The Physical Geology of the Dee Valley
The Physical Geology of the Dee Valley
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In our eReader you can find the full English version of the book. Read The Physical Geology of the Dee Valley 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 Physical Geology of the Dee Valley
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To quickly assess the difficulty of the text, read a short excerpt:
Vertical Scale, ^" = 100'.
Photo by y. Mathieson. VIEW J. Gorge of the Ey Burn from the Ledge called the " Colonel's Bed".
The upper portion of Glen Ey from the great bend up to Alltan- odhar Shieling has the shape typical of ice-erosion steep sides, flat bottom ; the gradient of the stream, too, is here exceptionally low, 50 feet per mile, which is less than half the average fall between the 1, 500 feet contour line and the junction of the Ey and Dee.
A wide hollow lies between Morven on the n...orth and the granite hills, Culblean and Crannach Hill, with the epidiorite hill, Creagan THE PHYSICAL GEOLOGY OF THE DEE VALLEY.
29 Riach, on the south. It is occupied by peat moss and sheep-pasture, and is drained by the Rashy Burn and other insignificant streams that unite to form the Tullich Burn. The outline sketch will show the discordance between the extent of the hollow and the size of the streamlets, as well as the curious way in which the latter quit the wide upper basin to breach the granite ridge.
What to read after The Physical Geology of the Dee Valley?
You can find similar books in the "Read Also" column, or choose other free books by Alexander Bremner to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Vertical Scale, ^" = 100'.
Photo by y. Mathieson. VIEW J. Gorge of the Ey Burn from the Ledge called the " Colonel's Bed".
The upper portion of Glen Ey from the great bend up to Alltan- odhar Shieling has the shape typical of ice-erosion steep sides, flat bottom ; the gradient of the stream, too, is here exceptionally low, 50 feet per mile, which is less than half the average fall between the 1, 500 feet contour line and the junction of the Ey and Dee.
A wide hollow lies between Morven on the n...orth and the granite hills, Culblean and Crannach Hill, with the epidiorite hill, Creagan THE PHYSICAL GEOLOGY OF THE DEE VALLEY.
29 Riach, on the south. It is occupied by peat moss and sheep-pasture, and is drained by the Rashy Burn and other insignificant streams that unite to form the Tullich Burn. The outline sketch will show the discordance between the extent of the hollow and the size of the streamlets, as well as the curious way in which the latter quit the wide upper basin to breach the granite ridge.
What to read after The Physical Geology of the Dee Valley?
You can find similar books in the "Read Also" column, or choose other free books by Alexander Bremner to read onlineMoreLess
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