The Triassic And Permian Rocks of the Midland Counties of England
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In our eReader you can find the full English version of the book. Read The Triassic And Permian Rocks of the Midland Counties of England 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 The Triassic And Permian Rocks of the Midland Counties of England
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Morton, F. G. S.
J Page 58.
85 which passes close to the Lime Street station ; the amount of throw is here about 400 feet. The throw of the ^Everton Fault is about 1, 500 at the centre of the town. * Mr. G. H. Morton, in his work on " The Geology of Liverpool, " has very fully described these beds as observed in the three tunnels which pass under the town, namely, those of Waterloo, Lime Street, and Wapping, all converging at their eastern extremities at Edge Hill. In all of them, the Everton f...ault was observed, and on the downthrow side the Lower Keuper Sandstone series, as follows : ft.
a. Upper beds (Wapping Tunnel). Laminated reddish sand- stones and shales - - 150 b. Lower shale series (St. James Cemetery). Grey, white, and reddish laminated sandy shales - - - 50 c. White and yellowish freestone, resting on harder pebbly sandstone .. -__- 175 3/5 All over this district, the basement beds of the Keuper series rest on a highly eroded surface of the Hunter, and we have here evidence that there has been considerable denudation of the Upper Mottled Sandstone of the latter division, before the more recent beds of the Keuper were deposited upon it ; for at the southern side of the town, as pointed out to me by Mr.
What to read after The Triassic And Permian Rocks of the Midland Counties of England?
You can find similar books in the "Read Also" column, or choose other free books by Edward Hull to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Morton, F. G. S.
J Page 58.
85 which passes close to the Lime Street station ; the amount of throw is here about 400 feet. The throw of the ^Everton Fault is about 1, 500 at the centre of the town. * Mr. G. H. Morton, in his work on " The Geology of Liverpool, " has very fully described these beds as observed in the three tunnels which pass under the town, namely, those of Waterloo, Lime Street, and Wapping, all converging at their eastern extremities at Edge Hill. In all of them, the Everton f...ault was observed, and on the downthrow side the Lower Keuper Sandstone series, as follows : ft.
a. Upper beds (Wapping Tunnel). Laminated reddish sand- stones and shales - - 150 b. Lower shale series (St. James Cemetery). Grey, white, and reddish laminated sandy shales - - - 50 c. White and yellowish freestone, resting on harder pebbly sandstone .. -__- 175 3/5 All over this district, the basement beds of the Keuper series rest on a highly eroded surface of the Hunter, and we have here evidence that there has been considerable denudation of the Upper Mottled Sandstone of the latter division, before the more recent beds of the Keuper were deposited upon it ; for at the southern side of the town, as pointed out to me by Mr.
What to read after The Triassic And Permian Rocks of the Midland Counties of England?
You can find similar books in the "Read Also" column, or choose other free books by Edward Hull to read onlineMoreLess
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