翻訳と辞書
Words near each other
・ "O" Is for Outlaw
・ "O"-Jung.Ban.Hap.
・ "Ode-to-Napoleon" hexachord
・ "Oh Yeah!" Live
・ "Our Contemporary" regional art exhibition (Leningrad, 1975)
・ "P" Is for Peril
・ "Pimpernel" Smith
・ "Polish death camp" controversy
・ "Pro knigi" ("About books")
・ "Prosopa" Greek Television Awards
・ "Pussy Cats" Starring the Walkmen
・ "Q" Is for Quarry
・ "R" Is for Ricochet
・ "R" The King (2016 film)
・ "Rags" Ragland
・ ! (album)
・ ! (disambiguation)
・ !!
・ !!!
・ !!! (album)
・ !!Destroy-Oh-Boy!!
・ !Action Pact!
・ !Arriba! La Pachanga
・ !Hero
・ !Hero (album)
・ !Kung language
・ !Oka Tokat
・ !PAUS3
・ !T.O.O.H.!
・ !Women Art Revolution


Dictionary Lists
翻訳と辞書 辞書検索 [ 開発暫定版 ]
スポンサード リンク

Clee Hill : ウィキペディア英語版
Titterstone Clee Hill

Titterstone Clee Hill, sometimes referred to as Titterstone Clee or, incorrectly, Clee Hill (which is the lower hill to the southeast), is a prominent hill in the rural English county of Shropshire, rising at the summit to above sea level.〔
It is one of the Clee Hills, in the Shropshire Hills Area of Outstanding Natural Beauty. The nearest town to the hill is Ludlow, and it can be seen from parts of the town.
==Geography==
Titterstone Clee is the third-highest hill in Shropshire, beaten only by the nearby Brown Clee Hill () and Stiperstones (). Much of the higher part of the hill is common land, used for the grazing of sheep, air traffic control services and both working and disused quarries. The summit of Titterstone Clee is bleak, treeless and shaped by decades of quarrying. Many of the industrial structures still remain, and lend to the ghostly atmosphere of the hill top, especially during the prolonged winter fogs that descend over these hills.
Investigations have led to some individuals to claim that Titterstone Clee was once an active volcano. However, this was conclusively shown to be incorrect in the 1930s when exposures clearly revealed an intrusive origin for the igneous rock which is found beneath the higher ground. Locally this is known as "Dhu Stone" (Welsh for Black Stone); geologically it is an olivine basalt, sometimes coarse enough to be a dolerite. It appears to have been intruded as a sill between sandstone layers within the unconsolidated strata of the Middle Westphalian soon after deposition of the latter.〔(Shropshire Geology - Titterstone Clee )〕
The weather on Titterstone Clee Hill can be particularly hazardous, with locally infamous fog and drizzle being commonplace. Snow and ice can also cause problems in winter, as well as gales.
Most of the summit of the hill is affected by man-made activity, the result of hill fort construction during the Bronze and Iron Ages and, more recently, by years of mining for coal and quarrying for dhustone (dolerite) to be used in road-building. Also, many derelict quarry buildings are scattered over the hill, now used only by sheep sheltering from the worst of weather but interesting from an industrial archaeology point of view as very early examples of the use of reinforced concrete. Combined, these give the summit of the hill an eerie, other worldly feel.
The A4117 between Cleobury Mortimer and Ludlow runs to the south of Titterstone Clee, and rises to 381 metres above sea level at its highest point on Clee Hill Common. Because of this, the road is often affected by snow in winter.
The village of Cleehill lies on this road as it crosses the hill and, at 395 metres above sea level, it is home to the highest pub in Shropshire, called "The Kremlin",〔(BBC Shropshire ) The Kremlin, Cleehill〕 and also to the highest primary school. On the northeast slope of the hill is the small village of Cleeton St Mary.
From the hill it is possible on a clear day to see west to Snowdonia, north east to the Peak District, east to the Black Country, south east to the Cotswolds, south to the Malvern Hills, and south west to the Black Mountains and Brecon Beacons. The hill is said to provide one of the best views in England on a clear day.

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「Titterstone Clee Hill」の詳細全文を読む



スポンサード リンク
翻訳と辞書 : 翻訳のためのインターネットリソース

Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.