The Building of the British Isles
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In our eReader you can find the full English version of the book. Read The Building of the British Isles 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 Building of the British Isles
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In the British region nothing comparable with the Muschelkalk is found, so that only the Lower and Upper divisions of the Trias are represented in this country. Of the distribution and com- ponent materials of these two divisions some account will now be given, dealing first with the Bunter and then with the Keuper.
1. LOWER TRIASSIC TIME A. Stratigraphical Evidence In most parts of England there is a certain amount of un- conformity between the Permian and the Bunter, but it is not so great as... some have supposed, and it does not indicate any great terrestrial disturbance. In the northern and central parts of the country there seems to have been some tilting of the Permian Beds and some rupturing of the older rocks by faults during the interval, and this interval may have been a considerable period of time ; but the physical changes were not great, for the Bunter deposits practically occupy the same areas as the Permian, though in many places it is evident that they passed over and beyond them, so as to cover wider spaces.
What to read after The Building of the British Isles?
You can find similar books in the "Read Also" column, or choose other free books by A J Alfred John Jukes Browne to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
In the British region nothing comparable with the Muschelkalk is found, so that only the Lower and Upper divisions of the Trias are represented in this country. Of the distribution and com- ponent materials of these two divisions some account will now be given, dealing first with the Bunter and then with the Keuper.
1. LOWER TRIASSIC TIME A. Stratigraphical Evidence In most parts of England there is a certain amount of un- conformity between the Permian and the Bunter, but it is not so great as... some have supposed, and it does not indicate any great terrestrial disturbance. In the northern and central parts of the country there seems to have been some tilting of the Permian Beds and some rupturing of the older rocks by faults during the interval, and this interval may have been a considerable period of time ; but the physical changes were not great, for the Bunter deposits practically occupy the same areas as the Permian, though in many places it is evident that they passed over and beyond them, so as to cover wider spaces.
What to read after The Building of the British Isles?
You can find similar books in the "Read Also" column, or choose other free books by A J Alfred John Jukes Browne to read onlineMoreLess
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