Genil

From Wikipedia, the free encyclopedia

Page Module:Infobox/styles.css has no content.

Genil
Lua error in package.lua at line 80: module 'Module:InfoboxImage/data' not found.
Genil flowing through the municipality of Fuente Vaqueros
Script error: No such module "Infobox mapframe".
Native nameTemplate:Native name checker
Location
CountrySpain
RegionAndalusia
CitiesGranada, Écija
Physical characteristics
Template:Infobox river/source
Template:Infobox river/source
Template:Infobox river/source
Template:Infobox river/source
Template:Infobox river/source
Template:Infobox river/source
MouthGuadalquivir
 • location
at Sanlúcar de Barameda
 • elevation
Template:Infobox river/calcunit
LengthTemplate:Infobox river/calcunit
Basin size
Template:Infobox river/calcunit
 • minimumTemplate:Infobox river/calcunit
 • averageTemplate:Infobox river/calcunit
 • maximumTemplate:Infobox river/calcunit
Template:Infobox river/discharge
Template:Infobox river/discharge
Template:Infobox river/discharge
Template:Infobox river/discharge
Template:Infobox river/discharge
Basin features
ProgressionTemplate:RGuadalquivir

Script error: No such module "Check for conflicting parameters".

The Genil River is the main (left) tributary of the river Guadalquivir in Andalusia, Spain. Known as Singilis in Latin, its modern name derives from the Moorish rendering of the Roman name: Sinyil, Sannil, and Sinnil.

Route

The source of the Genil is in the Sierra Nevada, north of its highest peak Mulhacén. The Genil flows through the towns Granada, Loja, Puente Genil and Écija. It flows into the Guadalquivir River near Palma del Río. Its main tributaries are the Darro in the Province of Granada and the Cabra River in the Province of Córdoba.

Geological history

The river today drains the Granada basin. In the latest Tortonian and the middle and late Turolian (9.0–5.3 Ma) this was an endorheic basin. Rivers flowed from the east and southwest into a central lake with no exit. During the Pliocene, the western part of the basin was drained by the paleo-Cacín river system, which flowed to the north and then left the basin to the west. The eastern part was drained by the Alhambra system, or paleo-Genil system, was fed by the mountains to the east and fed a small endorheic lake in the north. Some time later, the Genil river changed course to flow west, where it joined the paleo-Cacin system, and the basin became exorheic.[1]

See also

References

Page Template:Reflist/styles.css has no content.

  1. ^ Page Module:Citation/CS1/styles.css has no content.García Alix, Antonio; Minwer Barakat, Raef; Martín, José M.; Martín Suárez, Elvira; Freudenthal, Matthijs (July–August 2009), "Dating The Change From Endorheic To Exorheic Conditions In The Drainage System Of The Granada Basin (Southern Spain)", PALAIOS, 24 (7/8), SEPM Society for Sedimentary Geology: 544–549, Bibcode:2009Palai..24..544G, doi:10.2110/palo.2009.p09-015r, JSTOR 40606444

Lua error in package.lua at line 80: module 'Module:Authority control/config' not found.

Lua error: callParserFunction: function "#coordinates" was not found.


Template:Asbox