Tamigi

El Tamigi (in inglexe Thames, dal łatin Tamesis) el xe on fiume de ł'Inghiltera meridionałe che traversa Łondra e finise 'ntel Mare del Nord: ancorché no 'l sia el major par longhesa e portada, el xe da considerar de gran łonga el primo par inportansa storega e economica. El so bacin idrografego el xe abità da sirca 15 miłioni de persone.

Ła łonghezsa del fiume ła xe ojeto de ciàcołe parché se a xe bastansa ciaro dove che el scuminsia (ma anca inte sto caxo a ghe xe difarenti interpretasion), a no a xe asołutamente serto fin a dove el vaga considerà el corso del fiume in quanto eò va drento, co on profondo estuario, 'ntel Mar del Nord e ałora a se ga da considerar 'na łonghezsa convensional: siché a se distingue 'na prima łonghezsa de 272 Km fra Thames Head (ła sorgente convensional) e el London Bridge (scuminsio del Porto de Łondra); 'na seconda łonghezsa de 323 Km fin al banco de Nore (dove, in corispondenzsa del faro, a finise el grande Porto de Łondra che el ga oo sviłupo de 88 Km) indove ł'estuario el xe łargo 16 Km; 'na tersa łonghezsa de 365 Km ała foce deła Medway, visin Sheerness, che, pertanto, secondo alcuni Autori el sarìa da considerar on fiume con on proprio sboco al mar, secondo altri, el sarìa ł'ultimo afluente del Tamigi.

Contrariamente a queło ca se pol crèdare łe so portade mexe łe xe modeste (ancorché pitosto regołari, mancando grandi seche e grandi piene) e no łe supera, in xenare, el xentenaro de metri cubi al secondo a ła foce, ma ciò che ło fa parecio inportante ła xe ła łarghezsa de ł'estuario e el fato che ła marea ła va su ben oltre el sentro de Londra, faxendoło navigabiłe in ogni stajon: a Teddington, inte ł'area metropołitana osidental łondinese (a 6 m./s.l.m., indove a finise el corso fluvial vero e proprio parché pì su a non se risente pì ła marea), infati ła portada minima de settmbre ła xe de 28 mc/sec, mentre queła masima de xenaro ła xe de 129 mc/sec, ma al London Bridge, el fiume, co ł'alta marea, el xe profondo 9 m e el xe łargo 240 m, e questo a ło fa comodamente navigabiłe da grosi batełi.

Łe sorgenti łe se cata visin al viłajo de Kemble intel Gloucestershire inte ła cadena cołinare dełe Cotswold Hills, dove 'na serie de ruscełi (convensionalmente sete - The Seven Wells -) i sgorga da tereni permeabiłi formando el Churu, considerado come ramo sorgentizsio; ma altri i considera ła vera sorgente a Thames Head (Testa del Tamiji), 5 Km a est de Cirincester. I prinsipałi afluenti i xe Windrush, Evenlode, Cherwell, Thame, Kennet, Colne, Wey, Mole, tuti pitosto regołari come regime idraułico.

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