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Sandstone, Dent Marble arches: II: 35.7m high with 11 spans. Arthington Viaduct a.k.a. Wharfedale Viaduct: Arthington, West Yorkshire: 460 m (1,510 ft) 1849: Stone arch: II: 21 arches. Crosses the Wharfe valley. Carries the Leeds to Harrogate line. Also known as Castley Viaduct: Avonbank Viaduct: Whitecross, Falkirk: 105 m (344 ft) 1847: Stone ...
Red Marble Grade, Topton, North Carolina. A 2015 survey [12] lists the 3.5 mile stretch between MP 87 and MP 90.5 at a 4% average grade and says there are isolated stretches approaching 7%. When originally built the ruling grade was 4.2% as listed by southern railway. But due to the fills settling it has drastically changed. [12]
A "grandfather" is the largest marble, the size of a billiards ball or tennis ball. Various names for different marble types (regional playground talk, Leicester, UK): Marleys (marbles), prit (white marble), Kong (large marble), King Kong (larger than a bosser), steely (metal bearing-ball). Names can be combined: e.g. prit-Kong (large white ...
Railway lines in England and Wales, as of 2010 This is a list of railway lines in Great Britain that are currently in operation, split by country and region . There are a limited number of main inter-regional lines, with all but one entering Greater London . [ 1 ]
A smaller number of lines were formerly industrial or colliery railways. Many of these preserved railways are mentioned in national and international tour guides, and visits may form part of a school curriculum or feature in other studies, including civil engineering, mechanics, social, economic and political history, visual arts and drama.
The Marble Arch is a 19th-century white marble-faced triumphal arch in London, England. The structure was designed by John Nash in 1827 as the state entrance to the cour d'honneur of Buckingham Palace ; it stood near the site of what is today the three-bayed, central projection of the palace containing the well-known balcony. [ 1 ]
Enjoy a classic game of Hearts and watch out for the Queen of Spades!
Marble is a rock resulting from metamorphism of sedimentary carbonate rocks, most commonly limestone or dolomite. Metamorphism causes variable re-crystallization of the original carbonate mineral grains. The resulting marble rock is typically composed of an interlocking mosaic of carbonate crystals.