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Baker Channel
Baker Channel, also known as Calen Inlet, is a channel of Chile located in the Tortel, Aysén del General Carlos Ibáñez del Campo Region. The Baker River discharges into Martinez Inlet, the northern part of this large estuary. It penetrates the mainland about and opens into Tarn Bay at the south-east corner of the Gulf of Penas. Merino Jarpa Island lies wholly within this great estuary, while at its mouth lies a group of smaller islands, called Baker Islands, which separate it from Messier Channel. Baker Channel also receives the waters of the O'Higgins/San Martín Lake through the Pascua River. The lake's far-reaching fjord-like arms extend approximately from lat. 49° 11' to 48° 22' S. Its north-west arm is that which drains into the mentioned river. The calving front of Jorge Montt Glacier, which is the northern glacier of the Southern Patagonian Ice Field, reaches the Baker Channel. A number of icebergs can be seen in this area. The channel marks the northern border ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Channel (geography)
In physical geography, a channel is a type of landform consisting of the outline of a path of relatively shallow and narrow body of water or of other fluids (e.g., lava), most commonly the confine of a river, river delta or strait. The word is cognate to canal, and sometimes takes this form, e.g. the Hood Canal. Formation Channel initiation refers to the site on a mountain slope where water begins to flow between identifiable banks.Bierman, R. B, David R. Montgomery (2014). Key Concepts in Geomorphology. W. H. Freeman and Company Publishers. United States. This site is referred to as the channel head and it marks an important boundary between hillslope processes and fluvial processes. The channel head is the most upslope part of a channel network and is defined by flowing water between defined identifiable banks. A channel head forms as overland flow and/or subsurface flow accumulate to a point where shear stress can overcome erosion resistance of the ground surface. Channel h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pascua River
The Pascua River is a river located in the Aysén del General Carlos Ibáñez del Campo Region of Chile. In spite of being a short river, its drainage basin is the seventh-largest in the country due to the great size of the O'Higgins/San Martín Lake, its source. The Pascua River was discovered in 1898 by the German Hans Steffen, during the exploration of the area near Christmas time (''Pascua'' means Easter but is frequently used to describe Christmas in Chilean Spanish, thus explaining the origin of its name). The river has its source in the northern part of the north-west arm of the lake O'Higgins in the form of a small stream, in an area surrounded by steep-sided mountains that reach over 1,000 meters with glaciers spilling down to the lake or to the river. The river flows quickly forming rapids until it creates a cascade in the place where it falls into the Chico Lake. After leaving this lake, the river forms a new cascade and rushes furiously, preventing any type of navi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Patagonian Ice Field
The Northern Patagonian Ice Field, located in southern Chile, is the smaller of two remnant parts in which the Patagonian Ice Sheet in the Andes Mountains of southern South America can be divided. It is completely contained within the boundaries of Laguna San Rafael National Park. Description The Northern Patagonian Ice Field is a vestige of the Patagonian Ice Sheet, an extensive ice sheet that covered all of Chilean Patagonia and the westernmost parts of Argentine Patagonia during the Quaternary glaciations. Today, with its glaciers largely in retreat and only an area of , it is still the second largest continuous mass of ice outside of the polar regions. Its survival depends on its elevation (), favorable terrain and a cool, moist, oceanic climate. The ice field has 28 exit glaciers, the largest two — San Quintin and San Rafael — nearly reach sea level to the west at the Pacific Ocean. Smaller exit glaciers, like San Valentín and Nef, feed numerous rivers and gla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guayaneco Archipelago
The Guayaneco Archipelago ( es, Archipiélago Guayaneco) is an archipelago in southern Chile. It consists of 2 main islands, :es:Isla Wager (to the east), :es:Isla Byron (to the west), and many smaller islands. It was heavily glaciated during the most recent ice age. These glaciers dissected these mountain islands into a series of deep river valleys and glacial troughs. Today these glacial troughs are deep channels and fjords. The islands of the Guayaneco Archipelago comprise a series of elongated islands and deep bays that are the traces of a drowned coastal range. A number of deep channels are traversing generally north to south through the islands. These include the Messier Channel in the lower left portion of the image, and the Fallos Channel near the center of the image. Forests cover the lower slopes of the mountains throughout the many islands. Human settlement on these islands is scarce. History The archipelago is thought to have been a cohabitational contact zone be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caleta Tortel, Chile
Caleta Tortel is a coastal village ( es, aldea) in Chile. It is the administrative centre of the commune of Tortel and is located between the mouth of the Baker River the largest river in Chile and a small embayment of the Baker Channel. The surrounding geography is rugged, formed by a number of islands, fjords, channels and estuaries. The village was founded in 1955 to exploit the cypress de las guaytecas or Guaytecas Cypress (Pilgerodendron uviferum) wood that was abundant in the area. The timber business accounts for most of the economy in Tortel to this day. For most of its history the village had only air and boat access; the road was constructed only in 2003, and connects Caleta Tortel with the Carretera Austral. Caleta Tortel consists mainly of stilt houses, typical of Chilotan architecture, built along the coast for several kilometers. There are no conventional streets - instead there are wooden walkways build with Guaitecas Cypress. The wooden walkways give the villag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Katalalixar National Reserve
Katalalixar National Reserve is a natural reserve located in an archipelago between Southern Patagonian Ice Field, and Northern Patagonian Ice Field in Aysén del General Carlos Ibáñez del Campo Region of Chile. The reserve was created in 1983 and has no infrastructure. It covers an area of within the Magellanic subpolar forests ecoregion and exhibits more biodiversity than other areas of southern Chile. This may appear contradictory, as the area is supposed to have been covered by the Patagonian Ice Sheet upright=1.4, Map showing the extent of the Patagonian Ice Sheet in the Strait of Magellan area during the last glacial period. Selected modern settlements are shown with yellow dots. Sea level was much lower than shown here. The Patagonian Ice S ... during the last glacial maximum. References National reserves of Chile Protected areas of Aysén Region Protected areas established in 1983 Magellanic subpolar forests {{SouthAm-protected-area-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bernardo O'Higgins National Park
Bernardo O'Higgins National Park () is the largest of the protected areas in Chile, covering an area of in both the Aysén and Magallanes and Antártica Chilena regions. Management of this and other national parks in Chile is entrusted to the '' Corporación Nacional Forestal'' (CONAF). The park is named after General Bernardo O'Higgins, the first head of state of the Republic of Chile. Los Glaciares National Park (Argentina) and Torres del Paine National Park are its neighbours to the east, Laguna San Rafael National Park is located to the north, the Alacalufes National Reserve to the southwest and the Katalalixar National Reserve to the northwest. History The earliest occupants of the area were the Alacaluf people. In 1830, the then-Captain Phillip Parker King on board HMS ''Beagle'' visited the Eyre Fjord. In June 2007, it was announced that between March and May 2007 all the water within a glacial lake located within the park had disappeared, leaving behind a 100- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Patagonian Ice Field
The Southern Patagonian Ice Field ( es, Hielo Continental or '), located at the Southern Patagonic Andes between Chile and Argentina, is the world's second largest contiguous extrapolar ice field. It is the bigger of two remnant parts of the Patagonian Ice Sheet, which covered all of southern Chile during the last glacial period, locally called the Llanquihue glaciation. Geography The Southern Patagonia Ice Field extends from parallels 48° 15′ S to 51° 30′ S for approximately , and has an approximate area of , of which 14,200 km2 belong to Chile and 2,600 km2 belong to Argentina. The ice mass feeds dozens of glaciers in the area, among which are the Upsala (765 km2), Viedma (978 km2) and Perito Moreno (258 km2) in the Los Glaciares National Park in Argentina, and the Pío XI Glacier or Bruggen Glacier (1,265 km2, the largest in area and longest in the southern hemisphere outside of Antarctica), O'Higgins (820 km2), G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jorge Montt Glacier
Jorge Montt Glacier is a tidewater glacier located in the Aisén Region of Chile, south of the town of Caleta Tortel. It lies at the north end of the Southern Patagonian Ice Field, within Bernardo O'Higgins National Park. The mouth of Pascua River is located in the vicinity of the glacier calving front. The total drainage area of the glacier is about . The glacier's ice is thinning most at low elevations, where air temperature is the highest. Ice thinning between 1975 and 2000 averaged per year over the entire glacier, and reached per year at the lowest elevations. The glacier calving front experienced a major retreat of in those 25 years as a result of rapid thinning. The glacier calves off icebergs into the Baker Channel. In 2000, NASA wrote: ''Conventional topographic data from the 1970s and 1990s were compared with data from NASA's February 2000 Shuttle Radar Topography Mission to measure changes in the volumes of the 63 largest glaciers in the region over time. The resea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
O'Higgins/San Martín Lake
The lake known as O'Higgins in Chile and San Martín in Argentina is located around coordinates in Patagonia, between the Aysén del General Carlos Ibáñez del Campo Region and the Santa Cruz Province. General information The lake has a surface area of , an elevation of above mean sea level, and a shoreline length of . Viewed from above, the lake consists of a series of finger-shaped flooded valleys, of which are in Chile and in Argentina, although sources differ on the precise split, presumably reflecting water level variability. The lake is the deepest in the Americas with a maximum depth of near O'Higgins Glacier, and its characteristic milky light-blue color comes from rock flour suspended in its waters. It is mainly fed by the Mayer River and other streams, and its outlet, the Pascua River, discharges water from the lake towards the Pacific Ocean at a rate of . The O'Higgins Glacier flows eastwards towards the lake, as does the Chico Glacier. Both of these glacie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chile
Chile, officially the Republic of Chile, is a country in the western part of South America. It is the southernmost country in the world, and the closest to Antarctica, occupying a long and narrow strip of land between the Andes to the east and the Pacific Ocean to the west. Chile covers an area of , with a population of 17.5 million as of 2017. It shares land borders with Peru to the north, Bolivia to the north-east, Argentina to the east, and the Drake Passage in the far south. Chile also controls the Pacific islands of Juan Fernández, Isla Salas y Gómez, Desventuradas, and Easter Island in Oceania. It also claims about of Antarctica under the Chilean Antarctic Territory. The country's capital and largest city is Santiago, and its national language is Spanish. Spain conquered and colonized the region in the mid-16th century, replacing Inca rule, but failing to conquer the independent Mapuche who inhabited what is now south-central Chile. In 1818, after declaring ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Messier Channel
Messier Channel is a channel located in Patagonia, Chile. It trends north–south between Wellington Island and other Pacific islands and the continent, and is bounded on the north by the Gulf of Penas. Southward the name of this inside passage changes first to ''Angostura Inglesa'' (English Narrows) and then to '' Paso del Indio''. The channel is named after Charles Messier, who was a French astronomer. It is a fjord in the Scandinavian sense of the word. A depth of 1,358 m has been measured in the north part of this channel, making it one of the deepest fjords in the world. Messier Channel is surrounded by the Bernardo O'Higgins National Park and the Katalalixar National Reserve. The Fallos- Ladrillero-Picton Channel combination is an optional route to the Messier-Grappler-Wide Channels route between the Golfo de Penas and the Trinidad Channel. Just north of Angostura Inglesa (English Narrows), is the wreck of MV ''Capitán Leonidas'', a small freighter that ran aground ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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