|
1970 Huascarán Debris Avalanche
The 1970 Huascarán Debris Avalanche occurred on May 31 1970, when a debris avalanche and mudflow triggered by the 1970 Ancash earthquake, Ancash earthquake destroyed the Peruvian town of Santo Domingo de Yungay, Yungay and ten nearby villages, leaving up to 30,000 people dead. It is the List of avalanches by death toll, deadliest avalanche or glacier-related disaster in history, surpassing the death toll from the previous deadliest avalanche disaster, the avalanches of White Friday (1916), White Friday on the Italian front (World War I), Italian front of World War I and the third or fourth most deadly landslide-related disaster of the 20th century, after the 1920 Haiyuan earthquake, Haiyuan landslides (China), the Armero tragedy (Colombia) and by some estimates the Khait landslide (Tajikistan). The north peak of Huascarán from which the avalanche originated had been considered unstable since 1962, when a smaller collapse wiped out several villages of the Callejón de Huaylas val ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Santo Domingo De Yungay
Yungay, currently known as Yungay Viejo (Spanish for "Old Yungay") and founded in 1540 as Santo Domingo de Yungay, was a town in Peru that served as the seat of the province of the same name in the Department of Ancash. Located 2,400 m.a.s.l., it was destroyed by a landslide that originated at the nearby Huascarán mountain due to the 1970 Ancash earthquake. Five thousand people disappeared during the event, with some 300 people surviving due to taking refuge in the local cemetery. History Spanish era Yungay Valley was explored for the first time by the Spanish conquistadors in 1533 during reconnaissance expeditions from Cajamarca commanded by Hernando de Soto and Miguel de Estete. Dominican Order members founded the town and the convent of Santo Domingo de Yungay on August 4, 1540. At the initiative of Father Domingo de Santo Tomás, the jurisdiction was elevated to the category of Vicariate in 1579. On January 6, 1730, a violent earthquake caused an avalanche from Huandoy mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Callejón De Huaylas
The Santa Valley (Quechua language, Quechua ''Sancta'') is an inter-andean valley in the Ancash Region in the north-central highlands of Peru. Due to its location between two mountain ranges, it is known as Callejón de Huaylas, the Alley of Huaylas, whereas "Huaylas" refers to the territorial division's name during the Viceroyalty of Peru. Going north from Lima, the road climbs to an altitude of 3,945 m, where the lake Conococha marks the head of the valley. This lake is the main source of Santa River. From here the road descends into the Callejón de Huaylas, demarcated by the Cordillera Blanca ("white range") to the east and the Cordillera Negra ("black range") to the west. To the south rise the summits of the Huayhuash mountain range. Huaraz, the capital of Ancash Region, Ancash, is the largest city in the Callejón, located at 3,000 m above sea level. In the valley north of Huaraz there are the towns Carhuaz, Yungay, Peru, Yungay (the site of a major earthquake and landslide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Lake Outburst Flood
A glacial lake outburst flood (GLOF) is a type of outburst flood caused by the failure of a dam containing a glacial lake. An event similar to a GLOF, where a body of water contained by a glacier melts or overflows the glacier, is called a jökulhlaup. The dam can consist of glacier ice or a terminal moraine. Failure can happen due to erosion, a buildup of water pressure, an avalanche of rock or heavy snow, an earthquake or cryoseism, volcanic eruptions under the ice, or massive displacement of water in a glacial lake when a large portion of an adjacent glacier collapses into it. Increasing glacial melting because of climate change, alongside other environmental effects of climate change (i.e. permafrost melting) mean that regions with glaciers are likely to see increased flooding risks from GLOFs. This is especially true in the Himalayas where geologies are more active. A 2023 study found 15 million people at risk from this hazard, mostly in China, India, Nepal, Pakistan, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inca
The Inca Empire, officially known as the Realm of the Four Parts (, ), was the largest empire in pre-Columbian America. The administrative, political, and military center of the empire was in the city of Cusco. The History of the Incas, Inca civilisation rose from the Peruvian highlands sometime in the early 13th century. The Portuguese explorer Aleixo Garcia was the first European to reach the Inca Empire in 1524. Later, in 1532, the Spanish Empire, Spanish began the conquest of the Inca Empire, and by 1572 Neo-Inca State, the last Inca state was fully conquered. From 1438 to 1533, the Incas incorporated a large portion of western South America, centered on the Andes, Andean Mountains, using conquest and peaceful assimilation, among other methods. At its largest, the empire joined modern-day Peru with what are now western Ecuador, western and south-central Bolivia, northwest Argentina, the southwesternmost tip of Colombia and Incas in Central Chile, a large portion of modern- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saint Dominic
Saint Dominic, (; 8 August 1170 – 6 August 1221), also known as Dominic de Guzmán (), was a Castilians, Castilian Catholic priest and the founder of the Dominican Order. He is the patron saint of astronomers and natural scientists, and he and his order are traditionally credited with spreading and popularizing the rosary. Life Birth and early life Dominic was born in Caleruega, halfway between Osma and Aranda de Duero in Old Castile, Spain. He was named after Dominic of Silos, Saint Dominic of Silos. The Benedictine abbey of Santo Domingo de Silos lies a few miles north of Caleruega. In the earliest narrative source, by Jordan of Saxony, Dominic's parents are not named. The story is told that before his birth his barren mother made a pilgrimage to the Abbey of Santo Domingo de Silos, Abbey at Silos, and dreamt that a dog leapt from her womb carrying a flaming torch in its mouth, and seemed to set the earth on fire. This story is likely to have emerged when his order became ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Espacio Y Desarrollo
''Espacio y Desarrollo'' is an annual Peruvian peer-reviewed scientific journal of geography. It was established in 1989 and is published by the Centro de Investigación en Geografía Aplicada (Pontificia Universidad Católica del Perú). The current editor-in-chief is Ana Sabogal. ''Espacio y Desarrollo'' focuses on environmental geography, linking physical geography and human geography. Contributions often highlight the human-environmental relationship. The regional focus is on Latin America. Abstracting and indexing The journal is abstracted and indexed in ERIH PLUS, EBSCOhost and Latindex Latindex (Regional Cooperative Online Information System for Scholarly Journals from Latin America, the Caribbean, Spain and Portugal) is a bibliographical information system available for free consultation. Established as a network in 1997, the .... See also * Geography portal References External links * Centro de Investigación en Geografía Aplicada 1989 establishments in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yungay Cemetery
Yungay may refer to the following places: Chile *Yungay, Chile, a town in the Ñuble Region *Barrio Yungay, a neighborhood of Santiago, Chile * Yungay, the driest place on earth, in Antofagasta Region Peru *Yungay, Peru *Santo Domingo de Yungay, which existed from 1540 to 1970 *Yungay District Yungay district is a district in the Province of Yungay in the Ancash region, Peru. It was created by law on October 28, 1904.Yungay PeruYungay Peru retrieved March 7, 2008 Geography The Cordillera Blanca traverses the province. Waskaran, the ... * Yungay Province {{geodis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley Of Huaylas - Town Of Yungay, And The Huascaran Peak (cropped)
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. Format ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quechua Language
Quechua (, ), also called (, 'people's language') in Southern Quechua, is an Indigenous languages of the Americas, indigenous language family that originated in central Peru and thereafter spread to other countries of the Andes. Derived from a common ancestral "Proto-Quechuan language, Proto-Quechua" language, it is today the most widely spoken Pre-Columbian era, pre-Columbian language family of the Americas, with the number of speakers estimated at 8–10 million speakers in 2004,Adelaar 2004, pp. 167–168, 255. and just under 7 million from the most recent census data available up to 2011. Approximately 13.9% (3.7 million) of Peruvians speak a Quechua language. Although Quechua began expanding many centuries before the Inca Empire, Incas, that previous expansion also meant that it was the primary language family within the Inca Empire. The Spanish also tolerated its use until the Peruvian War of Independence, Peruvian struggle for independence in the 1780s. As a result, var ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holocene
The Holocene () is the current geologic time scale, geological epoch, beginning approximately 11,700 years ago. It follows the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene is an interglacial period within the ongoing Ice age, glacial cycles of the Quaternary, and is equivalent to Marine isotope stages, Marine Isotope Stage 1. The Holocene correlates with the last maximum axial tilt towards the Sun of the Earth#Axial tilt and seasons, Earth's obliquity. The Holocene corresponds with the rapid proliferation, growth, and impacts of the human species worldwide, including Recorded history, all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban culture, urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global significance for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to Semi-arid climate, semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where a flow of sediment or rocks emerge from a confined channel and are suddenly free to spread out in many directions. For example, many alluvial fans form when steep mountain valleys meet a flat plain. The transition from a narrow channel to a wide open area reduces the carrying capacity of flow and results in Deposition (geology), deposition of sediments. The flow can take the form of infrequent debris flows like in a landslide, or can be carried by an intermittent stream or creek. The reduction of flow is key to the formation of alluvial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
