Aragua: Difference between revisions

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[[File:Cuyagua 001.jpg|thumb|[[Cuyagua]], Aragua state.]]
Aragua borders the [[Caribbean Sea]] to the north, with its coastline backed by the fast-rising central [[Venezuelan Coastal Range|Cordillera mountain range]]. [[Codazzi Peak]] reaches over 2400 m above sea level. Much of the rest of the state is made up of fertile valleys used for intensive agriculture, apart from in the extreme south where the flats of the central [[Los Llanos, Venezuela|Llanos]] region begin. On the western border is [[Lake Valencia (Venezuela)|Lake Valencia]].
 
The main rivers in the state are the [[Aragua River|Aragua]], the [[Guárico River|Guárico]], the [[El Limón River|El Limón]], the [[Tuy River|Tuy]], the Pao and the [[Turmero River|Turmero]]. They flow into the Caribbean Sea, Lake Valencia, or feed the vast [[Orinoco River]] network. The Camatagua reservoir is one of the main reservoirs supplying Caracas.
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===Geology===
 
Four natural regions can be distinguished in the entity: the coastal mountain range, the depression of Lake Valencia, the inland mountain range, and the Central Wavy Plains. In the depression of Lake Valencia, recent sedimentary formations predominate, while the mountainous areas present others that are highly affected by metamorphic processes, although in the presence of nuclei with more conserved igneous and sedimentary rocks. In the mountain ranges of the Interior chain, galleys can be observed, as spurs of that mountain range, which smoothen their forms towards the South until they enter the formation of the plains.
 
===Area===