A Geological History of Manhattan Or New York Island Together With a Map of Th
A Geological History of Manhattan Or New York Island Together With a Map of Th
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In our eReader you can find the full English version of the book. Read A Geological History of Manhattan Or New York Island Together With a Map of Th Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book A Geological History of Manhattan Or New York Island Together With a Map of Th
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2. ) The locality of this rock is between the town of New- port and Fort Adams, near the Granite ; it is a black variety of nearly the same quality as the Serpentine of New York Island.
3d Talcose Slate. (See p late 6, fig. 3. ) This rock, may be seen at Fort Adams, in the area of A GEOLOGICAL HISTORY. 61 that fortification ; it is very similar to its brother rocks at Stoney Point; veins of Talc, Quartz and Carbonate of Iron run through this rock.
4th Graywacke. (See plate 6 9 jig. 4. ) There w...ere many rocks called Graywacke by the older Geologists, the one which I have retained this name for, is a slaty conglomerate of pebbles and sand, cemented together, by a silicious cement, and without fossils. There are four or more distinct varieties of this rock on this Island, the most curious of which, are seen at the bluff that separates Easton's beach from Sachuest, at the south end of the Island ; at this locality all the varieties may be seen, from the fine grain slaty sandstone or grit, to the coarse conglomerate ; at this locality also, one variety has pebbles of a somewhat ovate form, which lie all in one direction, that is, they are longer than broad and lie side by side, and do not cross each other.
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You can find similar books in the "Read Also" column, or choose other free books by Issachar Cozzens to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
2. ) The locality of this rock is between the town of New- port and Fort Adams, near the Granite ; it is a black variety of nearly the same quality as the Serpentine of New York Island.
3d Talcose Slate. (See p late 6, fig. 3. ) This rock, may be seen at Fort Adams, in the area of A GEOLOGICAL HISTORY. 61 that fortification ; it is very similar to its brother rocks at Stoney Point; veins of Talc, Quartz and Carbonate of Iron run through this rock.
4th Graywacke. (See plate 6 9 jig. 4. ) There w...ere many rocks called Graywacke by the older Geologists, the one which I have retained this name for, is a slaty conglomerate of pebbles and sand, cemented together, by a silicious cement, and without fossils. There are four or more distinct varieties of this rock on this Island, the most curious of which, are seen at the bluff that separates Easton's beach from Sachuest, at the south end of the Island ; at this locality all the varieties may be seen, from the fine grain slaty sandstone or grit, to the coarse conglomerate ; at this locality also, one variety has pebbles of a somewhat ovate form, which lie all in one direction, that is, they are longer than broad and lie side by side, and do not cross each other.
What to read after A Geological History of Manhattan Or New York Island Together With a Map of Th?
You can find similar books in the "Read Also" column, or choose other free books by Issachar Cozzens to read onlineMoreLess
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