Encyclopaedia Britannica, 11th Edition, volume 3, Part 1, Slice 2
Encyclopaedia Britannica, 11th Edition, volume 3, Part 1, Slice 2
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In our eReader you can find the full English version of the book. Read Encyclopaedia Britannica, 11th Edition, volume 3, Part 1, Slice 2 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 Encyclopaedia Britannica, 11th Edition, volume 3, Part 1, Slice 2
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To quickly assess the difficulty of the text, read a short excerpt:
V. _) are sometimes classed with the overlyingBarton clay as Middle Bagshot. In the London basin the Barton beds areunknown. In Surrey and Berkshire the Bracklesham beds are from 20 to 50 ft. Thick; in Alum Bay they are 100 ft. , with beds of lignite in the lowerportion; and about here they are sharply marked off from the Barton clay bya bed of conglomerate formed of flint pebbles. The Upper Bagshot beds, Barton sand and Barton clay, are from 140 to 200 ft. Thick in the Isle ofWight.
The Aggles...tone (or Haggerstone) rock and Puckstone rock, near Studland inDorsetshire, are formed of large indurated masses of the Lower Bagshot bedsthat have resisted the weather; Creechbarrow near Corfe is another strikingfeature due to the same beds. Many of the sarsen stones or greywethers ofS. E. England have been derived from Bagshot strata.
See _Memoirs of the Geological Survey_ (England):--"Geology of the Isle ofWight, " new edition (1889); "The Geology of London and Part of the ThamesValley, " vol.
What to read after Encyclopaedia Britannica, 11th Edition, volume 3, Part 1, Slice 2?
You can find similar books in the "Read Also" column, or choose other free books by Various to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
V. _) are sometimes classed with the overlyingBarton clay as Middle Bagshot. In the London basin the Barton beds areunknown. In Surrey and Berkshire the Bracklesham beds are from 20 to 50 ft. Thick; in Alum Bay they are 100 ft. , with beds of lignite in the lowerportion; and about here they are sharply marked off from the Barton clay bya bed of conglomerate formed of flint pebbles. The Upper Bagshot beds, Barton sand and Barton clay, are from 140 to 200 ft. Thick in the Isle ofWight.
The Aggles...tone (or Haggerstone) rock and Puckstone rock, near Studland inDorsetshire, are formed of large indurated masses of the Lower Bagshot bedsthat have resisted the weather; Creechbarrow near Corfe is another strikingfeature due to the same beds. Many of the sarsen stones or greywethers ofS. E. England have been derived from Bagshot strata.
See _Memoirs of the Geological Survey_ (England):--"Geology of the Isle ofWight, " new edition (1889); "The Geology of London and Part of the ThamesValley, " vol.
What to read after Encyclopaedia Britannica, 11th Edition, volume 3, Part 1, Slice 2?
You can find similar books in the "Read Also" column, or choose other free books by Various to read onlineMoreLess
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