Notes On Geological Map Reading
The book Notes On Geological Map Reading was written by author Here you can read free online of Notes On Geological Map Reading book, rate and share your impressions in comments. If you don't know what to write, just answer the question: Why is Notes On Geological Map Reading a good or bad book?
Where can I read Notes On Geological Map Reading for free?
In our eReader you can find the full English version of the book. Read Notes On Geological Map Reading 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 Notes On Geological Map Reading
In our eReader you can find the full English version of the book. Read Notes On Geological Map Reading 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 Notes On Geological Map Reading
What reading level is Notes On Geological Map Reading book?
To quickly assess the difficulty of the text, read a short excerpt:
To realise the relation, turn to figs. 14-16, and suppose ad and bf now to represent one and the same bedding-plane on opposite sides of a dip-fault ; or for a strike-fault imagine the bedding-plane on one side produced across the fault. It is easily seen that the relation between the vertical throw of a fault and the shift which it causes is precisely the same as the relation between the vertical thickness of a formation and the width of its outcrop. The discussion in 20, 21 can therefore be a...pplied, with the necessary substitution of terms, to the case of faulting. Note that the boundary-line on the downthrow side is always shifted backward (i. E. In the direction opposite to that of dip), save only in the exceptional case (fig. 16, B) in which the slope is steeper than the dip.
(27) For illustration take first the strike-fault shown in fig. 19. Here the dip, 100 in 1125, is seen to be the same on both sides of the fault. The downthrow is north-westward, and so against the dip. Accordingly there is repetition of beds in a traverse downstream, the formation A reappearing as a " faulted inlier.
What to read after Notes On Geological Map Reading?
You can find similar books in the "Read Also" column, or choose other free books by Alfred Harker to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
To realise the relation, turn to figs. 14-16, and suppose ad and bf now to represent one and the same bedding-plane on opposite sides of a dip-fault ; or for a strike-fault imagine the bedding-plane on one side produced across the fault. It is easily seen that the relation between the vertical throw of a fault and the shift which it causes is precisely the same as the relation between the vertical thickness of a formation and the width of its outcrop. The discussion in 20, 21 can therefore be a...pplied, with the necessary substitution of terms, to the case of faulting. Note that the boundary-line on the downthrow side is always shifted backward (i. E. In the direction opposite to that of dip), save only in the exceptional case (fig. 16, B) in which the slope is steeper than the dip.
(27) For illustration take first the strike-fault shown in fig. 19. Here the dip, 100 in 1125, is seen to be the same on both sides of the fault. The downthrow is north-westward, and so against the dip. Accordingly there is repetition of beds in a traverse downstream, the formation A reappearing as a " faulted inlier.
What to read after Notes On Geological Map Reading?
You can find similar books in the "Read Also" column, or choose other free books by Alfred Harker to read onlineMoreLess
Read book Notes On Geological Map Reading for free
You can download books for free in various formats, such as epub, pdf, azw, mobi, txt and others on book networks site. Additionally, the entire text is available for online reading through our e-reader. Our site is not responsible for the performance of third-party products (sites).
Write Review:
Guest
Read Also
9 / 10
User Reviews: