Webiga Loa
Wabiga Loa (Isbaanish: Río Loa) waa webi ku yaal waqooyiga gobolka Antofagasta ee dalka Chile. Dhererka webigu waa 440 km (270 mi), waa webiga ugu dheer dalka iyo marin biyoodka ugu muhiimsan saxaraha Atacama.
webiga loa | |
---|---|
Dalka | Jili |
Basin | |
Main source | Miño Volcano 4,277 m (14,032 ft) |
River mouth | Badweynta Baasifiga Heerka badda |
Basin size | 33,570 km2 (12,960 sq mi)[1] |
Physical characteristics | |
Length | 440 km (270 mi)[1] |
Discharge |
|
Features | |
Tributaries |
Koorso
wax ka badalIlaha Loa waxay ku yaalliin Andean dhaadhacyada buuraha ee ku yaal cagta Miño Volcano. Dooxada Loa ee sare waxa dhinaca galbeed kaga beegan lafo sare oo gaadhaysa ka sarraysa 4,500 m (14,800 ft), halka dhanka bari ay ku taalo silsilad foolkaane ah, taas oo ka soocda basinnada endorheic sida tan [ [Salar de Ascotán]].
Wabigu waxa uu ku socdaa koonfurta dhul sare, ilaa 150 km (90 mi), ilaa oasis ee Chiu Chiu. Koorasyada sare ee wabigu waxay ku yaalaan meel sare oo ka sarreysa heerka badda waxayna helayaan mug weyn oo biyo ah Andes, inta badan laba webi oo waaweyn: [[San Pedro de Inacaliri River] iyo Wabiga Salado . Kan hore waxa uu ku biiraa Loa oo u dhaw Conchi bakhaar kan dambena waxa uu ku saabsan yahay 3 km (1.9 mi) koonfurta Chiu Chiu. Biyaha koorsadooda sare iyo marinnada waa cusub yihiin. Si kastaba ha noqotee, koorsada hoose, sida dhammaan webiyada gobolkan waxay noqdaan kuwo jilicsan.
Laga soo bilaabo Chiu Chiu, Loa waxay u socotaa galbeedka iyo woqooyi iyada oo qalooc weyn u socota Quillagua. Ka dib markii uu u qulqulay 115 km (71 mi) qaybtan koorsadiisa oo uu dhex maray magaalada [[Calama, Chile | Calama], Loa wuxuu helayaa biyaha San Salvador River oo ku taal agagaarka "Chacance" Markaa wabigu wuxuu ku qulqulaa woqooyi ilaa Template:Beddel ilaa Quillagua.
Laga soo bilaabo Quillagua, kanaalkeeda engegan ayaa mar kale u leexda dhanka galbeed wuxuuna calaamadeeyaa soohdinta u dhaxaysa gobollada Tarapacá iyo Antofagasta. Inta ay socoto koorsada hoose, Loaku waxa uu maraa Template:Beddel canyon, kaas oo ka gudba Xeebaha Xeebta Chile. Wabigu waxa uu gaadhaa Badweynta Baasifiga lat. 21° 26' S., oo dhawr mayl koonfur ka xigta dekedii hore ee Huanillos.
Nidaamka biyo-raadinta ee dooxada webigu waa mid roobka u badan. Korodhka mugga biyuhu waxa uu dhacaa inta badan bilaha January iyo February, taas oo ka dhalatay ifafaalaha loo yaqaan Bolivian Winter.
Taariikhda
wax ka badalwaxa la deganaa tan iyo wakhtiyadii hore. Caddaynta tani waa tirada caanka ah ee geoglyph, petroglyph iyo sawirka ee laga helo kooraskeeda iyo basinkeeda sare.
Calaamad kale oo hodanteeda hore waa Pukará de Lasana.
xigasho
wax ka badal- ↑ 1.0 1.1 Lua error in Module:Lang at line 15: attempt to index field 'lang_name_table' (a nil value). Cuenca del río Loa
- Template:EB1911
- This article draws partially on the corresponding article in the Spanish-language Wikipedia, accessed July 10, 2007.