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The Malvern Hills in the United Kingdom, said by Alfred Watkins to have a ley line passing along their ridge. Ley lines (/ l eɪ ˈ l aɪ n z /) are straight alignments drawn between various historic structures, prehistoric sites and prominent landmarks. The idea was developed in early 20th-century Europe, with ley line believers arguing that ...
Like many places dedicated to St. Michael, the aligned sites are almost all located on prominent hilltops or other hard to reach places, and include Skellig Michael, St Michael's Mount, Mont Saint-Michel, the Sacra di San Michele, San Michele Arcangelo, the Sanctuary of Monte Sant'Angelo, the Panormitis Monastery of the Archangel Michael, and Stella Maris Monastery.
One criticism of Watkins' ley line theory states that given the high density of historic and prehistoric sites in Britain and other parts of Europe, finding straight lines that "connect" sites is trivial and ascribable to coincidence. A statistical analysis of lines concluded: "the density of archaeological sites in the British landscape is so ...
Many highways and railway lines in modern Japan follow the ancient routes and carry the same names. The early roads radiated from the capital at Nara or Kyoto. Later, Edo was the reference, and even today Japan reckons directions and measures distances along its highways from Nihonbashi in Chūō, Tokyo.
He was an intensely rational person with an active intellect, and I think he would be a bit disappointed with some of the fringe aspects of ley lines today. — John Bruno Hare, 17 June 2004 [ 9 ] In 2002 Watkins had a beer named after him, "Watkins' Triumph", brewed by Wye Valley Brewery Ltd. [ 10 ]
Column 4 indicates on which sheet, if any, of the British Geological Survey's 1:50,000 / 1" scale geological map series of England and Wales, the fault is shown and named (either on map/s or cross-section/s or both). A handful of BGS maps at other scales are listed too.
Pages in category "Ley lines" The following 7 pages are in this category, out of 7 total. This list may not reflect recent changes. ...
The geology of England is mainly sedimentary. The youngest rocks are in the south east around London , progressing in age in a north westerly direction. [ 1 ] The Tees–Exe line marks the division between younger, softer and low-lying rocks in the south east and the generally older and harder rocks of the north and west which give rise to ...