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Majes District
Majes District is one of twenty districts of the Caylloma Province of the Department of Arequipa in Peru. It is located some 55 miles (90 km) west of Arequipa, and about 50 miles (80 km) north of Camaná. Its capital is El Pedregal. History The district was created on December 20, 1999 under the government of Alberto Fujimori, with its designated capital being El Pedregal. Surrounding areas were incorporated into the district on its creation. The area was relatively barren up until 1981, when an irrigation program was carried out. With the increase of fertile land, the population also grew substantially. The valley is noted for its agricultural tradition and somewhat isolated location, being located two hours away from Arequipa. Being part of the Department of Arequipa, the first settlers were the pre-Incan peoples, such as the Wari, with the Inca Empire coming later. Once the Spanish had established and settled themselves in nearby Arequipa, Spanish descendants, as we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Districts Of Peru
The districts of Peru () are the third-level country subdivisions of Peru. They are subdivisions of the provinces of Peru, provinces, which in turn are subdivisions of the larger regions of Peru, regions or departments. There are 1,838 districts in total. Overview A 1982 law requires a minimum of residents in an area for a new district to be legally established: 3,500 if it is located in the rainforest, 4,000 in the Andes highlands and 10,000 in the Chala, coastal area. In the dry Andean area, many districts have less than 3,500 inhabitants due to low population density in the area. In some cases, their populations have decreased in comparison to the days when they were founded. Districts that are located at very high altitudes tend to be scarcely populated. These districts usually are large in area, have few available land for use. Many basic government services do not reach all residents of these districts due to their difficult geography. Many lack financial means to govern th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Camaná
Camaná is the district capital of the homonymous province, located in the Department of Arequipa, Peru. In 2015, it had an estimate of 39,026 inhabitants. It lies 180 km from Arequipa, on the Panamerican Highway The Pan-American Highway (french: (Auto)route panaméricaine/transaméricaine; pt, Rodovia/Auto-estrada Pan-americana; es, Autopista/Carretera/Ruta Panamericana) is a network of roads stretching across the Americas and measuring about in to ..., which can be traveled in three hours. History It is where the Spanish founded "Villa Hermosa" in 1539, moving into the valley of Arequipa in 1540. The city of Arequipa had his first crib in this rich and extensive valley of Camaná. References External links * INEIbr>Census results Populated places in the Arequipa Region {{Arequipa-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Petroglyph
A petroglyph is an image created by removing part of a rock surface by incising, picking, carving, or abrading, as a form of rock art. Outside North America, scholars often use terms such as "carving", "engraving", or other descriptions of the technique to refer to such images. Petroglyphs are found worldwide, and are often associated with prehistoric peoples. The word comes from the Greek prefix , from meaning "stone", and meaning "carve", and was originally coined in French as . Another form of petroglyph, normally found in literate cultures, a rock relief or rock-cut relief is a relief sculpture carved on "living rock" such as a cliff, rather than a detached piece of stone. While these relief carvings are a category of rock art, sometimes found in conjunction with rock-cut architecture, they tend to be omitted in most works on rock art, which concentrate on engravings and paintings by prehistoric or nonliterate cultures. Some of these reliefs exploit the rock's nat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olivine
The mineral olivine () is a magnesium iron silicate with the chemical formula . It is a type of nesosilicate or orthosilicate. The primary component of the Earth's upper mantle, it is a common mineral in Earth's subsurface, but weathers quickly on the surface. For this reason, olivine has been proposed as a good candidate for accelerated weathering to sequester carbon dioxide from the Earth's oceans and atmosphere, as part of climate change mitigation. Olivine also has many other historical uses, such as the gemstone peridot (or chrysolite), as well as industrial applications like metalworking processes. The ratio of magnesium to iron varies between the two endmembers of the solid solution series: forsterite (Mg-endmember: ) and fayalite (Fe-endmember: ). Compositions of olivine are commonly expressed as molar percentages of forsterite (Fo) and fayalite (Fa) (''e.g.'', Fo70Fa30). Forsterite's melting temperature is unusually high at atmospheric pressure, almost , while ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gabbro
Gabbro () is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt. Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term ''gabbro'' may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic". By rough analogy, gabbro is to basalt as granite is to rhyolite. Etymology The term "gabbro" was used in the 1760s to name a set of rock types that were found in the ophiolites of the Apennine Mountains in Italy. It was named after Gabbro, a hamlet near Rosignano Marittimo in Tuscany. Then, in 1809, the German geologist Christian Leopold von Buch used the term more restrictively in his descri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colca River
Colca River (possibly from Quechua ''qullqa'' deposit) which downstream is called Majes and Camaná is a Peruvian river in the Arequipa Region that flows deep in the rugged Andes of southern Peru. It originates south-east of the village Janq'u Lakaya ''(Ancolaccaya)'' in the Callalli District of the Caylloma Province. On its way from Chivay to Cabanaconde it flows through one of the deepest canyons of the world known as the Colca Canyon.escale.minedu.gob.pe - UGEL maps of the provinces Camana, Castilla and Caylloma (2) (Arequipa Region) Near the town of Camaná the river empties into the Pacific Ocean. See also * Majes-Siguas Majes-Siguas is an irrigation project in Peru which envisages transferring water from the Colca River to the Siguas River for irrigation purposes, and further to take water from the Apurimac River. The project The original plan of the project ... Sources Rivers of Peru Rivers of Arequipa Region {{Peru-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archeology
Archaeology or archeology is the scientific study of human activity through the recovery and analysis of material culture. The archaeological record consists of artifacts, architecture, biofacts or ecofacts, sites, and cultural landscapes. Archaeology can be considered both a social science and a branch of the humanities. It is usually considered an independent academic discipline, but may also be classified as part of anthropology (in North America – the four-field approach), history or geography. Archaeologists study human prehistory and history, from the development of the first stone tools at Lomekwi in East Africa 3.3 million years ago up until recent decades. Archaeology is distinct from palaeontology, which is the study of fossil remains. Archaeology is particularly important for learning about prehistoric societies, for which, by definition, there are no written records. Prehistory includes over 99% of the human past, from the Paleolithic until the adven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossils
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dinosaur Tracks
A trace fossil, also known as an ichnofossil (; from el, ἴχνος ''ikhnos'' "trace, track"), is a fossil record of biological activity but not the preserved remains of the plant or animal itself. Trace fossils contrast with body fossils, which are the fossilized remains of parts of organisms' bodies, usually altered by later chemical activity or mineralization. The study of such trace fossils is ichnology and is the work of ichnologists. Trace fossils may consist of impressions made on or in the substrate by an organism. For example, burrows, borings (bioerosion), urolites (erosion caused by evacuation of liquid wastes), footprints and feeding marks and root cavities may all be trace fossils. The term in its broadest sense also includes the remains of other organic material produced by an organism; for example coprolites (fossilized droppings) or chemical markers (sedimentological structures produced by biological means; for example, the formation of stromatolites). H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Viceroyalty Of Peru
The Viceroyalty of Peru ( es, Virreinato del Perú, links=no) was a Spanish imperial provincial administrative district, created in 1542, that originally contained modern-day Peru and most of the Spanish Empire in South America, governed from the capital of Lima. The Viceroyalty of Peru was officially called the Kingdom of Peru. Peru was one of the two Spanish Viceroyalties in the Americas from the sixteenth to the eighteenth centuries. The Spanish did not resist the Portuguese expansion of Brazil across the meridian established by the Treaty of Tordesillas. The treaty was rendered meaningless between 1580 and 1640 while Spain controlled Portugal. The creation during the 18th century of Viceroyalties of New Granada and Río de la Plata (at the expense of Peru's territory) reduced the importance of Lima and shifted the lucrative Andean trade to Buenos Aires, while the fall of the mining and textile production accelerated the progressive decay of the Viceroyalty of Peru. Even ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spanish Empire
The Spanish Empire ( es, link=no, Imperio español), also known as the Hispanic Monarchy ( es, link=no, Monarquía Hispánica) or the Catholic Monarchy ( es, link=no, Monarquía Católica) was a colonial empire governed by Spain and its predecessor states between 1492 and 1976. One of the largest empires in history, it was, in conjunction with the Portuguese Empire, the first to usher the European Age of Discovery and achieve a global scale, controlling vast portions of the Americas, territories in Western Europe], Africa, and various islands in Spanish East Indies, Asia and Oceania. It was one of the most powerful empires of the early modern period, becoming the first empire known as "the empire on which the sun never sets", and reached its maximum extent in the 18th century. An important element in the formation of Spain's empire was the dynastic union between Isabella I of Castile and Ferdinand II of Aragon in 1469, known as the Catholic Monarchs, which in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inca Empire
The Inca Empire (also known as the Incan Empire and the Inka Empire), called ''Tawantinsuyu'' by its subjects, (Quechua for the "Realm of the Four Parts", "four parts together" ) was the largest empire in pre-Columbian America. The administrative, political and military center of the empire was in the city of Cusco. The Inca civilization arose from the Peruvian highlands sometime in the early 13th century. The Spanish began the conquest of the Inca Empire in 1532 and by 1572, the last Inca state was fully conquered. From 1438 to 1533, the Incas incorporated a large portion of western South America, centered on the Andean Mountains, using conquest and peaceful assimilation, among other methods. At its largest, the empire joined modern-day Peru, what are now western Ecuador, western and south central Bolivia, northwest Argentina, the southwesternmost tip of Colombia and a large portion of modern-day Chile, and into a state comparable to the historical empires of Eurasia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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