An sabunta ta ƙarshe ranar 2 ga Satumba, 2022 ta Roger Kaufman
ban mamakir waterfall a kan Rhine
Bayani a kan Rhine Falls:
- Faɗin mita 150
- Tsayin mita 25
- zurfin mita 13
- 14000 - 17000 shekaru duk abin da
- 600 cubic meters na ruwa a sakan daya
Tarin bidiyo na ruwan ruwa na Rhine kusa da Schaffhausen
Ruwan ruwa mafi girma a Turai - Ruwan Rhine
A cikinsa duka akwai wani katon dutse wanda ya tsaya tsayin daka a kan abubuwan da aka gyara tsawon shekaru dubu.
Ana iya isa dutsen a kan tafiye-tafiye da ke kan rafin Rhine, inda za ku iya lura da al'amuran halitta kusa.
A zahiri a tsakiyar rafin Rhine, baƙi suna dogara kan dandamali waɗanda ke fitowa da wani bangare. yana iyo sama da Rhine.
Gine-gine na Wörth da Laufen ana iya isa su ta jirgin ruwa, kuma musamman m Baƙi na iya hayan kwalekwale.
Saboda sauye-sauyen tectonic a cikin Ice Age, an tura Rhine zuwa sabon kogin sama da shekaru 15.000 da suka wuce.
Ruwan Rhine ya kasance a wurin sauyawa inda alli mai wuya ya zama tsakuwa mai laushi.
Daruruwan mita cubic suna gudana a kan fadin mita 150 ruwa a gudun mita 23 a sakan daya.
Babban sama da mafi girma na Turai ruwan sama don tsayawa da jin ruri da girgizar ruwa a ko'ina cikin jikin ku - za ku iya fuskantar hakan a rafin Rhine kusa da Schaffhausen.
Tare da jirgin za ku iya ganin kaskoki, da ruwa na Rhine har ma da manyan duwatsu a tsakiyar tsakiyar. waterfall isa.
Ƙungiyar Schloss Laufen a haƙiƙa tana da haske tun Maris 2010.
Baya ga sabuwar cibiyar baƙo, an kuma buɗe filin wasan yara da "Historama".
Sabuwar hanyar kasada tare da tsarin ɗagawa sau biyu da hanyar kallo yana ba da sauƙi zuwa ga rafin Rhine mai ban sha'awa.
Kyawawan hotuna na ruwan ruwa na Rhine
Rhine Falls - Switzerland 4K
Ku kasance da mu mafi girma waterfall a Turai, jin hayaniya da girgizar ruwa a duk jikin ku - ana iya samun wannan a Rhine Falls kusa da Schaffhausen. Ta hanyar jirgin ruwa za ku iya zuwa katanga, kwarin ruwa na Rhine Falls da kuma manyan duwatsu a tsakiyar faɗuwar ruwa.
source: Panorama JL
Mafi kyawun ruwan ruwa a Switzerland - Rhine Falls
M Swiss German Rhyfall [ˈɾiːfal], FaransanciChutes du Rhin, Italiyanci Cascate del Reno, Romanci Cascada dal Rain), a baya ma Babban gudu ake kira (sabanin da gudu kadan), tare da daidai girman Sarpsfossen a Norway, yana ɗaya daga cikin manyan magudanan ruwa uku a Turai.
Tare da matsakaita na 577 m³/s, Sarpsfossen yana da ƙarin ruwa, yayin da babban Dettifoss sau biyu akan Iceland kawai yana da kusan rabin yawan ruwa.
Ruwan ruwa na Rhine yana cikin ƙasar Switzerland a yankin ƙananan hukumomi Neuhausen a Rhine Falls a yankin Schaffhausen (a bankin dama) da Laufen-Uhwiesen da ke yankin Zurich (a bankin hagu), kusan kilomita hudu yamma da birnin Schaffhausen.
Akan hanya daga Bodensee bayan Basel ta fuskanci high rhine ninka duwatsu masu juriya a cikin hanyar, waɗanda ke kunkuntar gadon kogin kuma wanda kogin ya yi nasara a cikin rapids da magudanar ruwa, Rhine Falls.
Ruwan Rhine yana da tsayin mita 23 da faɗin mita 150. Daga cikin zagi a cikin yankin tasiri yana da zurfin mita 13. A tsakiya ruwa373 cubic meters na ruwa a cikin dakika daya faɗuwar kan duwatsun da ke cikin rafin Rhine (matsakaicin fitarwa na bazara: kusan 600 m³/s).
An auna mafi girman yawan kwararar ruwa a cikin 1965 tare da mita 1250 cubic, mafi ƙanƙanci a cikin 1921 tare da mita cubic 95 a sakan daya.
Hakanan a cikin shekarun 1880, 1913 da 1953 fitarwar ta kasance kadan.
Kifaye ba zai iya hawan rafin Rhine zuwa sama ba, sai ta ulu.[1] Wannan yana nufin a gefe (a wajen gadon kogin a cikin karkara) sama da duwatsu.
Fitowa
Gidan gadon, wanda ya girme shi da Rhine Falls kanta, da kuma mahimman hanyoyin tafiyar da yanayin ƙasa a halin yanzu. shekarun kankara ya kai ga samuwar rafin Rhine.
Ci gaban glacial na farko ya fara kusan shekaru 500 da suka gabata sakamakon raguwar yanayin zafi gabaɗaya. Mittelland da siffata yanayin yanayin yau.
Har zuwa karshen fasa shekarun kankara Kimanin shekaru 200 da suka wuce Rhine ya malalo yamma daga Schaffhausen ta cikin Klettgau.
Wannan tsohon gadon kogin an sake rufe shi da tsakuwa mai tsayi (molasses) cika.
Kusan shekaru 120 da suka gabata, an karkatar da kogin kudu kusa da Schaffhausen kuma ya kafa tashar Rhine na zamanin Rift.
Hanyar Rhine da ke ƙasa da kwandon ruwa heute yayi daidai da wannan tashar, wadda aka sake cika da tsakuwa.
A lokacin lokacin ƙanƙara na ƙarshe, wanda ake kira Würm Ice Age, Rhine an tura shi zuwa kudu a cikin baka mai faɗi kuma ya isa gadonsa na yanzu akan Malmkalk mai wuya (Weissjura, Oberer Jura) sama da faɗuwar.
Ruwan Rhine a cikin nau'in su na yanzu an kafa shi ne kimanin shekaru 14 zuwa 000 da suka wuce a lokacin sauye-sauye daga babban dutsen Malm zuwa tashar tsakuwa mai sauƙin cirewa daga lokacin fashewa.
Rheinfallfelsen (babba, dutse mai hawa da kuma, bisa ga almara, dutsen rawa na rai) ya zama ragowar asalin dutsen farar ƙasa na tsohon tashar magudanar ruwa.
Za'a iya bayyana ƙarancin juzu'in juzu'i na ɓangaren faɗuwar har zuwa yanzu ta hanyar ƙarancin ja (nauyin gadon kogin) na Rhine a ƙarƙashin Lake Constance.
source: wikipedia
