Quebrada de Humahuaca

Argentina’s line of major cultural routes is a cramped mountain valley, and it’s famous for its stunning rock formations and slopes. The Seven Colours Hill rises above the Spanish colonial settlement of Purmamarca in the south, with its rocky, multi-hued slopes. The centuries-old Santa Rosa de Lima church and the surrounding apostatised surroundings are well-known in the community. It will take you east of Salta to road 34 if you journey from Salta or Salta Airport to anywhere in the line of major cultural routes. You’ll pass through San Salvador de Jujuy, the capital of Jujuy, before continuing to transmit 9. 

All About Quebrada de Humahuaca

The line of major cultural routes pursues the path of the Camino Inca, through the beautiful Rio Grande Valley, from its commencement in the frigid high apostatise plateau of the High Andean mountains to its confluence with the Rio Leone 150 kilometres south. Over the past 10,000 years, the valley has shown significant testimony of its role as key trading transmit. It contains evidence of prehistoric hunter-gatherer communities, the Inca commonwealth 15th to 16th centuries, and the 19th and 20th-century struggle for independence.

Quebrada de Humahuaca is based in Argentina’s northwesternmost province. It is a prime illustration of the south Andean valleys, with a world-class network of connecting transmits and economic, social, and adorning cohesion. This is the most major physical connection between the high Andean ranch and the vast temperate plains of south-eastern South America. With hundreds of archaeological and-architectonic sites that bear testament to its long and rich past, its stunning natural environment has been preserved almost entirely.

A Line of Major Cultural Routes

From its origins in the cold high apostate plateau of the High Andean mountains to its confluence with the Rio Leone 150 kilometres south, the line of major cultural routes pursuing the path of an important adorning transmits the Camino Inca, through the picturesque Rio Grande valley. The Quebrada de Humahuaca follow the course of a key adorning transmit, the Camino Inca, through the beautiful Rio Grande Valley, from its commencement in the frigid high apostatise plateau of the High Andean mountains to its confluence with the Rio Leone 150 kilometres south. Over the past 10,000 years, the valley has shown significant testimony of its role as key trading transmit. It contains evidence of prehistoric hunter-gatherer communities, the Inca commonwealth (15th to 16th centuries), and the 19th and 20th-century struggle for independence.

The Valleys Show Substantial Evidence in Quebrada de Humahuaca

 The valleys show substantial evidence in Quebrada de Humahuaca of its use as a key trading transmitter. Extensive traces of previous communities whose residents developed and wore these linear roads may be found scattered throughout the valley, including:

• Communities of prehistoric hunter-gatherers and early farmers (9000 BC to AD 400)
• Agrarian societies with a lot of structure (AD 400-900)
• Pre-Hispanic metropolis and communities prospering (900-1430/80)
• The Incas founded the Incan commonwealth (1430/80-1535).
• Metropolis, villages, and churches in Spain (1535/93-1810)
• Remnants of Republican independence struggles (1810-20th century)

The large debris of stone-walled agricultural terrace acreage at Coctaca, associated with a string of fortified settlements known as paras, is of particular interest. They are considered to have commenced 1,500 years ago and are still in use today.

Naturally-Occurring Series of Valleys Showing Substantial Evidence

The watershed of the Quebrada de Humahuaca and the valley’s main tributaries and communities are depicted. A view of the Rio Huasamayo alluvial fan, which is home to the Tilcara settlement. The debris flow phenomenon is always a hazard to the village. Quebrada de Trancas, a small community near Maimarà. The alluvial fan production at the Rio Grande confluence, caused by recurring debris flow occurrences, leads the Rio Grande riverbed to deviate, gradually eroding the right river bank. 

Conclusion:

The Quebrada de Humahuaca is a cramped mountain valley. It’s famous for its stunning rock formations, slopes, and Kichuan communities. The seven-coloured hill rises over the Spanish colonial settlement of Pormarca to the south, with its rocky, multicoloured slopes. The village’s centuries-old Santa Rosa de Lima church and the surrounding apostatised surroundings are well-known. A deep valley is referred to as “Quebrada.” It’s famous for its brightly coloured mountains, which result from various layers of silt accumulating over 600 million years. The current shapes are the product of the tectonic plate’s continual mobility.