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Lynch Brook : ウィキペディア英語版
River Lynch

The River Lynch, also known as the Lynch Brook, is a minor tributary of the River Lea in Hoddesdon, Hertfordshire, England.
==History==
Historically, the River Lynch was named after the flat terraces, known as a lynch in Old English, which were formed when cultivating the steep slopes of a river valley, much the same as the rice terraces of South East Asia. The terrace, or lynch, was designed to reduce soil erosion by slowing the rapid run-off of water, and a series of these terraces gave the Lynch landscape a stepped appearance. These terraces were used extensively in the area directly above the River Lynch for the production of water cress during the 19th and early 20th centuries, using the fertile brick earth soils of the valley sides. The site of these former terraces is still clearly visible today within the Lampits housing estate, in the sloping open area below the course of the New River, leading downhill to Conduit Lane East and the Lynch Mill Pond.
The terraces at the Lynch were situated above a deep funnel-shaped natural hole that carried water up from the chalk. The pond and watermill at Lynch Corner, fed by the spring, were described in medieval court rolls, as being ancient and known locally as 'Le Lince.' 〔Tregelles, J.A, ''A History of Hoddesdon in the County of Hertfordshire'', 1908, p99-100〕
The New River, which passes directly overhead, closely hugging the 100 foot contour of the Lea Valley, destroyed much of the original landscape of the area, notably Lynch Hill and the Lynch Gap.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「River Lynch」の詳細全文を読む



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