trough
91Slyne-Erris Trough — The Slyne Erris Trough is a geological basin off the west coast of Donegal, Ireland.In recent years it has been shown to be prospective for hydrocarbons, hosting Shell s Corrib gas field (discovered by Enterprise Oil, bought by Shell), and… …
92Oil Trough, Arkansas —   Town   …
93Laurentian Trough — ▪ submarine trough, North America submarine glacial trough in the eastern continental shelf of North America, the most impressive such feature on Earth. It extends from the mouth of the St. Lawrence River eastward through the Gulf of St.… …
94Xihu Trough — The Xihu Trough (Chinese: 西湖凹陷) is a region in the East China Sea, located approximately 400 kilometres east of the cities of Shanghai and Ningbo, China. The Xihu Trough falls within the territorial waters of China. The region is a repository for …
95Parabolic trough — A parabolic trough is a type of solar thermal energy collector. It is constructed as a long parabolic mirror (usually coated silver or polished aluminum) with a Dewar tube running its length at the focal point. Sunlight is reflected by the mirror …
96Metropolitan Drinking Fountain and Cattle Trough Association — Advertisement from Burke s Peerage, 1879. The Metropolitan Drinking Fountain and Cattle Trough Association was an association set up in London by Samuel Gurney an MP and philanthropist and Edward Thomas Wakefield, a barrister in 1859 to provide… …
97Watering Trough — A Watering Trough or (artificial watering point)is a receptacle for the storage of water so both domestic and non domestic livestock can obtain drinking water. In Australia, the watering trough is established so that sheep, cattle and other… …
98Rockall Bank and Trough — The Rockall Trough (Scottish Gaelic: Clais Sgeir Rocail ) is a deep water bathymetric feature to the northwest of Scotland and Ireland, running roughly from southwest to northeast, flanked on the north by the Rockall Plateau and to the south by… …
99Tropical Upper Tropospheric Trough — A Tropical Upper Tropospheric Trough (TUTT) is a trough situated in upper level (at about 200 hPa) tropics. Its formation is usually caused by the expansion of the Trough of Westerlies Wind to the tropics. It can also develop from the inverted… …
100Near-equatorial trough — Since 1954, studies concluded that the near equatorial trough was associated with a maximum in oceanic sea surface temperature. It is sometimes used as a synonym for the terms near equatorial tradewind convergence,[1] Intertropical convergence… …
