Venustiano Carranza, Mexico Ceety

Venustiano Carranza
Venustiano Carranza athin the Federal Destrict
Venustiano Carranza athin the Federal Destrict
Kintra Mexico
Federal entity D.F.
Established 1970
Named for Venustiano Carranza
Seat Colonia Jardín Balbuena
 • Jefe delegacional Alejandro Piña Medina ( PRD)
 • Total (12.90 sq mi)
 • Tot 430,978
 • Density 13,000/km2 (33,000/sq mi)
Time zone Central Staundart Time ( UTC-6)
 • Simmer ( DST) Central Daylicht Time ( UTC-5)
Postal codes 15000 – 15990

Venustiano Carranza is ane o the 16 delegaciones (burghs) o Mexico Ceety. The burgh wis shapit in 1970 whan the centre o Mexico Ceety wis subdividit intae fower burghs. Venustiano Carranza extends frae the far eastren portion o the historic centre o Mexico Ceety eastwaird tae the Peñón de los Baños an the border dividin the Federal Destrict frae the State o Mexico. Historically, maist o the territory wis unner Loch Texcoco, but ower the colonial period intae the 20t hunderyear, the loch dree'd up an the day the aurie is completely urbanisit. The burgh is hame tae three o Mexico Ceety’s major tradeetional mercats, includin La Merced, the Naitional Airchives o Mexico, the Palacio Legislativo de San Lázaro, the TAPO intercity bus terminal an the Mexico Ceety Internaitional Airport.

Geografie an environs

The burgh is locatit in the centre-east o Mexico Ceety. It borders Gustavo A. Madero, Cuauhtémoc an Iztacalco wi the State o Mexico tae the east. The territory measurs 33.42km2 which is 2.24% o the tot o the Federal Destrict. The burgh haes 2,290 blocks an aichty offeecially designatit neebourheids. [1]

It haes a average altitude o 2,240 meters abuin sea level wi maist o the surface flat. The territory is maistly the bed o the umwhile Lake Texcoco wi soils o compressed clay ower sand, wi the exception o the Peñón de los Banos at 2,290 meters abuin sea level, made o basalt . [1] [2] Acause it is maistly umwhile lochbed, floodin (especially durin the rainy saison frae Juin tae October) an hailstorms in winter, are no uncommon. Floodin is aften caused or exacerbatit bi the deterioratit drainage seestem. [3] Aside frae the ane elevation, the far wast o the burgh corresponds tae the far east o the umwhile Tenochtitlan island. For this raison, aboot ane quairter o the historic centre o Mexico Ceety belangs tae the burgh. [4] It haes a semi dry, temperate climate wi a average annual temperatur o 16C an a average rainfaw o 600mm. [1]

In the pairks an ither green spaces o the burgh, trees sic as ash, white cedar, cypress, fig an Indian laurel, various scrubs an gresses can be foond. Wildlife is limitit tae birds, rodents, lizards an insects. [3] In 2011, reforestation efforts teuk place in fower auries o the burgh, plantin 15,000 trees. [5]

Other Languages