Key to a Chart of the Successive Geological Formations With An Actualsection Fr
Key to a Chart of the Successive Geological Formations With An Actualsection Fr
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In our eReader you can find the full English version of the book. Read Key to a Chart of the Successive Geological Formations With An Actualsection Fr 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 Key to a Chart of the Successive Geological Formations With An Actualsection Fr
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Above the Coal measures, and overlying them, sometimes conformably, and at other times unconformably, is found a series of red sandstones, red, green, and variegated shales, marls, and sandstones, with yellow magnesian limestones. These contain few traces of vegetation, and the organic remains are quite distinct from those in the rocks below. The system has been divided into Permian and Triassic systems.
The rocks recognized as of the New Red Sand- stone period, are the sandstones and shales of... the Connecticut River valley, New Jersey, Virginia, and North Carolina. These belong apparently to the Triassic System, and represent a portion of the upper marls and sandstones of the period, as more fully developed in Europe. The remains of fishes, and the tracks of birds, which have been so beauti- fully developed and illustrated by Professor Hitch- cock, Dr. Deane, Mr. Redfield, and Mr. Marsh, are among the interesting fossil remains of this period in the United States.
It will be observed that no American localities are given upon the chart for any of the strata of the Permian system, none of its members having yet been found in this .
What to read after Key to a Chart of the Successive Geological Formations With An Actualsection Fr?
You can find similar books in the "Read Also" column, or choose other free books by James Hall to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Above the Coal measures, and overlying them, sometimes conformably, and at other times unconformably, is found a series of red sandstones, red, green, and variegated shales, marls, and sandstones, with yellow magnesian limestones. These contain few traces of vegetation, and the organic remains are quite distinct from those in the rocks below. The system has been divided into Permian and Triassic systems.
The rocks recognized as of the New Red Sand- stone period, are the sandstones and shales of... the Connecticut River valley, New Jersey, Virginia, and North Carolina. These belong apparently to the Triassic System, and represent a portion of the upper marls and sandstones of the period, as more fully developed in Europe. The remains of fishes, and the tracks of birds, which have been so beauti- fully developed and illustrated by Professor Hitch- cock, Dr. Deane, Mr. Redfield, and Mr. Marsh, are among the interesting fossil remains of this period in the United States.
It will be observed that no American localities are given upon the chart for any of the strata of the Permian system, none of its members having yet been found in this .
What to read after Key to a Chart of the Successive Geological Formations With An Actualsection Fr?
You can find similar books in the "Read Also" column, or choose other free books by James Hall to read onlineMoreLess
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