On the Four Rocks of the New Haven Region, East Rock, West Rock, Pine Rock, And Mill Rock, in Illustration of the Features of Non-Volcanic Igneous Ejections. With a Guide to Walks And Drives About New Haven
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In our eReader you can find the full English version of the book. Read On the Four Rocks of the New Haven Region, East Rock, West Rock, Pine Rock, And Mill Rock, in Illustration of the Features of Non-Volcanic Igneous Ejections. With a Guide to Walks And Drives About New Haven 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 On the Four Rocks of the New Haven Region, East Rock, West Rock, Pine Rock, And Mill Rock, in Illustration of the Features of Non-Volcanic Igneous Ejections. With a Guide to Walks And Drives About New Haven
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To quickly assess the difficulty of the text, read a short excerpt:
The latter rock, in hand specimens, looks like an igneous rock ; but its relation to the slate shows that the two had the same kind of origin. Since it consists largely of the fo'me-feldspar, labradorite, it was probably formed from those portions of the mud of an ancient West Connecticut sea that contained much lime (from the presence of fossils ?). It will be observed that the dip of the slate is small (about 25°) nearly northward.
On Campbell Avenue, at the house of J. Foote, situated high a...bove the avenue, a finely glaciated knoll of rock will be found by the north side of the house ; the rocky knoll is a beautiful example of what Agassiz named " Roches moutonnes " (Sheep- backs). Along the track of the N. Y. & N. H. Railroad, the same facts with regard to the rocks may be seen as in the Derby cut, though less perfectly displayed. At the railroad cut take the path going west and continue for 300 yards neai'ly to a north-and-south road ; thence over the field south, where there has long been an exposure of rock finely glacier-marked, and another of the "roches moutonnes" larger than that in Mr.
What to read after On the Four Rocks of the New Haven Region, East Rock, West Rock, Pine Rock, And Mill Rock, in Illustration of the Features of Non-Volcanic Igneous Ejections. With a Guide to Walks And Drives About New Haven?
You can find similar books in the "Read Also" column, or choose other free books by James Dwight Dana to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The latter rock, in hand specimens, looks like an igneous rock ; but its relation to the slate shows that the two had the same kind of origin. Since it consists largely of the fo'me-feldspar, labradorite, it was probably formed from those portions of the mud of an ancient West Connecticut sea that contained much lime (from the presence of fossils ?). It will be observed that the dip of the slate is small (about 25°) nearly northward.
On Campbell Avenue, at the house of J. Foote, situated high a...bove the avenue, a finely glaciated knoll of rock will be found by the north side of the house ; the rocky knoll is a beautiful example of what Agassiz named " Roches moutonnes " (Sheep- backs). Along the track of the N. Y. & N. H. Railroad, the same facts with regard to the rocks may be seen as in the Derby cut, though less perfectly displayed. At the railroad cut take the path going west and continue for 300 yards neai'ly to a north-and-south road ; thence over the field south, where there has long been an exposure of rock finely glacier-marked, and another of the "roches moutonnes" larger than that in Mr.
What to read after On the Four Rocks of the New Haven Region, East Rock, West Rock, Pine Rock, And Mill Rock, in Illustration of the Features of Non-Volcanic Igneous Ejections. With a Guide to Walks And Drives About New Haven?
You can find similar books in the "Read Also" column, or choose other free books by James Dwight Dana to read onlineMoreLess
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