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Less than 1 kilometre (0.62 mi) later the river carves through a limestone ridge in the Aare Gorge (German: Aareschlucht). [3] It is here that the Aare proves itself to be more than just a river, as it attracts thousands of tourists annually to the causeways through the gorge. [4] A little past Meiringen, near Brienz, the river expands into ...
Rivers of Japan are characterized by their relatively short lengths and considerably steep gradients due to the narrow and mountainous topography of the country. An often-cited quote is 'this is not a river, but a waterfall' by the Dutch engineer (o-yatoi gaikokujin) Johannis de Rijke who had visited the Jōganji River, Toyama Prefecture.
A. Abashiri River; Abe River; Abukuma River; Agano River; Agatsuma River; Agi River; Ai River (Gifu) Aibiki River; Aikawa River (Miyagi, Japan) Aka River; Akan River
This is the pronunciation key for IPA transcriptions of Japanese on Wikipedia. It provides a set of symbols to represent the pronunciation of Japanese in Wikipedia articles, and example words that illustrate the sounds that correspond to them.
The Unteraargletscher (German: [ˈʊntəraːrˌglɛtʃər]), literally "Lower Aare-Glacier", is the larger of the two sources of the Aare river in the Bernese Alps.It emerges from the association of the Finsteraargletscher (near the Finsteraarhorn) and the Lauteraargletscher (near the Lauteraarhorn) and flows for about 6 km (3.7 mi) to the east down to the Grimselsee near the Grimsel Pass.
The river Suhre is a 34 kilometer long tributary of the river Aare in the Swiss cantons of Lucerne and Aargau.The river rises in Sempachersee (or Lake Sempach) at an elevation of 504 meters above sea level, and joins the Aare east of the town Aarau at an elevation of 362 meters.
The Aare Gorge (German: Aareschlucht) is a section of the river Aare that carves through a limestone ridge near the town of Meiringen, in the Bernese Oberland region of Switzerland. [1] The gorge is an indirect product of glaciation ; 10,000 years ago, just as the Ice Age was coming to an end, torrential runoff water from melting glaciers ...
In Japanese this accent is called 尾高型 odakagata ("tail-high"). If the word does not have an accent, the pitch rises from a low starting point on the first mora or two, and then levels out in the middle of the speaker's range, without ever reaching the high tone of an accented mora. In Japanese this accent is named "flat" (平板式 ...