Dec 7, 2020

Vinicunca ( The Rainbow Mountain), Cordillera de Vilcanota, Cusco, Peru

Vinicunca or Winikunka, also called Montaña de Siete Colores, Montaña de Colores or Rainbow Mountain, is a mountain in the Andes of Peru with an altitude of 5,200 meters above sea level. It is located on the road to the Ausangate mountain in the Peruvian Andes, in the Cusco region, between the districts of Cusipata, province of Quispicanchi, Pitumarca, and the province of Canchis.

Tourist access requires a two-hour drive from Cusco, and a walk of about 5-kilometer (3.1 mi) or three-and-a-half-hour drive through Pitumarca and a one-half-kilometre (0.31 mi) steep walk (1-1.5 hours) to the hill. As of 2019, no robust methods of transportation to Vinicunca have been developed to accommodate travelers, as it requires passage through a valley.

In the middle of the 2010s, mass tourism came, attracted by the mountain's series of stripes of various colors due to its mineralogical composition on the slopes and summits. The mountain used to be covered by glacier caps, but these have melted recently due to global warming.
 









Travelers to Peru and locals generally agree that the best time of the year to visit the colorful site is in August, since it is dry season and provides a beautiful view, maximizing the vivid colors of the mountains. Nevertheless, the famous colors always look beautiful. Travelers are advised to try to avoid days following significant rainfall (in December, January and February), more so after snow has fallen.As to fauna, travelers may see a wide variety of alpacas and other camelids in certain short seasons.

According to the Cultural Landscape Office of the Decentralization of the City of Cusco, the seven colors of the mountain are due to its mineralogical composition: the pink color is due to red clay, fangolitas (mud) and arilitas (sand); the whitish colouring is due to quartzose, sandstone and marls, rich in calcium carbonate; the red is due to claystones (iron) and clays belonging to the Upper Tertiary period; the green is due to phyllites and clays rich in ferro magnesian; the earthy brown is a product of fanglomerate composed of rock with magnesium belonging to the Quaternary period; and the mustard yellow color comes from the calcareous sandstones rich in sulphurous minerals.
 
for more information - Official Website  

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