From Huánuco
To Cerro de Pasco
Trip Thursday 25 April

Huánuco to Cerro de Pasco

04/25/2024


Information about the city Huánuco

Huánuco is a city in central Peru. It had a population of 75,000 as of 2007 and in 2014 it had a population of 172,924. It is the capital of the Huánuco Region and the Huánuco District. It is the seat of the diocese of Huánuco. The metropolitan city of Huanuco is 170,000 hab (2011, urban pop, INEI). It has three districts, Huanuco (head), Amarilis, and Pillco Marca. In this city, the Higueras river meets the Huallaga river, one of the largest rivers in the country. The city of Huánuco was founded by Spanish conquistador Gómez de Alvarado in 1539, in the Inca town of Yarowilca. In 1541, the city was moved to its current location in the Pillco Valley. It is served by the Alférez FAP David Figueroa Fernandini Airport. One of the main highways of the country passes by Huanuco, communicating Lima-Callao with Tingo Maria and Pucallpa in the Peruvian Amazonia.

Huánuco has a mild semi-arid climate. The temperatures are pleasant (with warm days and cool nights) throughout the year due to its elevation (1913 mt. - 6275 feet).


Information about the city Cerro de Pasco

Cerro de Pasco (population 70,000) is a city in central Peru, located at the top of the Andean mountains. It is the capital of the Pasco region, and an important mining center. At 4,330 metres (14,210 ft) elevation, it is one of the highest cities in the world, and the highest or the second highest city with over 50,000 inhabitants, with elevation reaching up to 4,380 m in the Yanacancha area. It is connected by road and by rail to the capital Lima, as far as 300 km.

Cerro de Pasco became one of the world's richest silver producing areas after silver was discovered there in 1630.[2] It is still an active mining center. The Spanish mined the rich Cerro de Pasco silver-bearing oxide ore deposits since colonial times. Sulfide minerals are more common in the Atacocha district however.

Francisco Uville arranged for steam engines made by Richard Trevithick of Cornwall, England, to be installed in Cerro de Pasco in 1816 to pump water from the mines and allow lower levels to be reached. However, fighting in the Peruvian War of Independence brought production to a halt from 1820 to 1825. Three major mines in the area include the Machcan, Atacocha, and Milpo. SIlver ore occurs in hydrothermal veins or as sulfides and clay minerals replacing the Jurassic Pucara limestone. Porphyry dacite stocks are found intruded near the Atacocha and Milpo mines along the Atacocha Fault. Compania Minera Atacocha started operations at the Atacocha Mine in 1936. Ore minerals include galena and sphalerite.

At 4,330 metres (14,210 ft) above sea level, Cerro de Pasco has an (E) Alpine Climate (the average temperature of the warmest month is lower than 10 °C (50 °F)), the city is one of the largest in the world with this classification. Temperatures are too cold to allow for tree growth in and around the city giving the countryside its barren appearance. Cerro de Pasco has humid summers, dry winters and chilly to cold temperatures throughout the year. Snowfall occurs annually.

Vídeo de Huánuco

Vídeo de Cerro de Pasco