English Coastal Evolution
English Coastal Evolution
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In our eReader you can find the full English version of the book. Read English Coastal Evolution 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 English Coastal Evolution
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Leonards and in western Hastings by buildings, but elsewhere they rise steeply, increasing in altitude from the low clay cliffs at Bexhill to some two hundred feet at the Castle and over three hundred feet near Fairlight. Everywhere where not artificially protected they are being actively cut back by the waves. The hill ridges must once, then, have extended further seawards. The cliffs in which they end must have been developed during their recession. The 180 ENGLISH COASTAL EVOLUTION EVOLUTION... OF S. E. COASTS (I) 181 Asten and Priory valleys are occupied by low- level tracts of alluvium which show that once they were arms of the sea ; the flat ribbon of alluvial lands winds up the Priory Valley for one and a half miles from its mouth and is still below high-water mark.
The former irregularity of the coastline is then evident. The exact distance to which the head- lands extended seawards at the beginning of the present period of unchanging sea-level is discussed in the next chapter. It can obviously only be roughly estimated.
What to read after English Coastal Evolution?
You can find similar books in the "Read Also" column, or choose other free books by Edith Marjorie Ward to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Leonards and in western Hastings by buildings, but elsewhere they rise steeply, increasing in altitude from the low clay cliffs at Bexhill to some two hundred feet at the Castle and over three hundred feet near Fairlight. Everywhere where not artificially protected they are being actively cut back by the waves. The hill ridges must once, then, have extended further seawards. The cliffs in which they end must have been developed during their recession. The 180 ENGLISH COASTAL EVOLUTION EVOLUTION... OF S. E. COASTS (I) 181 Asten and Priory valleys are occupied by low- level tracts of alluvium which show that once they were arms of the sea ; the flat ribbon of alluvial lands winds up the Priory Valley for one and a half miles from its mouth and is still below high-water mark.
The former irregularity of the coastline is then evident. The exact distance to which the head- lands extended seawards at the beginning of the present period of unchanging sea-level is discussed in the next chapter. It can obviously only be roughly estimated.
What to read after English Coastal Evolution?
You can find similar books in the "Read Also" column, or choose other free books by Edith Marjorie Ward to read onlineMoreLess
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