Summary

| override_editor Encyclopædia Britannica, Ninth Edition…

Galveston Island is a low sandy island, about 28 miles long and 1 to 3 miles wide, stretching along the coast of Texas in a north-easterly and south-westerly direction, and forming the gulf coast-line throughout its entire length. Its surface, which has an average height of 4 to 5 feet above tide level, is diversified by a number of freshwater ponds and intersected by several creeks and small bayous. The beach, on the Gulf side, furnishes a smooth and pleasant drive during low-water stage, and excellent surf-bathing at all times.
Source: Wikisource

| override_editor Encyclopædia Britannica, Ninth Edition…

The mean rise and fall of tide at Galveston is 1 feet, but spring-tides occasionally rise more than 3 feet above, and fall nearly 2 feet below the plane of mean low water, and fluctuations between much wider limits are not uncommon under the influence of heavy winds. During a storm which occurred in October 1867 the water rose 6 feet above mean low-water stage, and in September 1875 it rose in some portions of the bay 7 feet, and in others 9 feet above the same level. Two years later there was a rise of 5 feet, produced by an onshore wind which reached a maximum velocity of 60 miles per hour.
Source: Wikisource

| override_editor Encyclopædia Britannica, Ninth Edition…

It frequently attains a height of 20 to 25 feet, and grows rapidly from slips with great luxuriance, blooming the year round. The fig, orange, the black Hamburg and other kinds of grape, and many varieties of flowers and evergreen shrubbery, thrive and flourish. Throughout the most thickly-settled portions of the city the sidewalks are paved with either asphaltum, concrete, brick, or German or English tiles. Oleander Park embraces 80 acres, and the city park about 25 acres, and there are three public gardens and six public squares.
Source: Wikisource

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