. . . "UT-30-B"@en . . . "ut0382"@en . "UT-30-I"@en . "1"^^ . . "2"^^ . . . . "Highline Canal"@en . "ut0373"@en . . "Rhodes Canal"@en . . . . . "UT-30"@en . . . . . "UT-30-H"@en . "Bacino Uinta"@it . . . "40.22499847412109"^^ . . . "ut0380"@en . "ut0185"@en . . . . . . "10156479"^^ . "POINT(-109.54222106934 40.224998474121)"^^ . . . . . . "4"^^ . . . . . "The Uinta Basin (also known as the Uintah Basin) is a physiographic section of the larger Colorado Plateaus province, which in turn is part of the larger Intermontane Plateaus physiographic division. It is also a geologic structural basin in eastern Utah, east of the Wasatch Mountains and south of the Uinta Mountains. The Uinta Basin is fed by creeks and rivers flowing south from the Uinta Mountains. Many of the principal rivers (Strawberry River, Currant Creek, Rock Creek, Lake Fork River, and Uintah River) flow into the Duchesne River which feeds the Green River\u2014a tributary of the Colorado River. The Uinta Mountains forms the northern border of the Uinta Basin. They contain the highest point in Utah, Kings Peak, with a summit 13,528 feet (4123 metres) above sea level. The climate of the "@en . "UT-30-F"@en . . . . . . . . . . . . . . "Wissiup Homestead"@en . . . . "ut0378"@en . "Whiterocks and Ouray Valley Canal"@en . . . "The Uinta Basin (also known as the Uintah Basin) is a physiographic section of the larger Colorado Plateaus province, which in turn is part of the larger Intermontane Plateaus physiographic division. It is also a geologic structural basin in eastern Utah, east of the Wasatch Mountains and south of the Uinta Mountains. The Uinta Basin is fed by creeks and rivers flowing south from the Uinta Mountains. Many of the principal rivers (Strawberry River, Currant Creek, Rock Creek, Lake Fork River, and Uintah River) flow into the Duchesne River which feeds the Green River\u2014a tributary of the Colorado River. The Uinta Mountains forms the northern border of the Uinta Basin. They contain the highest point in Utah, Kings Peak, with a summit 13,528 feet (4123 metres) above sea level. The climate of the Uinta Basin is semi-arid, with occasionally severe winter cold."@en . . . . . . "Uinta Basin"@en . "ut0381"@en . . "Rocky Point Canal"@en . "UT-30-C"@en . . "UT-30-J"@en . . . . "U.S. Whiterocks Canal"@en . "1115509969"^^ . "P\u00E1nev Uinta (anglicky Uinta Basin) je oblast v severn\u00ED \u010D\u00E1sti Koloradsk\u00E9 plo\u0161iny. Le\u017E\u00ED na v\u00FDchod\u011B Utahu, ve Spojen\u00FDch st\u00E1tech americk\u00FDch. Jedn\u00E1 se o asymetrickou struktur\u00E1ln\u00ED p\u00E1nev. Je nejn\u00ED\u017Ee polo\u017Een\u00FDm m\u00EDstem Koloradsk\u00E9 plo\u0161iny."@cs . . "ut0376"@en . . . "Deep Creek Canal"@en . . . . . . "Irrigation Canals in the Uinta Basin"@en . . . . "-109.5422210693359"^^ . "UT-30-A"@en . "40.225 -109.54222222222222" . . "108"^^ . . . "Il bacino Uinta, (scritto anche bacino Uintah) \u00E8 una sezione fisiografica della vasta provincia degli Altopiani del Colorado, la quale a sua volta fa parte della pi\u00F9 estesa divisione fisiografica degli , negli Stati Uniti d'America. Dal punto di vista geologico \u00E8 un bacino strutturale situato nella parte orientale dell'Utah, a est dei monti Wasatch e a sud dei monti Uinta. Il bacino Uinta \u00E8 alimentato da torrenti e fiumi che scorrono verso sud provenendo dai monti Uinta. Molti di questi corsi d'acqua (Strawberry River, Currant Creek, Rock Creek, Lake Fork River e Uinta River) confluiscono nel , il quale a sua volta va a gettarsi nel Green River che \u00E8 un tributario del fiume Colorado. Il confine nord del bacino \u00E8 segnato dai monti Uinta, dove si trova anche il Kings Peak che, con i suoi 4123 m.s.l.m, \u00E8 la cima pi\u00F9 elevata dell'Utah. Il clima del bacino \u00E8 semiarido, con occasionali inverni rigidi."@it . . . . "ut0379"@en . . . . . . . "ut0374"@en . . "Jepp Thomas Canal"@en . "2"^^ . . "3"^^ . . . . . . . . "UT-30-G"@en . . . . . . . . . "ut0377"@en . . "Knight Ditch"@en . "ut0372"@en . . "P\u00E1nev Uinta (anglicky Uinta Basin) je oblast v severn\u00ED \u010D\u00E1sti Koloradsk\u00E9 plo\u0161iny. Le\u017E\u00ED na v\u00FDchod\u011B Utahu, ve Spojen\u00FDch st\u00E1tech americk\u00FDch. Jedn\u00E1 se o asymetrickou struktur\u00E1ln\u00ED p\u00E1nev. Je nejn\u00ED\u017Ee polo\u017Een\u00FDm m\u00EDstem Koloradsk\u00E9 plo\u0161iny."@cs . "19"^^ . . . . . . . "Ouray Park Canal"@en . . . "8"^^ . . . "UT-30-E"@en . . . "12"^^ . . "13"^^ . "2"^^ . . . . "UT-30-D"@en . . "1"^^ . "6"^^ . "7"^^ . . "UT-30-K"@en . "5"^^ . . . . . "P\u00E1nev Uinta"@cs . . "U.S. Lake Fork Canal"@en . "ut0375"@en . . . . . . . . . . "Il bacino Uinta, (scritto anche bacino Uintah) \u00E8 una sezione fisiografica della vasta provincia degli Altopiani del Colorado, la quale a sua volta fa parte della pi\u00F9 estesa divisione fisiografica degli , negli Stati Uniti d'America. Dal punto di vista geologico \u00E8 un bacino strutturale situato nella parte orientale dell'Utah, a est dei monti Wasatch e a sud dei monti Uinta. Il confine nord del bacino \u00E8 segnato dai monti Uinta, dove si trova anche il Kings Peak che, con i suoi 4123 m.s.l.m, \u00E8 la cima pi\u00F9 elevata dell'Utah. Il clima del bacino \u00E8 semiarido, con occasionali inverni rigidi."@it . . . . . . "11759"^^ .