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Robert M. (Bob) Cunningham (July 1, 1919 – April 15, 2008) was an American cloud physicist.He specialized in the study of fog, running a weather research station on Kent Island in the Bay of Fundy for over 60 years.
Mount Tsurumi is a lava dome. It has several peaks, including Mount Kuranoto, Mount Uchi, and Mount Garan. It has several peaks, including Mount Kuranoto, Mount Uchi, and Mount Garan. This mountain is one of the Japan 300 mountains , and a part of Aso Kujū National Park .
The Beppu Ropeway (別府ロープウェイ, Beppu rōpuwei) is a Japanese aerial lift line in Beppu, Ōita.This is the only line operated by Beppu Ropeway, a subsidiary of the Kintetsu Group.
Tsurumi was connected to Yokohama and Tokyo by train in 1872, and the area rapidly urbanized. Sōji-ji, the head temple of the Sōtō sect of Zen Buddhism relocated to Tsurumi from Ishikawa Prefecture in 1911. Tsurumi suffered severe damage from the 1923 Great Kantō earthquake. In April 1924, Tsurumi became a town within Tachibana District.
Tsurumi-ryokuchi Station (鶴見緑地駅, Tsurumi-ryokuchi-eki, Station Number: N26) is a train station on the Osaka Metro Nagahori Tsurumi-ryokuchi Line in Tsurumi-ku, Osaka, Japan. [1] The line was opened to provide access to Tsurumi-ryokuchi Park during the 1990 International Garden and Greenery Exposition .
The Tsurumi River (鶴見川, Tsurumi-gawa) is a river in Kanagawa and Tokyo Prefectures on Honshū, Japan. It begins in Kamioyamada-machi, Machida and flows 42.5 kilometers before emptying into Tokyo Bay at the Keihin industrial area of Tsurumi-ku, Yokohama .
Umi-Shibaura Station (海芝浦駅, Umi-shibaura-eki) is a railway station on the Tsurumi Line in Tsurumi-ku, Yokohama, Kanagawa Prefecture, Japan, operated by East Japan Railway Company (JR East). The station is located on the grounds of Toshiba's Keihin Product Operations, and the only exit from the station is into the company's grounds. As a ...
Another way fog forms in deserts occurs when a desert is close to an ocean which has a cold current. When air is heated over desert land and blows towards the cool water in the ocean, it condenses and fog is formed. The cool fog is then blown inland by the ocean breeze. Fog is mainly formed in the early morning or after sunset. [5]