Cusco, Peru in the context of "Landslide"

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⭐ Core Definition: Cusco, Peru

Cusco or Cuzco (Latin American Spanish: [ˈkusko]; Quechua: Qosqo or Qusqu, both pronounced in Cuzco Quechua as [ˈqosqɔ]) is a city in southeastern Peru, near the Sacred Valley of the Andes mountain range, and the Huatanay and Urubamba rivers. It is the capital and largest city of the eponymous Cusco Province and Cusco Department. It has historically been one of the largest cultural, economic and political centers of Peru.

The city was originally founded in the 12th century as the capital of the Inca Empire. The region was conquered in the 16th-century by the Spanish and reestablished on 23 March 1524, with most of the city being constructed over monuments left from the Inca Empire. In 1983, Cusco was declared a World Heritage Site by UNESCO with the title "City of Cusco". It has become a major tourist destination, hosting over 2 million visitors a year and providing passage to numerous Incan ruins, such as Machu Picchu, one of the Seven modern wonders of the world and many others. The Constitution of Peru (1993) designates the city as the Historical Capital of Peru.

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👉 Cusco, Peru in the context of Landslide

Landslides, also known as landslips, rockslips or rockslides, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides.

Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable.

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