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Lake Llanquihue
Lake Llanquihue is the second-largest lake in Chile with an area of about , after Lake General Carrera which shared with Argentina. It is situated in the southern Los Lagos Region in the Llanquihue and Osorno provinces. The lake's fan-like form was created by successive piedmont glaciers during the Quaternary glaciations. The last glacial period is called Llanquihue glaciation in Chile after the terminal moraine systems around the lake.Patagonia Chilena Some historians consider Llanquihue Lake to have been within the range of ancient Chono nomadism. Lake Llanquihue is located in southern Chile a territory of northern Patagonia in the Los Lagos Region. The lake's views of Volcán Osorno make the surrounding cities such as Puerto Varas Puerto Varas, also known as "La ciudad de las rosas" or “the city of roses”, is a city and commune located in the southern Chilean province of Llanquihue, in the Los Lagos Region. The city is famous for its German traditions, its natur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osorno (volcano)
Osorno Volcano is a tall conical stratovolcano lying between Osorno Province and Llanquihue Province, in Los Lagos Region of Chile. It stands on the southeastern shore of Llanquihue Lake, and also towers over Todos los Santos Lake. Osorno is considered a symbol of the local landscape and, as such, tends to be the referential element of the area in regards to tourism and marks the beginning of Chilean Patagonia. Etymology The current name comes from a nearby town, Osorno, where it was visible to Spanish settlers. Native populations gave it different names, such as Purailla, Purarhue, Prarauque, Peripillan, Choshueco, Hueñauca and Guanauca. The latter two names were the most common in the mid-18th century. Overview The volcano has a height of 2,652 meters (8,701 feet) and its imposing conical feature looms over lake Llanquihue, across from the cities of Frutillar, Puerto Varas, and Llanquehue. There has been no volcanic activity for over one hundred years. Skiing and hiking ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llanquihue Province
Llanquihue Province ( es, Provincia de Llanquihue) is one of four provinces of the Chilean region of Los Lagos (X). Its capital is Puerto Montt. Chile's second largest lake, Lake Llanquihue, is located in the province as well as four volcanoes: Osorno, Calbuco, Puntiagudo and Cerro Tronador. European settlement of Llanquihue began in 1852 when Germans were encouraged to immigrate to southern Chile. A century later in 1945 a new wave of Jewish refugees came from Germany. The region is well known for the beauty of its natural environment as well as for the food and seafood from the ports of Puerto Montt and |
Volcán Osorno
Osorno Volcano is a tall conical stratovolcano lying between Osorno Province and Llanquihue Province, in Los Lagos Region of Chile. It stands on the southeastern shore of Llanquihue Lake, and also towers over Todos los Santos Lake. Osorno is considered a symbol of the local landscape and, as such, tends to be the referential element of the area in regards to tourism and marks the beginning of Chilean Patagonia. Etymology The current name comes from a nearby town, Osorno, where it was visible to Spanish settlers. Native populations gave it different names, such as Purailla, Purarhue, Prarauque, Peripillan, Choshueco, Hueñauca and Guanauca. The latter two names were the most common in the mid-18th century. Overview The volcano has a height of 2,652 meters (8,701 feet) and its imposing conical feature looms over lake Llanquihue, across from the cities of Frutillar, Puerto Varas, and Llanquehue. There has been no volcanic activity for over one hundred years. Skiing and hikin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chono People
The Chono people, or GuaitecoUrbina Burgos 2007, p. 334. were a nomadic indigenous people or group of peoples of the archipelagos of Chiloé, Guaitecas and Chonos. The Chono people lived as hunter-gatherers traveling by canoe. Much of what is known from Spanish sources on Chonos is filtered by a Huilliche worldview, as Huilliches and Huilliche language was used to communicate with Chonos. Physical appearance Together with other canoe-faring peoples of western Patagonia, the Chono people shared the physical features of being of low stature, being long-headed (dolichocephalic) and having a "low face". In the opinion of Robert FitzRoy who saw the Chono people in the 1830s, they were more muscular and with a more beautiful appearance when compared to canoe-farers further south.Trivero Rivera 2005, p. 42. Alberto Achacaz Walakial, himself a Kawésqar born around 1929, said that the Chono people were taller and of darker skin than his people. He also added that their noses and fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Proven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Llanquihue Glaciation
The last glacial period and its associated glaciation is known in southern Chile as the Llanquihue glaciation ( es, Glaciación de Llanquihue). Its type area lies west of Llanquihue Lake where various drifts or end moraine systems belonging to the last glacial period have been identified. The glaciation is the last episode of existence of the Patagonian Ice Sheet. The preceding interglacial is known as the Valdivia interglacial after its type locality of Valdivia. General characteristics The characteristics of the glaciation differ according to latitude. In Central Chile, south of Atacama Desert, the extent of the Llanquihue glaciation was controlled by precipitation which increases to the south. Maximum glaciers advances were not synchronous across the whole latitudinal gradient as they were triggered by north and southward shifts in the moisture-bringing Westerlies and its storm tracks. Glaciers in Central Chile were particularly sensitive to shifts in the precipitation pat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary Glaciation
The Quaternary glaciation, also known as the Pleistocene glaciation, is an alternating series of glacial and interglacial periods during the Quaternary period that began 2.58 Ma (million years ago) and is ongoing. Although geologists describe this entire period up to the present as an "ice age", in popular culture this term usually refers to the most recent glacial period, or to the Pleistocene epoch in general. Since Earth still has polar ice sheets, geologists consider the Quaternary glaciation to be ongoing, though currently in an interglacial period. During the Quaternary glaciation, ice sheets appeared, expanding during glacial periods and contracting during interglacial periods. Since the end of the last glacial period, only the Antarctic and Greenland ice sheets have survived, with other sheets formed during glacial periods, such as the Laurentide Ice Sheet, having completely melted. The major effects of the Quaternary glaciation have been the continental erosion o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piedmont Glacier
Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories: * Ice flow is constrained by the underlying bedrock topography * Ice flow is unrestricted by surrounding topography Unconstrained Glaciers Ice sheets and ice caps Ice sheets and ice caps cover the largest areas of land in comparison to other glaciers, and their ice is unconstrained by the underlying topography. They are the largest glacial ice formations and hold the vast majority of the world's fresh water. Ice sheets Ice sheets are the largest form of glacial formation. They are continent sized ice masses that span areas over . They are dome ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osorno Province
Osorno Province ( es, Provincia de Osorno) is one of the four provinces in the southern Chilean region of Los Lagos (X). The province has an area of and a population of 221,496 distributed across seven communes ( Spanish: ''comunas''). The provincial capital is the city of Osorno. Osorno is a city located in southern Chile a territory of northern Patagonia in the Los Lagos Region. The Chilean Patagonia starts at Latitude 39° South in Valdivia and then it continues through the Chiloe Island and the fiords that continue its course south through the Pacific Ocean and the Cordillera de los Andes until it reaches Latitude 56° South at Cape Horn.The province possesses one of the most frequented mountain passes of Chile, the Cardenal Antonio Samoré Pass which links the province with Villa La Angostura and San Carlos de Bariloche in Argentina. Administration As a province, Osorno is a second-level administrative division, governed by a provincial governor who is appointed by the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Los Lagos Region
Los Lagos Region ( es, Región de Los Lagos , ''Region of the Lakes'') is one of Chile's 16 regions, which are first order administrative divisions, and comprises four provinces: Chiloé, Llanquihue, Osorno and Palena. The region contains the country's second largest island, Chiloé, and the second largest lake, Llanquihue. Its capital is Puerto Montt; other important cities include Osorno, Castro, Ancud, and Puerto Varas. The mainland portion of Los Lagos Region south of Reloncaví Sound (Palena Province) is considered part of Patagonia. Historically, the Huilliche have called this territory between Bueno River and Reloncaví Sound Futahuillimapu, meaning "great land of the south". The region hosts Monte Verde, one of the oldest archaeological sites of the Americas. The largest indigenous group of the region are the Huilliche who lived in the area before the arrival of the Spanish. The Spanish crown settled Chiloé Archipelago in 1567 Hanisch, Walter. ''La Isla de Chi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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