A History of the City of Brooklyn and Kings County; in two volumes, Volume I. - The Original Classic Edition(Kobo/電子書)

Finally available, a high quality book of the original classic edition of A History of the City of Brooklyn and Kings County; in two volumes, Volume I.. It was previously published by other bona fide publishers, and is now, after many years, back in print.

This is a new and freshly published edition of this culturally important work by Stephen Ostrander, which is now, at last, again available to you.

Get the PDF and EPUB NOW as well. Included in your purchase you have A History of the City of Brooklyn and Kings County; in two volumes, Volume I. in EPUB AND PDF format to read on any tablet, eReader, desktop, laptop or smartphone simultaneous - Get it NOW.

Enjoy this classic work today. These selected paragraphs distill the contents and give you a quick look inside A History of the City of Brooklyn and Kings County; in two volumes, Volume I.:

Look inside the book:

Until quite recently very few scientific men have even deigned to give it a passing notice, though the assertion may be safely hazarded that scarcely any other tract of land of equal extent on the American Continent furnishes more abundant room for the imagination of geologists to play upon, or that imposes a stronger necessity for conjecturing the operation of some tremendous agency, which in its freaks had invaded the domains of both the land and the ocean, and after completing its sport had silently retired without leaving a track to determine its origin or identify its form.' ...For example, the boulders on the east end are like the granite, gneiss, mica slate, green-stone, and sienite of Rhode Island and the east part of Connecticut; opposite New London and the mouth of the Connecticut River are boulders like the granites, gneiss, and hornblende rock of those localities; opposite New Haven, are found the red sandstone and conglomerate, fissile and micaceous red sandstone, trap conglomerate, compact trap, amygdaloid and verd antique; opposite Black Rock are the granites, gneiss, hornblende, quartz, and white lime-stone, like those in Fairfield County; and from Huntington to Brooklyn, hornblende, crystalline lime-stone, trap, red sandstone, gneiss, and granite, are the same in appearance as those found in the vicinity of the Hudson River.'

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