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The Sierra consists of two major chains of the Andes mountains, known as the Cordillera Occidental (Western Chain) and Cordillera Oriental (Eastern Chain), and the intermontane basin or plateau between the two chains.

Several transversal mountain spurs, known as nudos, cut across the plateau.

The Nudo del Azuay, at 4,500 meters the highest of these transversal spurs, divides the Sierra into two subregions the area of modern volcanism to the north and the area of ancient volcanism to the south.

The former area consists of newer, higher mountains than those in the ancient volcanism section, which with time have eroded to lower levels.

The rainy season in this area lasts from October to May, with an average annual temperature range of 11.5° to 18° C.

The daily variation, however, can be extreme with very hot days and quite cold nights.

Yet, some often refer to the Sierra climate as "eternal spring".

The Sierra's climatic conditions, as well as recent volcanic activity, has produced peculiar and interesting plant formations that distinguish the area's beautiful landscapes called the paramo.

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