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Statements

Subject Item: dbr:Canadian_Cascade_Arc
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Subject Item: dbr:Cape_Breton_Island
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Subject Item: dbr:Carbajal_Valley
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Subject Item: dbr:Carrauntoohil
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Subject Item: dbr:Cary,_North_Carolina
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Subject Item: dbr:Cascade_Canyon
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Subject Item: dbr:Queets_River
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Subject Item: dbr:Rocky_Mountain_Trench
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Subject Item: dbr:Morphotectonics
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Subject Item: dbr:Bavarian_Alps
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Subject Item: dbr:Beatty_Creek_(Tahltan_River_tributary)
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Subject Item: dbr:Belknap_Crater
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Subject Item: dbr:Benbaun
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Subject Item: dbr:Benbrack
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Subject Item: dbr:Bencorr
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Subject Item: dbr:Bighorn_Mountains
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Subject Item: dbr:Black_Butte_(Oregon)
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Subject Item: dbr:Bormio
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Subject Item: dbr:Death_Canyon
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Subject Item: dbr:Derryclare
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Subject Item: dbr:Huascarán_National_Park
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Subject Item: dbr:List_of_hill_passes_of_the_Lake_District
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Subject Item: dbr:Little_Pamir
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Subject Item: dbr:Rila
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Subject Item: dbr:Upton,_Merseyside
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Subject Item: dbr:Val_d'Anniviers
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Subject Item: dbr:Valbonë_Valley_National_Park
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Subject Item: dbr:Valhalla_Canyon
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Subject Item: dbr:Colter_Canyon
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Subject Item: dbr:Coropuna
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Subject Item: dbr:County_Donegal
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Subject Item: dbr:Russvatnet
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Subject Item: dbr:Erosion
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Subject Item: dbr:Eskdale,_North_Yorkshire
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Subject Item: dbr:Geology_of_New_England
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Subject Item: dbr:Geology_of_the_Cairngorms_National_Park
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Subject Item: dbr:Old_Man_of_the_Mountain
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Subject Item: dbr:Rock_glacier
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Subject Item: dbr:Purcell_Trench
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Subject Item: dbr:Cliviger
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Subject Item: dbr:Cochamó_Valley
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Subject Item: dbr:Enipeus_Vallis
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Subject Item: dbr:Gap_of_Dunloe
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Subject Item: dbr:Geography_of_Albania
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Subject Item: dbr:Glacier_National_Park_(U.S.)
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Subject Item: dbr:Glen_Coe
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Subject Item: dbr:Glenmalure
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Subject Item: dbr:Gorleben
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Subject Item: dbr:Grand_Teton_National_Park
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Subject Item: dbr:Granite_Canyon
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Subject Item: dbr:Great_Langdale
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Subject Item: dbr:Mist_Trail
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Subject Item: dbr:Mount_Beulah
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Subject Item: dbr:Mount_Giluwe
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Subject Item: dbr:Mount_Shasta
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Subject Item: dbr:Mountains_of_the_Central_Dingle_Peninsula
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Subject Item: dbr:The_Volcano_(British_Columbia)
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Subject Item: dbr:Thingwall
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Subject Item: dbr:Subaqueous_fan
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Subject Item: dbr:Lechkhumi_Range
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Subject Item: dbr:Leigh_Canyon
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Subject Item: dbr:Leirdal
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Subject Item: dbr:Level_Mountain
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Subject Item: dbr:Los_Pelambres_mine
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Subject Item: dbr:Lugnaquilla
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Subject Item: dbr:MacGillycuddy's_Reeks
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Subject Item: dbr:Mangfall_Mountains
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Subject Item: dbr:Sitting_Bull_Mountain
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Subject Item: dbr:Slieve_Mish_Mountains
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Subject Item: dbr:Snowdonia
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Subject Item: dbr:Snowshoe_Canyon
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Subject Item: dbr:Stanwell-Fletcher_Lake
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Subject Item: dbr:Zealand_Notch
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Subject Item: dbr:Post-glacial_rebound
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Subject Item: dbr:Avalanche_Canyon
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Subject Item: dbr:Azas_Plateau
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Subject Item: dbr:Bad_Kleinkirchheim
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Subject Item: dbr:Banff_National_Park
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Subject Item: dbr:Brittain_River
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Subject Item: dbr:Bøvra
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Subject Item: dbr:Cautley_Spout
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Subject Item: dbr:Tokko_(river)
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Subject Item: dbr:Tronador
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Subject Item: dbr:Twelve_Bens
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Subject Item: dbr:Waterfalls_Canyon
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Subject Item: dbr:Waterton_Lakes_National_Park
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Subject Item: dbr:Webb_Canyon
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Subject Item: dbr:Weminuche_Wilderness
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Subject Item: dbr:West_Kill
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Subject Item: dbr:Wether_Hill_(Lake_District)
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Subject Item: dbr:Wicklow_Mountains
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Subject Item: dbr:Dlaboka_River
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Subject Item: dbr:Glacial_landform
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Subject Item: dbr:Glacial_stream
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Subject Item: dbr:Glacier
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Subject Item: dbr:Head_of_the_valley
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Subject Item: dbr:Jósepsdalur
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Subject Item: dbr:Kashubian_Lake_District
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Subject Item: dbr:Lamoille_Canyon
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Subject Item: dbr:Misfit_stream
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Subject Item: dbr:Abisko
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Subject Item: dbr:Acadia_National_Park
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Subject Item: dbr:Aeolis_Mensae
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Subject Item: dbr:Dudidontu_River
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Subject Item: dbr:Duror
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Subject Item: dbr:Earth
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Subject Item: dbr:Alpe_Veglia_and_Alpe_Devero_Natural_Park
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Subject Item: dbr:Feistritz_im_Rosental
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Subject Item: dbr:Fish_Creek_Falls
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Subject Item: dbr:Barnim_Plateau
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Subject Item: dbr:Broome_County,_New_York
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Subject Item: dbr:North_American_Cordillera
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Subject Item: dbr:North_Cascades
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Subject Item: dbr:Palatinate_Forest
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Subject Item: dbr:Fall_line
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Subject Item: dbr:Glossary_of_shapes_with_metaphorical_names
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Subject Item: dbr:Hinterriß
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Subject Item: dbr:Water_on_Mars
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Subject Item: dbr:List_of_National_Natural_Landmarks_in_New_Hampshire
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Subject Item: dbr:Hanging_Canyon
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Subject Item: dbr:Heidal
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Subject Item: dbr:Herschweiler-Pettersheim
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Subject Item: dbr:High_Desert_Discovery_Scenic_Byway
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Subject Item: dbr:Irby,_Merseyside
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Subject Item: dbr:Jacques-Cartier_National_Park
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Subject Item: dbr:Vale_of_Ewyas
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Subject Item: dbr:Arve_Valley
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Subject Item: dbr:Ablation_Point_–_Ganymede_Heights_Antarctic_Specially_Protected_Area
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Subject Item: dbr:Abrasion_(geology)
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Subject Item: dbr:Achaidh_Leithdeircc
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Subject Item: dbr:Chachani
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Subject Item: dbr:Jim_Savage
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Subject Item: dbr:Lake_Hāwea
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Subject Item: dbr:Lake_Wānaka
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Subject Item: dbr:Lapporten
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Subject Item: dbr:Blodgett_Canyon
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Subject Item: dbr:Sultan_River
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Subject Item: dbr:High_Cup_Gill
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Subject Item: dbr:Highline_Trail_(Glacier_National_Park)
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Subject Item: dbr:Raydale
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Subject Item: dbr:Arête
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Subject Item: dbr:Mansfield_Creek
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Subject Item: dbr:Pirin
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Subject Item: dbr:Plummer_Mountain
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Subject Item: dbr:Sperry_Chalet
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Subject Item: dbr:Groundwater_sapping
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Subject Item: dbr:New_Brunswick
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Subject Item: dbr:Ojos_del_Salado
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Subject Item: dbr:Open_Canyon
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Subject Item: dbr:Cathedral_Group
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Subject Item: dbr:Rackwick
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Subject Item: dbr:Recknitz
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Subject Item: dbr:Channeled_Scablands
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Subject Item: dbr:Shebenik-Jabllanicë_National_Park
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Subject Item: dbr:Wānaka
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Subject Item: dbr:Yihun_Lhatso
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Subject Item: dbr:Yosemite_Valley
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Subject Item: dbr:Topographical_relief_of_Spain
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Subject Item: dbr:Stanford_torus
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Subject Item: dbr:U-shaped_valley
rdf:type: yago:Thing100002452 yago:WikicatFjords yago:WikicatValleys yago:NaturalElevation109366317 yago:Object100002684 yago:NaturalDepression109366017 yago:PhysicalEntity100001930 yago:Fjord109281104 yago:BodyOfWater109225146 yago:GeologicalFormation109287968 yago:WikicatMountains yago:Inlet109313716 yago:YagoPermanentlyLocatedEntity yago:YagoGeoEntity yago:Mountain109359803 yago:Valley109468604
rdfs:label: Trogdal Vall glacial Trogtal Трог U-shaped valley Трог (геологія) 빙하곡 Vale glaciar U字谷 Vallée glaciaire Trog U型山谷 Glaziar haran U-dal Valle glaciar Dolina U-kształtna
rdfs:comment: Une vallée glaciaire, vallée en auge ou vallée en U est un type de vallée caractéristique des régions de montagnes qui ont été affectées par une glaciation régionale. Elles résultent du travail d’écoulement en bloc des glaciers, emplissant tout le fond de la vallée et l’érodant par surcreusement. Les vallées glaciaires se définissent par leur profil transversal (plus précisément parabolique), mais surtout par profil longitudinal fait d'une succession de paliers et de ressauts. Dans la plupart des cas, les vallées glaciaires correspondent à des héritages des glaciations pléistocènes où de puissants icestreams (courants de glace) en provenance des hauts massifs ont utilisé ces axes préexistants pour se diriger vers les piémonts. Ils se sont souvent réunis dans de très grandes vallées longitu Un valle glaciar, también llamado artesa glaciar, se define como aquel valle por el que circula o ha circulado un glaciar de dimensiones importantes que ha dejado una geomorfología clara de glaciarismo. Los valles glaciares son ríos de hielo. Se forman cuando el espesor del hielo acumulado en el circo es grande. El hielo de las capas inferiores se desplaza fuera del circo y se derrama valle abajo. Los fragmentos rocosos que contienen hielo ensanchan el valle. También excavan cubetas en las zonas de roquedo menos resistente. Estas cubetas, al fundirse el hielo, se convierten en lagos. Trog neboli ledovcové údolí je zvláštním případem údolí s typickým tvarem písmene U, které vzniká působením erozivní činnosti postupujícího ledovce. Трог (від нім. Trog — «корито») — річкова долина з коритоподібним поперечним профілем, що утворилася в результаті проходження льодовика. Vale glaciário, vale glaciar ou vale em U é o termo empregue para definir um vale de origem glaciar, encontrado nas regiões de montanha resultantes do trabalho de erosão de um glaciar que anteriormente ocupava o vale atual. A sua forma característica está na origem de ser chamado vale em U Een trogdal of U-dal is een daltype. Het heeft een U-vorm en een platte bodem met aan beide zijden steile wanden. Een U-dal ontstaat doordat er een rivier of een gletsjer de bodem erodeert. Normaal is er sprake van een verticale en een horizontale erosie, hierdoor ontstaat een V-dal. Bij een trogdal is echter het gesteente op de bodem te hard waardoor de verticale erosie nauwelijks nog plaatsvindt. De horizontale erosie gaat echter wel gewoon door. Zo ontstaat de U-vorm. Ook kan een U-dal ontstaan doordat een gletsjer grote stukken land meeneemt/afschuurt. 冰川谷（又称U形谷、冰川槽谷）是冰川侵蚀作用形成的谷地。它的山谷陡峭，谷底平缓，横剖面呈抛物线形，类似字母U。当冰川顺着倾斜的山坡向下移动，山谷就会被冲刷、侵蚀。等到冰川融化或解冻，就留下一个山谷，其中常常散落着被冰川运来的小石块。多山的地区常常有冰川谷。如在阿尔卑斯山、喜马拉雅山、洛矶山、苏格兰高地、斯堪的纳维亚半岛、新西兰和加拿大等。一个典型的冰川谷是的流经，位于美国蒙大拿州的冰河国家公园的冰川谷。 U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Dolina U-kształtna, dolina lodowcowa, rynna polodowcowa, dolina rynnowa, żłób lodowcowy – dolina powstała w wyniku przekształcenia doliny V-kształtnej przez lodowiec górski. Profil takiej doliny przypomina literę U: charakteryzuje się ona stromymi ścianami skalnymi i stosunkowo płaskim dnem, zwykle wypełnionym osadami morenowymi lub pochodzącymi ze stoków (stożki piargowe, aluwialne i koluwia osuwiskowe). Ma ona przebieg bardziej prostoliniowy niż dolina, z której została uformowana. Dodatkowo, w przeciwieństwie do dolin rzecznych, rynna polodowcowa może mieć niewyrównany profil podłużny, a jej przegłębione dno może sięgać poniżej poziomu morza (skalne dna dolin alpejskich, Sognefjorden w Norwegii). Jest to element charakterystyczny dla obszarów wysokogórskich, które są lub były w przeszło Трог, троговая долина (от нем. Trog — «корыто») — долина в ледниковой или древнеледниковой области с корытообразным (U-образным) поперечным профилем, ш��роким дном и крутыми вогнутыми бортами, которые связаны с выпахивающей деятельностью ледников. Борта типичных троговых долин вверху переходят в более пологие обработанные льдом участки, называемые плечами трогов. У некоторых трогов бывает не одна, а две или три пары плеч. Такие вложенные троги часто объясняют тем, что более молодые долины врезаны в днища более древних. Glaziar harana glaziarren higaduraren eraginez U itxura hartu duen harana da. Izotzak egindako haran hauek oso ohikoak dira Alpeetan, Himalaian, Mendi Harritsuetan, Eskoziako Lur Garaietan, Eskandinavian edo Kanadan. Haranaren barrenean glaziarraren urtutako urak sortutako ibai bat izan daiteke. Ein Trogtal oder U-Tal ist eine große Talform stark reliefierter, durch Gletscher überformter Gebirge. Sie ist gekennzeichnet durch ein im unteren Bereich typisches U-förmiges Querprofil. Un vall glacial, es defineix com aquella vall per la qual hi circula o ha circulat una glacera de dimensions importants que ha deixat una geomorfologia clara de glacialisme. Una vall glacial és una forma de relleu característica de les regions de muntanyes afectades per una glaciació regional. Les valls glacials es defineixen pel seu perfil transversal, però sobretot pel seu perfil longitudinal. En la seva major part les valls glacials es van fer en el període del Plistocè. U字谷（ユーじこく、ユーじだに）とは、氷河の侵食によって地表がU字状に削り取られて生じた侵食谷のことである。氷食谷ともいう。アルプス山脈やロッキー山脈、ヒマラヤ山脈などの山岳地帯に多く存在する。日本では立山周辺などで観察される。なお、U字谷に海水が流入して生じた細長い湾のことをフィヨルドという。また、U字谷に淡水がたまってできた湖を氷河湖という。 U-dal, eller trågdal, är en bred dalgång med jämn botten och där dalens tvärsnitt påminner om bokstaven U. U-dalar bildas av glaciärer som vidgar befintliga V-dalar eller när flera glaciärer tar sig nedför bergssluttningar. När glaciären smälter lämnar den, på botten av U-dalen, alla de stenar och det grus den tidigare plockat upp och transporterat inom sig. Inte sällan har U-dalar olika branta sidor, då erosionen har skett osymmetriskt eller då olika bergarter på sidorna kan vara olika motståndskraftiga. * U-formad dal i , Ladakh i nordvästra indiska Himalaya * Lapporten, Sverige * * 빙하곡(氷河谷)은 빙하의 침식에 의해서 지표가 U자 모양으로 깎여서 형성된 이다. 빙식곡(氷蝕谷) 또는 유자곡(U字谷)이라고도 한다. 또 이것에 해수가 유입해 생긴 좁고 긴 만을 피오르라고 한다. 알프스 산맥이나 로키 산맥, 히말라야 산맥 등의 산악 지대에 많이 존재한다.
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dbo:abstract: Трог, троговая долина (от нем. Trog — «корыто») — долина в ледниковой или древнеледниковой области с корытообразным (U-образным) поперечным профилем, широким дном и крутыми вогнутыми бортами, которые связаны с выпахивающей деятельностью ледников. Борта типичных троговых долин вверху переходят в более пологие обработанные льдом участки, называемые плечами трогов. У некоторых трогов бывает не одна, а две или три пары плеч. Такие вложенные троги часто объясняют тем, что более молодые долины врезаны в днища более древних. В продольном профиле троговые долины обычно имеют ступенчатую форму, где чередуются переуглубленные участки (бассейны выпахивания) с приподнятыми скалистыми ступенями (ригелями). Бассейны часто заполнены озёрами или речными отложениями, а ригели чаще всего обнажены, покрыты бараньими лбами и изборождены ледниковыми шрамами и штриховкой. Отличительной чертой троговых долин служат висячие долины-притоки. Их днище лежит выше, нередко на 150—200 м и более, чем дно основной троговой долины, и отделяется от него устьевой ступенью. Это объясняется тем, что ледник, заполнявший основную долину, врезался заметно сильнее, чем его более мелкий приток. Наиболее крупные троги могут достигать в длину нескольких десятков, иногда сотен километров. Троги широко распространены во всех горно-ледниковых районах суши. Там, где ледники достигали или достигают уровня моря, троговые долины продолжаются в виде фьордов. Un valle glaciar, también llamado artesa glaciar, se define como aquel valle por el que circula o ha circulado un glaciar de dimensiones importantes que ha dejado una geomorfología clara de glaciarismo. Los valles glaciares son ríos de hielo. Se forman cuando el espesor del hielo acumulado en el circo es grande. El hielo de las capas inferiores se desplaza fuera del circo y se derrama valle abajo. Los fragmentos rocosos que contienen hielo ensanchan el valle. También excavan cubetas en las zonas de roquedo menos resistente. Estas cubetas, al fundirse el hielo, se convierten en lagos. Dolina U-kształtna, dolina lodowcowa, rynna polodowcowa, dolina rynnowa, żłób lodowcowy – dolina powstała w wyniku przekształcenia doliny V-kształtnej przez lodowiec górski. Profil takiej doliny przypomina literę U: charakteryzuje się ona stromymi ścianami skalnymi i stosunkowo płaskim dnem, zwykle wypełnionym osadami morenowymi lub pochodzącymi ze stoków (stożki piargowe, aluwialne i koluwia osuwiskowe). Ma ona przebieg bardziej prostoliniowy niż dolina, z której została uformowana. Dodatkowo, w przeciwieństwie do dolin rzecznych, rynna polodowcowa może mieć niewyrównany profil podłużny, a jej przegłębione dno może sięgać poniżej poziomu morza (skalne dna dolin alpejskich, Sognefjorden w Norwegii). Jest to element charakterystyczny dla obszarów wysokogórskich, które są lub były w przeszłości zlodowacone. Doliny lodowcowe formowane są przez lodowce górskie (Alpy, Tatry) lub strumienie lodu na obrzeżach lądolodów i czap lodowych (Grenlandia, Skandynawia). W Polsce przykładem są doliny tatrzańskie, na przykład Dolina Roztoki. Specyficznym przypadkiem doliny U-kształtnej jest fierd. Een trogdal of U-dal is een daltype. Het heeft een U-vorm en een platte bodem met aan beide zijden steile wanden. Een U-dal ontstaat doordat er een rivier of een gletsjer de bodem erodeert. Normaal is er sprake van een verticale en een horizontale erosie, hierdoor ontstaat een V-dal. Bij een trogdal is echter het gesteente op de bodem te hard waardoor de verticale erosie nauwelijks nog plaatsvindt. De horizontale erosie gaat echter wel gewoon door. Zo ontstaat de U-vorm. Ook kan een U-dal ontstaan doordat een gletsjer grote stukken land meeneemt/afschuurt. Wanneer een trogdal gedeeltelijk opgevuld wordt door zeewater wordt het een fjord genoemd. Трог (від нім. Trog — «корито») — річкова долина з коритоподібним поперечним профілем, що утворилася в результаті проходження льодовика. Une vallée glaciaire, vallée en auge ou vallée en U est un type de vallée caractéristique des régions de montagnes qui ont été affectées par une glaciation régionale. Elles résultent du travail d’écoulement en bloc des glaciers, emplissant tout le fond de la vallée et l’érodant par surcreusement. Les vallées glaciaires se définissent par leur profil transversal (plus précisément parabolique), mais surtout par profil longitudinal fait d'une succession de paliers et de ressauts. Dans la plupart des cas, les vallées glaciaires correspondent à des héritages des glaciations pléistocènes où de puissants icestreams (courants de glace) en provenance des hauts massifs ont utilisé ces axes préexistants pour se diriger vers les piémonts. Ils se sont souvent réunis dans de très grandes vallées longitudinales comme les vallées de l’Isère, du haut Rhône, du haut Rhin, de l’Inn, de l’Enns, de la Drave, où se concentrait la glace. Comme l’ont souligné P. & G. Veyret (1967), c’est cette exceptionnelle puissance de transport et de réaménagement qui a permis l’élargissement, le creusement et le surcreusement de ces vallées et qui confèrent aux vallées alpines une « surprenante maturité » par rapport à l’extrême jeunesse du massif. Ein Trogtal oder U-Tal ist eine große Talform stark reliefierter, durch Gletscher überformter Gebirge. Sie ist gekennzeichnet durch ein im unteren Bereich typisches U-förmiges Querprofil. U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, and the Scottish Highlands. A classic glacial trough is in Glacier National Park in Montana, USA in which the St. Mary River runs. Another well-known U-shaped valley is the Nant Ffrancon valley in Snowdonia, Wales. When a U-shaped valley extends into saltwater, becoming an inlet of the sea, it is called a fjord, from the Norwegian word for these features that are common in Norway. Outside of Norway, a classic U-shaped valley that is also a fjord is the Western Brook Pond Fjord in Gros Morne National Park in Newfoundland, Canada. U字谷（ユーじこく、ユーじだに）とは、氷河の侵食によって地表がU字状に削り取られて生じた侵食谷のことである。氷食谷ともいう。アルプス山脈やロッキー山脈、ヒマラヤ山脈などの山岳地帯に多く存在する。日本では立山周辺などで観察される。なお、U字谷に海水が流入して生じた細長い湾のことをフィヨルドという。また、U字谷に淡水がたまってできた湖を氷河湖という。 빙하곡(氷河谷)은 빙하의 침식에 의해서 지표가 U자 모양으로 깎여서 형성된 이다. 빙식곡(氷蝕谷) 또는 유자곡(U字谷)이라고도 한다. 또 이것에 해수가 유입해 생긴 좁고 긴 만을 피오르라고 한다. 알프스 산맥이나 로키 산맥, 히말라야 산맥 등의 산악 지대에 많이 존재한다. U-dal, eller trågdal, är en bred dalgång med jämn botten och där dalens tvärsnitt påminner om bokstaven U. U-dalar bildas av glaciärer som vidgar befintliga V-dalar eller när flera glaciärer tar sig nedför bergssluttningar. När glaciären smälter lämnar den, på botten av U-dalen, alla de stenar och det grus den tidigare plockat upp och transporterat inom sig. Inte sällan har U-dalar olika branta sidor, då erosionen har skett osymmetriskt eller då olika bergarter på sidorna kan vara olika motståndskraftiga. Exempel på U-dalar finns i bergsområden som Alperna, Himalaya, Anderna, Klippiga bergen, skotska högländerna och i länder som Sverige, Norge, Nya Zeeland och Kanada. I Sverige är Lapporten vid Abisko berömd. * U-formad dal i , Ladakh i nordvästra indiska Himalaya * Lapporten, Sverige * Høyanger, Norge * Alggavagge, Sverige, Sareks nationalpark Vale glaciário, vale glaciar ou vale em U é o termo empregue para definir um vale de origem glaciar, encontrado nas regiões de montanha resultantes do trabalho de erosão de um glaciar que anteriormente ocupava o vale atual. A sua forma característica está na origem de ser chamado vale em U Trog neboli ledovcové údolí je zvláštním případem údolí s typickým tvarem písmene U, které vzniká působením erozivní činnosti postupujícího ledovce. 冰川谷（又称U形谷、冰川槽谷）是冰川侵蚀作用形成的谷地。它的山谷陡峭，谷底平缓，横剖面呈抛物线形，类似字母U。当冰川顺着倾斜的山坡向下移动，山谷就会被冲刷、侵蚀。等到冰川融化或解冻，就留下一个山谷，其中常常散落着被冰川运来的小石块。多山的地区常常有冰川谷。如在阿尔卑斯山、喜马拉雅山、洛矶山、苏格兰高地、斯堪的纳维亚半岛、新西兰和加拿大等。一个典型的冰川谷是的流经，位于美国蒙大拿州的冰河国家公园的冰川谷。 Un vall glacial, es defineix com aquella vall per la qual hi circula o ha circulat una glacera de dimensions importants que ha deixat una geomorfologia clara de glacialisme. Una vall glacial és una forma de relleu característica de les regions de muntanyes afectades per una glaciació regional. Les valls glacials es defineixen pel seu perfil transversal, però sobretot pel seu perfil longitudinal. En la seva major part les valls glacials es van fer en el període del Plistocè. Glaziar harana glaziarren higaduraren eraginez U itxura hartu duen harana da. Izotzak egindako haran hauek oso ohikoak dira Alpeetan, Himalaian, Mendi Harritsuetan, Eskoziako Lur Garaietan, Eskandinavian edo Kanadan. Haranaren barrenean glaziarraren urtutako urak sortutako ibai bat izan daiteke.
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