height of those two li t fur tin- high waters ami '2. 3 feet lor the low waters. When tin- moon's declin...ation is . >t those dill'crences are 1. 11 font and . '!. " feet respectively. The average dillbrcnce of tin' highest high ami lu\\. -. -t low waters of the same day is 7. 9 feet, and when the moon's decli- natioii is greate-- The highest high tide iii the twenty-tour hours occurs ulioiit 1 \in. After the moon's upper Iran-it, (southing, ) when the moon'. - derlination is north, and iilmiit O/i. 1")H. Before, when south. The lowest of the low waters occurs about TA hours after the highest high water.

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