Information about the city Puno
Puno is a city in southeastern Peru, located on the shore of Lake Titicaca. It is the capital city of the Puno Region and the Puno Province with a population of approximately 149,064 (2014 estimate). The city was established in 1668 by viceroy Pedro Antonio Fernández de Castro as capital of the province of Paucarcolla with the name San Juan Bautista de Puno. The name was later changed to San Carlos de Puno, in honor of king Charles II of Spain. Puno has several churches dating back from the colonial period; they were built to service the Spanish population and evangelize the natives.
Puno is an important agricultural and livestock region; important livestock are llamas and alpacas, which graze on its immense plateaus and plains. Much of the city economy relies on the black market, fueled by cheap goods smuggled in from Bolivia. Puno is served by the Inca Manco Capac International Airport in nearby Juliaca.
Puno is situated between the shores of Lake Titicaca and the mountains surrounding the city. There is less than two miles of flat land between the shores and the foothills, which has caused the growing city to continue to expand upwards onto the hillsides. As a result, the town's less developed and poorest areas, which are high on the hillsides, often have very steep streets, which are generally unpaved and cannot be accessed by automobile.
Up one of these streets is the Kuntur Wasi viewpoint, which has a large metal sculpture of a condor. There are some 700 steps to climb to reach the sculpture, but the view across the city and Lake Titicaca beyond is breathtaking.
During the celebrations of the Feast of the "Virgen de la Candelaria" and the Regional Competition of Autochthonous Dances. Puno's access to Lake Titicaca is surrounded by 41 floating islands. To this day, the Uros people maintain and live on these man-made islands, depending on the lake for their survival, and are a large tourist destination. Dragon Boat racing, an old tradition in Puno, is a very popular activity amongst tourists.
Puno is the first major hub in the constant migration of indigenous peoples of the Andes to the larger cities of Peru. It is the largest city in the Southern Altiplano and is the recipient of new residents from surrounding smaller agricultural communities of people seeking better opportunities for education and employment. As such, Puno is served by several small Institutes of Technology, Education and other technical or junior college-type facilities. Additionally it is home to what is commonly referred to as the "UNA" or the Universidad Nacional del Altiplano, which was founded in 1856.
Puno features a subtropical highland climate (Cwc).
As Puno is located at such a high elevation, it experiences more extreme weather conditions than would be expected for its tropical latitude. The average annual temperature is about 8.4 °C,[2] and the weather never gets overly warm. During the winter months from June to August, night-time temperatures usually drop well below 0 °C. At this high altitude, the rays of the sun are very strong. Most of the annual precipitation falls during the southern hemisphere summer, with the winter months being very dry.
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.
