Organizacion Economia De La Epoca Colonial

GEOGRAPHY
Relief: They cross the state from east to west, two parallel mountain ranges, separated by a central depression, which determines the existence of three distinct physiographic regions, which follow from north to south. The northern end is injured by the central section of the Cordillera del Litoral culminating peak of 2,435 m Ash and Codazzi Peak, 2,426 m.

Due to the proximity ofthe mountains, the coast is rocky and steep, rugged coats and presenting good, presenting

good natural shelters such as Turiamo Cove, natural harbor that penetrates about 4 km inland. South of the Cordillera del Litoral opens tectonic depression Aragua rivers, the most important inmisario Lake Valencia, and Tuy, flowing in the opposite direction and whose births are separated by an alignment ofalluvial hill.
In the far west, the lake of Valencia occupies the bottom of the depression. Finally, the Serrania d
the Interior, whose highest elevation is on the hill Cataure, of 1,614 m, separates depression Tuy Aragua-western end of the Central Plains.

Hydrography: The river flows from depression every year and reduces the surface of Lake oats Camatagua the southern slopes of the Serraniadel Interior.
Valencia tended to decline, reversed situation with water supply pranks.

Tuy River, which rises at the foot of the peak Codazzi, Aragua state goes through the gorge of Tileries to follow Miranda state. Guarico River, whose water reservoir holds

Forest Resources: ACAPRO, mahogany, cedar, mijao, saman.

Mineral Resources: pottery clay, barite, limestone and nickel.

TOURISMHot Springs:
Hot Springs Onoto
    Hot Springs Villa de Cura
Bays and beaches:
   Cata Bay
    Turiamo Bay
    Ocumare Cove
    Choroní
    Ocumare Swamp
    Juan Andrés Cove
    Cuyagua Cove
    Puerto Maya Cove
    Chuao Cove
    Cove Café
    Aroa Beach
Islands:
 Caigüire Island
  Stone Island
    La Cucaracha
    Ant
    The Del Zorro
Lakes and Ponds:
Lake Valencia: IsVenezuela in the second extension of 378 km2. According to report of the division of hydrology. In its waters shared with the Carabobo State are 22 islands. Little is known of the history of soil Pliocene lake, they may be related to the terraces pleitocenas of marginal lands that stretch to the west, in the state of Carabobo. On the banks of the lake there is almost no population, it is forced towithdraw from the muddy banks, as crops are paragraphs, the lake is considered to be an appropriate site for recreation and tourism.

Taiguaiguay Lagoon: Located within districts Zamora and Marino. It is a lagoon formed by the river mined land with slight depressions. Today is a reservoir for irrigation of 8,000 hectares.

National Parks:
 Henry Pittier National Park
    National ParkAgustin Codazzi

History
Prehistory
The region currently Aragua form Columbian times was inhabited by ethnic group primarily Caribbean. Among the people known to the Spanish during the Conquest were the meregotos.
Spanish Conquest and times
Aragua was part of the Province of Caracas from 1555.
European groups later entered the area of ​​Aragua that what is now Carabobo and Miranda. It was in thelast decade of the sixteenth century when the Spanish began to introduce parcels in the valleys of Aragua.
By 1620 all of Aragua lands were divided among some 40 trustees, primarily living in the valley of Caracas.
Ottawa was founded in 1701.
By 1780 the Victory was a village with about 800 Indians who spoke only Spanish and more than 4,000 people from other groups, including Spanish, Creoles,mestizos, blacks and zambos.4
Humboldt meant that for 1800 in the valleys of Aragua - which at that time included both sides of Lake Valencia, most consisted of brown and Creoles, mulattos and slaves apart and still had about 5000 registered indigenous most concentrated in Turmeremo and Guacara. Now no one spoke their ancestral languages.
Nineteenth century
In February 1848 came the Gauteng...