Rdxfbgrtj

This article may be expanded with text translated from the corresponding article in Japanese. (October 2018) Click [show] for important translation instructions. View a machine-translated version of the Japanese article. Machine translation like Deepl or Google Translate is a useful starting point for translations, but translators must revise errors as necessary and confirm that the translation is accurate, rather than simply copy-pasting machine-translated text into the English Wikipedia. Do not translate text that appears unreliable or low-quality. If possible, verify the text with references provided in the foreign-language article. You must provide copyright attribution in the edit summary by providing an interlanguage link to the source of your translation. A model attribution edit summary (using German): Content in this edit is translated from the existing German Wikipedia article at [[:de:Exact name of German article]]; see its history for attribution. You should also add the template {{Translated|ja|利根川}} to the talk page. For more guidance, see Wikipedia:Translation.

Tone River
Tone River at Narita and Kawachi (2015)
Native name	利根川
Country	Japan
Physical characteristics
Main source	Mount Ōminakami 1,831 m (6,007 ft)
River mouth	Pacific Ocean 0 m (0 ft)
Length	322 km (200 mi)
Discharge	Average rate: 256 m3/s (9,000 cu ft/s)
Basin features
Basin size	16,840 km2 (6,500 sq mi)

The Tone River (利根川, Tone-gawa) is a river in the Kantō region of Japan. It is 322 kilometers (200 mi) in length (the second longest in Japan after the Shinano) and has a drainage area of 16,840 square kilometers (6,500 sq mi) (the largest in Japan). It is nicknamed Bandō Tarō (坂東太郎); Bandō is an obsolete alias of the Kantō Region, and Tarō is a popular given name for an oldest son.^[1] It is regarded as one of the "Three Greatest Rivers" of Japan, the others being the Yoshino in Shikoku and the Chikugo in Kyūshū.

Geography

The source of the Tone River is at Mount Ōminakami (大水上山) (1,831 meters (6,007 ft)) in the Echigo Mountains, which straddle the border between Gunma and Niigata Prefectures in Jōshin'etsu Kōgen National Park.^[1] The Tone gathers tributaries and pours into the Pacific Ocean at Cape Inubō, Choshi in Chiba Prefecture.^[2]

Tributaries

Major tributaries of the Tone River include the Agatsuma, Watarase, Kinu, Omoi, and the Kokai. The Edo River branches away from the river and flows into Tokyo Bay.

History

Rivers in Kantō in the 16th century

Rivers in Kantō in the 20th century

The Tone River was once known for its uncontrollable nature, and its route changed whenever floods occurred. It is hard to trace its ancient route, but it originally flowed into Tokyo Bay along the route of the present-day Edo River, and tributaries like the Watarase and Kinu had independent river systems. For the sake of water transportation and flood control, extensive construction began in the 17th century during the Tokugawa shogunate, when the Kantō region became the political center of Japan.^[3] The course of the river was significantly changed, and the present route of the river was determined during the Meiji period,^[4] with the assistance of Dutch civil engineer Anthonie Rouwenhorst Mulder^[5]. Its vast watershed is thus largely artificial.

Two ships of the Imperial Japanese Navy were named after the river, one of World War I vintage and another from World War II, the lead ship of its class.

Fukushima Daiichi nuclear disaster

As a result of the Fukushima Daiichi nuclear disaster radioactive cesium concentrations of 110 becquerels per kilogram were found in silver crucian carp fish caught in the Tone River in April 2012. The river is 180 kilometres (110 mi) from the Fukushima Daiichi Plant. Six fishery cooperatives and 10 towns along the river were asked to stop all shipments of fish caught in the Tone.^[6]

Use

Kurihashi Water Level Observatory (June 2005)

The Tone River was an indispensable inland water link between the capitol at Edo, and later Tokyo, to the Pacific Ocean. It carried not only local products like soy sauce from Choshi, but also products from the Tōhoku region, in order to save time and to avoid risk in the open sea. With the advent of the railway in the 19th century major shipping on the Tone quickly declined, and inland ports such as Noda, Sekiyado, now part of Noda, Nagareyama, and Sawara, now part of Katori diminished in importance.^[2] Today the river has several dams that supply water for more than 30 million inhabitants of metropolitan Tokyo and large-scale industrial areas such as the Keiyō Industrial Zone.

Rafting and kayaking

The Minakami onsen area in Gunma Prefecture is near the source for the Tone River and during the Spring snow melt period, April - June, the river provides consistent grade 4 rapids (on the International Scale of River Difficulty) over a 12 kilometers (7.5 mi) stretch. The river provides some of the best white water rafting and kayaking in Japan. The snow melt swells the river to grade 4 in spring; in the summer it is a gentle grade 2. The Momijikyo section has 7 grade 3-4 rapids for 1 kilometer (0.62 mi) and is 12 kilometers (7.5 mi) long in total.^[7]

References

Wikimedia Commons has media related to Tone River.

Coordinates: 35°59′01″N 139°53′26″E / 35.98361°N 139.89056°E / 35.98361; 139.89056