The Cascade Range or Cascades is a major mountain range of western North America , extending from southern British Columbia through Washington and Oregon to Northern California . It includes both non-volcanic mountains, such as many of those in the North Cascades , and the notable volcanoes known as the High Cascades . The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains . The highest peak in the range is Mount Rainier in Washington at 14,411 feet (4,392 m).
96-679: Baker City Tower or Baker Tower (originally Baker Community Hotel , then Baker Hotel ) is the tallest building east of the Cascade Range in the U.S. state of Oregon , located in Baker City . It was constructed in 1929 in the Art Deco style and is nine stories high. It is part of the Baker Historic District and listed in the National Register of Historic Places. It was designed by
192-578: A magnitude-8.8 earthquake struck central Chile on February 27, 2010 , the Puyehue-Cordón Caulle volcano erupted in 2011 , and a M8.2 earthquake struck northern Chile on April 1, 2014 . The main shock was preceded by a number of moderate to large shocks and was followed by a large number of moderate to very large aftershocks, including a magnitude-7.6 event on April 2. Bolivia hosts active and extinct volcanoes across its territory. The active volcanoes are located in western Bolivia where they make up
288-480: A chain of volcanoes (the Cascade Volcanic Arc) above the subduction zone. Soil conditions for farming are generally good, especially downwind of volcanoes . This is largely because volcanic rocks are often rich in potassium -bearing minerals such as orthoclase , and erode relatively easily. Volcanic debris, especially lahars , also helps to spread mineral-rich volcanic material, and the storage of water in
384-734: A few wolf packs returning from Canada live in the Cascades. Fewer than 50 grizzly bears reside in the Cascades of Canada and Washington. Ring of Fire The Ring of Fire (also known as the Pacific Ring of Fire , the Rim of Fire , the Girdle of Fire or the Circum-Pacific belt ) is a tectonic belt of volcanoes and earthquakes . It is about 40,000 km (25,000 mi) long and up to about 500 km (310 mi) wide, and surrounds most of
480-583: A few strikingly large volcanoes, like Mount Hood and Mount St. Helens, that dominate the landscape. The Cascade volcanoes define the Pacific Northwest section of the Ring of Fire , an array of volcanoes that rim the Pacific Ocean. The Ring of Fire is also known for its frequent earthquakes. The volcanoes and earthquakes arise from a common source: subduction , where the dense Juan de Fuca Plate plunges beneath
576-421: A foreclosure auction. Its owner since 1961, A.C Lighthall, had sold it twice to owners who continued to operate it as a hotel, but both lost it by failing to make the payments. Lighthall then closed it on January 1, 1969. It remained vacant for almost two years, then was resold to a local investor who believed it was the "largest and finest building in all Baker". It was converted to restaurant/retail/office usage on
672-600: A fur trader with the North West Company , seeking a viable route across the mountains, explored and crossed the northern Cascades between Fort Okanogan and Puget Sound. His report of the journey is vague about the route taken. He followed the lower Methow River into the mountains. He might have used Cascade Pass to reach the Skagit River . Ross was the first European-American to explore the Methow River area and likely
768-436: A lava flow. The last major eruption of Calbuco, in 1961, sent ash columns 12–15 km (7.5–9.3 mi) high and produced plumes that dispersed mainly to the southeast and two lava flows were also emitted. A minor, four-hour eruption happened on August 26, 1972. Strong fumarolic emission from the main crater was observed on August 12, 1996. Lonquimay is a stratovolocano of late-Pleistocene to dominantly Holocene age, with
864-693: A traveler passes through the Cascade Range, the climate first gets colder, then warmer and drier east of the crest. Most of the Cascades' lower and middle elevations are covered in coniferous forest ; the higher altitudes have extensive meadows as well as alpine tundra and glaciers . The southern part of the Cascades are within the California Floristic Province , an area of high biodiversity . Silver fir predominates above 2500 ft, while there are moors , meadows , and mountain hemlock / subalpine fir groves from 4500 to 6000 ft on
960-554: Is a major late Cenozoic volcanic province. Sabancaya is an active 5,976-metre (19,606 ft) stratovolcano in the Andes of southern Peru , about 100 km (60 mi) northwest of Arequipa . It is the most active volcano in Peru, with an ongoing eruption that started in 2016. Ubinas is another active volcano of 5,672-metre (18,609 ft) in southern Peru; its most recent eruption occurred in 2019. Volcanoes in Peru are monitored by
1056-461: Is a part of the American Cordillera , a nearly continuous chain of mountain ranges (cordillera) that form the western "backbone" of North, Central , and South America . The Cascades are home to many national parks and protected areas, including North Cascades National Park , Mount Rainier National Park , Crater Lake National Park , and Lassen Volcanic National Park . The northern half of
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#17328772057351152-474: Is a stratovolcano and the most active volcano of the northern Chilean Andes. The largest eruption of Lascar took place about 26,500 years ago, and following the eruption of the Tumbres scoria flow about 9,000 years ago, activity shifted back to the eastern edifice, where three overlapping craters were formed. Frequent small-to-moderate explosive eruptions have been recorded from Lascar in historical time since
1248-561: Is a stratovolcano in southern Chile, located southeast of Llanquihue Lake and northwest of Chapo Lake , in Los Lagos Region . The volcano and the surrounding area are protected within Llanquihue National Reserve . It is a very explosive andesite volcano that underwent edifice collapse in the late Pleistocene , producing a volcanic debris avalanche that reached the lake. At least nine eruptions occurred since 1837, with
1344-630: Is a stratovolcano located in the Antofagasta Region of Chile, immediately north of Cerro Miscanti . Laguna Lejía lies to the north of the volcano and has been dormant for at least 10,000 years, but is now showing signs of life. A January 6, 2002, nighttime thermal infrared image from ASTER revealed a hot spot in the summit crater, as well as several others along the upper flanks of the volcano's edifice, indicating new volcanic activity. Examination of an earlier nighttime thermal infrared image from May 24, 2000, showed no such hot spots. Calbuco
1440-528: Is an arid plateau that was largely formed 17 to 14 million years ago by the many flows of the Columbia River Basalt Group . Together, these sequences of fluid volcanic rock form the 200,000-square-mile (520,000 km ) Columbia Plateau in eastern Washington, Oregon, and parts of western Idaho. The Columbia River Gorge is the only major break of the range in the United States. When
1536-736: Is an interpretive site there now at "The End of The Oregon Trail". The road was constructed as a toll road – $ 5 per wagon – and was very successful. In addition, the Applegate Trail was created to allow settlers to avoid rafting down the Columbia River. The Trail used the path of the California Trail to north-central Nevada . From there, the Trail headed northwest into northern California, and continued northwest towards today's Ashland, Oregon . From there, settlers would head north along
1632-792: Is being subducted beneath the Aleutian Islands arc. Farther west, the Pacific plate is being subducted at the Kamchatka Peninsula and Kuril arcs. Farther south, at Japan, Taiwan and the Philippines, the Philippine Plate is being subducted beneath the Eurasian plate. The southwest section of the Ring of Fire is more complex, with a number of smaller tectonic plates in collision with the Pacific plate at
1728-681: Is great local relief . The southern part of the Canadian Cascades, particularly the Skagit Range , is geologically and topographically similar to the North Cascades, while the northern and northeastern parts are less glaciated and more plateau-like, resembling nearby areas of the Thompson Plateau . The range is near the Pacific Ocean and in the region's prevailing westerly winds , so it receives significant rain and snowfall, especially on
1824-577: Is known as the North Cascades in the United States but is formally named the Cascade Mountains north of the Canada–United States border , reaching to the northern extremity of the Cascades at Lytton Mountain . Overall, the North Cascades and Canadian Cascades are extremely rugged; even the lesser peaks are steep and glaciated, and valleys are quite low relative to peaks and ridges, so there
1920-607: Is not related to subduction; therefore, they are not part of the Ring of Fire. The world's highest active volcano is Ojos del Salado (6,893 m or 22,615 ft), which is in the Andes Mountains section of the Ring of Fire. It forms part of the border between Argentina and Chile and it last erupted in AD 750. Another Ring of Fire Andean volcano on the Argentina-Chile border is Llullaillaco (6,739 m or 22,110 ft), which
2016-458: Is not uncommon for some places in the Cascades to have over 500 inches (1,300 cm) of annual snow accumulation, such as at Lake Helen , near Lassen Peak. Most of the High Cascades are therefore white with snow and ice year-round. The western slopes are densely covered with Douglas-fir ( Pseudotsuga menziesii ), western hemlock ( Tsuga heterophylla ) and red alder ( Alnus rubra ), while
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#17328772057352112-464: Is now eastern China. The Pacific plate came into existence in the Early Jurassic about 190 million years ago, far from the margins of the then Paleo-Pacific Ocean. Until the Pacific plate grew large enough to reach the margins of the ocean basin, other older plates were subducted ahead of it at the ocean basin margins. For example, subduction has been occurring at the coast of South America since
2208-490: Is subducted in the western Pacific, with steeper angles of slab descent. This variation affects, for example, the location of volcanoes relative to the ocean trench, lava composition, type and severity of earthquakes, sediment accretion , and the amount of compression or tension. A spectrum of subduction zones exists between the Chilean and Mariana end members. Oceanic trenches are the topographic expression of subduction zones on
2304-559: Is the world's highest historically active volcano, last erupting in 1877. Chile has experienced numerous volcanic eruptions from about 90 volcanoes during the Holocene Epoch. Villarrica is one of Chile's most active volcanoes, rising above the lake and town of the same name. It is the westernmost of three large stratovolcanoes that trend perpendicular to the Andes along the Gastre Fault . Villarrica, along with Quetrupillán and
2400-463: Is topped with an eight-sided cupola, with a matching octagonal hip roof with a flagpole. The cupola was designed as an observation center, from which the Powder River Basin and Elkhorn Mountains can be seen. The original windows were double-hung wood sashes. Decorative elements included concrete garlands and scrolls, pairs of 4-foot (1.2 m) terra cotta eagles at the entrances, and urns at
2496-484: The Baker River is dammed to form Lake Shannon and Baker Lake . The Cascades harbor a largely-untapped potential for geothermal power . The U.S. Geological Survey Geothermal Research Program has been investigating this potential. Some of this energy is already being used in places like Klamath Falls, Oregon , where volcanic steam is used to heat public buildings. The highest recorded underground temperature found in
2592-601: The Cascades Rapids in the Columbia River Gorge, a feature on the river now submerged beneath the Bonneville Reservoir . Before long, the great white-capped mountains that loomed above the rapids were called the "mountains by the cascades" and later simply as the "Cascades". The earliest attested use of the name "Cascade Range" is in the writings of botanist David Douglas in 1825. In 1814, Alexander Ross ,
2688-746: The Cordillera Occidental , the western limit of the Altiplano plateau. Some of the active volcanoes are international mountains shared with Chile . All Cenozoic volcanoes of Bolivia are part of the Central Volcanic Zone (CVZ) of the Andean Volcanic Belt that results due to processes involved in the subduction of the Nazca plate under the South American plate . The Central Volcanic Zone
2784-559: The Great Depression without losses to the owners of their investment. It was near default on its mortgage obligations and petitioned for bankruptcy reorganization in 1936, but bond-holders rejected the plan. The debt was refinanced and reduced, in part with a loan from the Reconstruction Finance Corporation . Interest payments were reduced by 50 percent and the hotel remained solvent. National conventions were held in
2880-654: The Hudson's Bay Company (HBC) at Fort Vancouver near today's Portland, Oregon . From this base HBC trapping parties traveled throughout the Cascades in search of beaver and other fur-bearing animals. For example, using what became known as the Siskiyou Trail , Hudson's Bay Company trappers were the first non-natives to explore the southern Cascades in the 1820s and 1830s, establishing trails which passed near Crater Lake , Mount McLoughlin , Medicine Lake Volcano , Mount Shasta , and Lassen Peak. The course of political history in
2976-556: The Jurassic Period more than 145 million years ago, and remnants of Jurassic and Cretaceous volcanic arcs are preserved there. At about 120 to 115 million years ago, the Farallon plate was subducting under South America, North America and north-east Asia while the Izanagi plate was subducting under east Asia. By 85 to 70 million years ago, the Izanagi plate had moved north-eastwards and
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3072-521: The Lushootseed name for Mount Rainier, and "Louwala-Clough", meaning "smoking mountain" for Mount St. Helens. In early 1792, British navigator George Vancouver explored Puget Sound and gave English names to the high mountains he saw. Mount Baker was named for Vancouver's third lieutenant, Joseph Baker , although the first European to see it was Manuel Quimper , who named it la gran montaña del Carmelo ("Great Mount Carmel ") in 1790. Mount Rainier
3168-527: The Mariana Islands , the Philippines , eastern Indonesia , Papua New Guinea , Tonga , and New Zealand; this part of the Ring excludes Australia , because that landmass lies in the center of its tectonic plate far from subduction zones. If a tectonic plate's oceanic lithosphere is subducted beneath oceanic lithosphere of another plate, a volcanic island arc is created at the subduction zone. An example in
3264-515: The North American Plate . As the oceanic slab sinks deep into the Earth's interior beneath the continental plate, high temperatures and pressures allow water molecules locked in the minerals of solid rock to escape. The water vapor rises into the pliable mantle above the subducting plate, causing some of the mantle to melt. This newly formed magma rises toward the Earth's surface to erupt, forming
3360-810: The Pacific Crest Trail follows the range. The Cascades extend northward from Lassen Peak (also known as Mount Lassen) in northern California to the confluence of the Nicola and Thompson rivers in British Columbia . The Fraser River separates the Cascades from the Coast Mountains in Canada, as does the Willamette Valley from the upper portion of the Oregon Coast Range . The highest volcanoes of
3456-663: The Pacific Northwest saw the spine of the Cascade Range being proposed as a boundary settlement during the Oregon Dispute of 1846. The United States rejected the proposal and insisted on the 49th parallel north , which cuts across the range just north of Mount Baker. Throughout the period of dispute and up to the creation of the Crown Colony of British Columbia in 1858, the Hudson's Bay Company's York Factory Express route, as well
3552-457: The Pacific Ocean . The Ring of Fire contains between 750 and 915 active or dormant volcanoes, around two-thirds of the world total. The exact number of volcanoes within the Ring of Fire depends on which regions are included. About 90% of the world's earthquakes, including most of its largest, occur within the belt. The Ring of Fire is not a single geological structure. It was created by
3648-794: The railway roadbed and the Othello Tunnels , now decommissioned, are popular tourist recreation destinations for hiking and bicycling. The pass is used by the Coquihalla Highway , a government megaproject built as part of the Expo 86 spending boom of the 1980s, which is now the main route from the Coast to the British Columbia interior. Traffic formerly went via the Fraser Canyon , to the west, or via Allison Pass and Manning Park along Highway 3 to
3744-830: The subduction of different tectonic plates at convergent boundaries around the Pacific Ocean. These include: the Antarctic , Nazca and Cocos plates subducting beneath the South American plate ; the Pacific and Juan de Fuca plates beneath the North American plate ; the Philippine Plate beneath the Eurasian plate ; and a complex boundary between the Pacific and Australian plate . The interactions at these plate boundaries have formed oceanic trenches , volcanic arcs , back-arc basins and volcanic belts . The inclusion of some areas in
3840-405: The 2001 renovation, the building was configured with retail and office space on floors one through five, with the upper floors residential condominiums . Cast and crew of the 1969 musical film Paint Your Wagon , starring Lee Marvin and Clint Eastwood , stayed at the hotel during filming which occurred near Baker City. The hotel was nearly fully booked just before its permanent closure after
3936-441: The Alpide belt). Some geologists include the Antarctic Peninsula and the South Shetland Islands in the Ring of Fire, other geologists exclude these areas. The rest of Antarctica is excluded because the volcanism there is not related to subduction. The Ring of Fire does not extend across the southern Pacific Ocean from New Zealand to the Antarctic Peninsula or from New Zealand to the southern tip of South America because
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4032-552: The Cascades began to rise 7 million years ago in the late Miocene , the Columbia River drained the relatively low Columbia Plateau. As the range grew, erosion from the Columbia River was able to keep pace, carving out the gorge and major pass seen today. The gorge also exposes uplifted and warped layers of basalt from the plateau. Before European exploration, First Nations tribes named many peaks, including "Wy'east" for Mount Hood , "Seekseekqua" for Mount Jefferson (Oregon) , "M'laiksini Yaina" for Mount McLoughlin , "Tahoma",
4128-414: The Cascades, known as the High Cascades, dominate their surroundings, often standing twice the height of the nearby mountains. They often have a visual height (height above nearby crestlines) of one mile or more. The highest peaks, such as the 14,411-foot (4,392 m) Mount Rainier, dominate their surroundings for 50 to 100 miles (80 to 161 km). The northern part of the range, north of Mount Rainier,
4224-443: The Chilean part of Lanín , are protected within Villarrica National Park . Villarrica, with its lava of basaltic-andesitic composition, is one of only five volcanoes worldwide known to have an active lava lake within its crater. The volcano usually generates strombolian eruptions , with ejection of incandescent pyroclasts and lava flows. Melting of snow and glacier ice , as well as rainfall, often causes lahars , such as during
4320-422: The Gulf of California and due partly to the San Andreas Fault (a non-volcanic transform boundary ). Another North American gap in subduction-related volcanic activity occurs in northern British Columbia, Yukon and south-east Alaska, where volcanism is caused by intraplate continental rifting . The four largest volcanic eruptions on Earth in the Holocene Epoch (the last 11,700 years) occurred at volcanoes in
4416-550: The Holocene epoch all occurred at volcanoes in the Ring of Fire. Most of Earth's active volcanoes with summits above sea level are located in the Ring of Fire. Many of these subaerial volcanoes are stratovolcanoes (e.g. Mount St. Helens ), formed by explosive eruptions of tephra alternating with effusive eruptions of lava flows. Lavas at the Ring of Fire's stratovolcanoes are mainly andesite and basaltic andesite but dacite , rhyolite , basalt and some other rarer types also occur. Other types of volcano are also found in
4512-417: The Kula and Farallon plates had been subducted and the Pacific plate was subducting around its rim in a configuration closely resembling the outline of the present-day Ring of Fire. The eastern parts of the Ring of Fire result from the collision of a few relatively large plates. The western parts of the Ring are more complex, with a number of large and small tectonic plates in collision. In South America,
4608-445: The Portland office of architectural firm Tourtellotte & Hummel . The general contractor was John Almeter of Portland and the roofing contractor was Cook & Emele of Baker City. An earlier building on the site housed the first livery stable in Baker, but it was demolished to make way for the hotel. The building is constructed of concrete and has its main entrance on Main Street, with an auxiliary entrance on Auburn Avenue. The roof
4704-403: The Ring of Fire at some parts of the Pacific coast of the Americas. In some places, the gaps are thought to be caused by flat slab subduction ; examples are the three gaps between the four sections of the Andean Volcanic Belt in South America. In North America, there is a gap in subduction-related volcanic activity in northern Mexico and southern California, due partly to a divergent boundary in
4800-411: The Ring of Fire is the Mariana Arc in the western Pacific Ocean. If, however, oceanic lithosphere is subducted under continental lithosphere, then a volcanic continental arc forms; a Ring of Fire example is the coast of Chile. The steepness of the descending plate at a subduction zone depends on the age of the oceanic lithosphere that is being subducted. The older the oceanic lithosphere being subducted,
4896-429: The Ring of Fire is the result of the Antarctic plate , the Nazca plate and the Cocos plate being subducted beneath the South American plate . In Central America , the Cocos plate is being subducted beneath the Caribbean plate . A portion of the Pacific plate and the small Juan de Fuca plate are being subducted beneath the North American plate . Along the northern portion, the northwestward-moving Pacific plate
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#17328772057354992-411: The Ring of Fire volcanoes as follows: "They [the Japanese Islands] are in the line of that immense circle of volcanic development which surrounds the shores of the Pacific from Tierra del Fuego around to the Moluccas ." ( Narrative of the Expedition of an American Squadron to the China Seas and Japan, 1852–54 . ) An article appeared in Scientific American in 1878 with the title "The Ring of Fire, and
5088-423: The Ring of Fire, such as subaerial shield volcanoes (e.g. Plosky Tolbachik ), and submarine seamounts (e.g. Monowai ). From Ancient Greek and Roman times until the late 18th century, volcanoes were associated with fire, based on the ancient belief that volcanoes were caused by fires burning within the Earth. This historical link between volcanoes and fire is preserved in the name of the Ring of Fire, despite
5184-426: The Ring of Fire, such as the Antarctic Peninsula and western Indonesia, is disputed. The Ring of Fire has existed for more than 35 million years but subduction has existed for much longer in some parts of the Ring; many older extinct volcanoes are located within the Ring. More than 350 of the Ring of Fire's volcanoes have been active in historical times , while the four largest volcanic eruptions on Earth in
5280-465: The Ring of Fire. The next most seismically active region (5–6% of earthquakes and some of the world's largest earthquakes) is the Alpide belt, which extends from central Indonesia to the northern Atlantic Ocean via the Himalayas and southern Europe. From 1900 to the end of 2020, most earthquakes of magnitude M w ≥ 8.0 occurred in the Ring of Fire. They are presumed to have been megathrust earthquakes at subduction zones, including four of
5376-421: The Ring of Fire. They are the eruptions at Fisher Caldera (Alaska, 8700 BC ), Kurile Lake (Kamchatka, 6450 BC), Kikai Caldera (Japan, 5480 BC) and Mount Mazama (Oregon, 5677 BC). More broadly, twenty of the twenty-five largest volcanic eruptions on Earth in this time interval occurred at Ring of Fire volcanoes. About 90% of the world's earthquakes and most of the world's largest earthquakes occur along
5472-445: The South Shetland subduction zone. The Antarctic Peninsula (Graham Land) is also sometimes included in the Ring. Volcanoes south of the Antarctic Circle (e.g. the volcanoes of Victoria Land including Mount Erebus , and the volcanoes of Mary Byrd Land ) are not related to subduction; therefore, they are not part of the Ring of Fire. The Balleny Islands , located between Antarctica and New Zealand, are volcanic but their volcanism
5568-409: The Volcanic Peaks of the West Coast of the United States", which outlined the phenomenon of volcanic activity around the boundaries of the Pacific. Early explicit references to volcanoes forming a "ring of fire" around the Pacific Ocean also include Alexander P. Livingstone's book "Complete Story of San Francisco's Terrible Calamity of Earthquake and Fire" , published in 1906, in which he describes "...
5664-559: The central parts of the Pacific Basin, for example the Hawaiian Islands , are very far from subduction zones and they are not part of the Ring of Fire. The Ring of Fire has existed for more than 35 million years. In some parts of the Ring of Fire, subduction has been occurring for much longer. The current configuration of the Pacific Ring of Fire has been created by the development of the present-day subduction zones, initially (by about 115 million years ago) in South America, North America and Asia. As plate configurations gradually changed,
5760-538: The corners of the eighth floor. The hotel was built to serve long-distance automobile travelers who were becoming common in the 1920s, and it did not need to be located near the railroad tracks. It was planned as a community hotel, both a community asset and an investment. Local ownership meant that the community was "financially and emotionally involved in the project's success". The hotel was originally owned by 300 local residents who purchased stock shares, priced affordably to be within reach of many residents, and survived
5856-432: The current subduction zones of Indonesia and New Guinea were created (about 70 million years ago), followed finally by the New Zealand subduction zone (about 35 million years ago). Along the coast of east Asia, during the Late Triassic about 210 million years ago, subduction of the Izanagi plate (the Paleo-Pacific plate) was occurring, and this continued in the Jurassic , producing volcanic belts, for example, in what
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#17328772057355952-414: The drier eastern slopes feature mostly ponderosa pine ( Pinus ponderosa ), with some western larch ( Larix occidentalis ), mountain hemlock ( Tsuga mertensiana ) and subalpine fir ( Abies lasiocarpa ) and subalpine larch ( Larix lyallii ) at higher elevations. Annual rainfall is as low as 9 inches (230 mm) on the eastern foothills due to a rain shadow effect. Beyond the eastern foothills
6048-439: The early 1840s, at first only marginally. Following the Oregon Treaty the inward flux of migration from the Oregon Trail intensified and the passes and back-valleys of what is now the state of Washington were explored and populated, and it was not long after that railways followed. Despite its being traversed by several major freeways and rail lines, and its lower flanks subjected to major logging in recent decades, large parts of
6144-545: The eruptions of 1964 and 1971. A two-kilometre-wide ( 1 + 1 ⁄ 4 mi) postglacial caldera is located at the base of the presently active dominantly basaltic-to-andesitic cone at the northwest margin of the Pleistocene caldera. About 25 scoria cones dot Villarica's flanks. Plinian eruptions and pyroclastic flows have been produced during the Holocene from this dominantly basaltic volcano, but historical eruptions have consisted of largely mild-to-moderate explosive activity with occasional lava effusion. Lahars from
6240-477: The established Siskiyou Trail into the Willamette Valley . With the exception of the 1915 eruption of remote Lassen Peak in Northern California, the range was quiet for more than a century. Then, on May 18, 1980, the dramatic eruption of Mount St. Helens shattered the quiet and brought the world's attention to the range. Geologists were also concerned that the St. Helens eruption was a sign that long-dormant Cascade volcanoes might become active once more, as in
6336-442: The fact that volcanoes do not burn the Earth with fire. The existence of a belt of volcanic activity around the Pacific Ocean was known in the early 19th century; for example, in 1825 the pioneering volcanologist G. P. Scrope described the chains of volcanoes around the Pacific Ocean's rim in his book Considerations on Volcanos [ sic ]. Three decades later, a book about the Perry Expedition to Japan commented on
6432-403: The first to explore the Stehekin River and Bridge Creek region. Due to the difficulty of crossing the northern Cascades and the paucity of beaver, fur-trading companies made only a few explorations into the mountains north of the Columbia River after Ross. Exploration and settlement of the Cascades region by Europeans and Americans was accelerated by the establishment of a major trading post of
6528-564: The first, second, ninth and tenth floors and apartments on other floors in 1972. Eleven rooms on the second floor remained nightly rental hotel rooms. The remainder of the rooms were made into one or two bedroom apartments. In 1992, the building was "run-down" and a $ 1.2 million restoration was performed to convert it to senior housing. A 1999 renovation brought a new elevator, HVAC system, fire sprinklers, windows. Later work brought restoration of art deco detailing and fiber-optic wiring enabling it to be marketed as high-tech office space. After
6624-458: The floor of the oceans. Oceanic trenches associated with the Ring of Fire's subduction zones are: Subduction zones around the Pacific Ocean do not form a complete ring. Where subduction zones are absent, there are corresponding gaps in subduction-related volcanic belts in the Ring of Fire. In some gaps there is no volcanic activity; in other gaps, volcanic activity does occur but it is caused by processes not related to subduction. There are gaps in
6720-421: The form of snow and ice is also important for agriculture. The snow-capped mountains, such as Mt. Hood and Mt. Bachelor , are used as ski resorts in the late winter, while in the summer they become popular hiking and mountaineering locations. Much of their meltwater eventually flows into reservoirs, where it is used for recreation, while its potential energy is captured to generate hydroelectric power before
6816-482: The glacier-covered volcanoes have damaged towns on its flanks. The Llaima Volcano is one of the largest and most active volcanoes in Chile. It is situated 82 km (51 mi) northeast of Temuco and 663 km (412 mi) southeast of Santiago , within the borders of Conguillío National Park . Llaima's activity has been documented since the 17th century, and consists of several separate episodes of moderate explosive eruptions with occasional lava flows. Lascar
6912-440: The great ring of fire which circles round the whole surface of the Pacific Ocean.". In 1912, geologist Patrick Marshall introduced the term " Andesite Line " to mark a boundary between islands in the southwest Pacific, which differ in volcano structure and lava types. The concept was later extended to other parts of the Pacific Ocean. The Andesite Line and the Ring of Fire closely match in terms of location. The development of
7008-406: The hotel, which had a reputation as "the finest place to dine in eastern Oregon". The original stockholders sold the building in 1946 after more than 60 percent of them agreed to a sale, at which time the word "community" was dropped from the name. The building was originally an 82-room hotel and operated as one from its opening on August 24, 1929, until the late 1960s before being closed and sold in
7104-521: The intersection of the Ring of Fire and the Alpide belt (which is the Earth's other very long subduction-related volcanic and earthquake zone, also known as the Mediterranean–Indonesian volcanic belt, running east–west through southern Asia and southern Europe). Some geologists include all of Indonesia in the Ring of Fire; many geologists exclude Indonesia's western islands (which they include in
7200-565: The latest one in 1972. One of the largest historical eruptions in southern Chile took place there in 1893–1894. Violent eruptions ejected 30 cm (12 in) bombs to distances of 8 km (5.0 mi) from the crater, accompanied by voluminous hot lahars. Strong explosions occurred in April 1917, and a lava dome formed in the crater accompanied by hot lahars. Another short explosive eruption in January 1929 also included an apparent pyroclastic flow and
7296-469: The mid-19th century, along with periodic larger eruptions that produced ash and tephra fall up to hundreds of kilometers away from the volcano. The largest eruption of Lascar in recent history took place in 1993, producing pyroclastic flows as far as 8.5 km (5 mi) northwest of the summit and ash fall in Buenos Aires , Argentina, more than 1,600 km (1,000 mi) to the southeast. Chiliques
7392-584: The most powerful earthquakes on Earth since modern seismological measuring equipment and magnitude measurement scales were introduced in the 1930s: Some geologists include the volcanoes of the South Shetland Islands , off the northern tip of the Antarctic Peninsula, as part of the Ring of Fire. These volcanoes, e.g. Deception Island , are due to rifting in the Bransfield back-arc basin close to
7488-489: The mountain range which contained these peaks. He referred to it simply as the "eastern snowy range". Earlier Spanish explorers called it Sierra Nevada , meaning "snowy mountains". In 1805, the Lewis and Clark Expedition passed through the Cascades on the Columbia River, which for many years was the only practical way to pass that part of the range. They were the first non-indigenous people to see Mount Adams , but they thought it
7584-592: The movie production ended. Cascade Range The Cascades are part of the Pacific Ocean 's Ring of Fire , the ring of volcanoes and associated mountains around the Pacific Ocean. All of the eruptions in the contiguous United States over the last 200 years have been from the Cascade Volcanoes . The two most recent were Lassen Peak from 1914 to 1921 and a major eruption of Mount St. Helens in 1980 . Minor eruptions of Mount St. Helens have also occurred since, most recently from 2004 to 2008. The Cascade Range
7680-734: The older Hudson's Bay Company Brigade Trail from the Canyon to the Interior, the Dewdney Trail, and older routes which connected east to the Similkameen and Okanagan valleys. The southern mainline of the Canadian Pacific Railway penetrated the range via the passes of the Coquihalla River , along one of the steepest and snowiest routes in the entire Pacific Cordillera . Near Hope, B.C. ,
7776-578: The period from 1800 to 1857 when a total of eight erupted. None have erupted since St. Helens, but precautions are being taken nevertheless, such as the Cascades Volcano Observatory and Mount Rainier Volcano Lahar Warning System in Pierce County, Washington . The Cascade Range is made up of a band of thousands of very small, short-lived volcanoes that have built a platform of lava and volcanic debris. Rising above this volcanic platform are
7872-466: The range is 510 °F (266 °C) at 3,075 feet (937 m) below Newberry Volcano 's caldera floor. Forests of large, coniferous trees ( western red cedars , Douglas-firs, western hemlocks, firs , pines , spruces , and others) dominate most of the Cascade Range. Cool, wet winters and warm, dry summers (largely a result of oceanic influence) favor evergreen species, whereas mild temperatures and rich soils promote fast and prolonged growth. As
7968-485: The range remain intense and forbidding alpine wilderness. Much of the northern half of the Cascades, from Rainier north, have been preserved by U.S. national or British Columbia provincial parks (such as E.C. Manning Provincial Park ), or other forms of protected area. The Canadian side of the range has a history that includes the Fraser Canyon Gold Rush of 1858–60 and its famous Cariboo Road , as well as
8064-511: The route of fur brigades, followed the Okanogan River along the east edge of the Cascades and the Columbia River through the range. Passes across the range were not well known and little used. Naches Pass was used for driving cattle and horses to Fort Nisqually . Yakima Pass was also used by the Hudson's Bay Company. American settlement of the flanks of the Coast Range did not occur until
8160-469: The shape of a truncated cone. The cone is largely andesitic, though basaltic and dacitic rocks are present. It is located in La Araucanía Region of Chile , immediately southeast of Tolhuaca volcano. Sierra Nevada and Llaima are their neighbors to the south. The snow-capped volcano lies within the protected area Malalcahuello-Nalcas . The volcano last erupted in 1988, ending in 1990. The VEI
8256-667: The south, near the border. The Barlow Road was the first established land path for U.S. settlers through the Cascade Range in 1845, and formed the final overland link for the Oregon Trail (previously, settlers had to raft down the treacherous rapids of the Columbia River). The Road left the Columbia at what is now Hood River and passed along the south side of Mount Hood at what is now Government Camp , terminating in Oregon City. There
8352-497: The steeper the angle of descent of the subducted slab. As the Pacific's mid-ocean ridges , which are the source of its oceanic lithosphere, are not actually in the middle of the ocean but located much closer to South America than to Asia, the oceanic lithosphere consumed at the South American subduction zones is younger and therefore subduction occurs at the South American coast at a relatively shallow angle. Older oceanic lithosphere
8448-690: The submarine plate boundaries in this part of the Pacific Ocean (the Pacific–Antarctic Ridge , the East Pacific Rise and the Chile Ridge ) are divergent instead of convergent. Although some volcanism occurs in this region, it is not related to subduction. Some geologists include the Izu Islands , the Bonin Islands , and the Mariana Islands , other geologists exclude them. Volcanoes in
8544-447: The theory of plate tectonics since the early 1960s has provided the current understanding and explanation of the global distribution of volcanoes and earthquakes, including those in the Ring of Fire. There is consensus among geologists about most of the regions which are included in the Ring of Fire. There are, however, a few regions on which there is no universal agreement. (See: § Distribution of volcanoes ). Indonesia lies at
8640-450: The water is used to irrigate crops. Because of the abundance of powerful streams, many of the major westward-draining rivers of the Cascades have been dammed to provide hydroelectric power . One of these, Ross Dam on the Skagit River , retains a reservoir which spans the border southeast of Hope, British Columbia , extending 2 miles (3.2 km) into Canada. At the foot of the southeast flank of Mount Baker, at Concrete, Washington ,
8736-471: The west side. The treeline is at ~6000 feet. On the east side, subalpine forests of larch trees grade to pine and interior fir forests below 4200 ft, which grade to ponderosa below 2500 ft, which in turn grades to semidesert scrub near sea level. Above 7500 ft, the landscape is barren with either no plants or only moss and lichen . Black bears , coyotes , bobcats , cougars , beavers , deer , elk , moose , mountain goats and
8832-524: The western slopes due to orographic lift , with annual snow accumulations of up to 1,000 inches (2,500 cm) (= 83 feet (25 m)) in some areas. Mount Baker in Washington recorded a national record single-season snowfall in the winter of 1998–99 with 1,140 inches (2,900 cm) (= 95 feet (29 m)). Before that year, Mount Rainier held the American record for snow accumulation at Paradise in 1978. It
8928-581: Was 3. The eruption was from a flank vent and involved lava flows and explosive eruptions. Some fatalities occurred. The volcanoes in Chile are monitored by the National Geology and Mining Service (SERNAGEOMIN) Earthquake activity in Chile is related to subduction of the Nazca plate to the east. Chile notably holds the record for the largest earthquake ever recorded, the 1960 Valdivia earthquake . More recently,
9024-457: Was Mount St. Helens. When they later saw Mount St. Helens they thought it was Mount Rainier. On their return trip, Lewis and Clark spotted a high but distant snowy pinnacle that they named for the sponsor of the expedition, U.S. President Thomas Jefferson . Lewis and Clark called the Cascade Range the "Western Mountains". The Lewis and Clark expedition, and the many settlers and traders that followed, met their last obstacle to their journey at
9120-555: Was named after Admiral Peter Rainier . Later in 1792, Vancouver had his lieutenant William Robert Broughton explore the lower Columbia River . He named Mount Hood after Lord Samuel Hood , an admiral of the Royal Navy . Mount St. Helens was sighted by Vancouver in May 1792, from near the mouth of the Columbia River. It was named for Alleyne FitzHerbert, 1st Baron St Helens , a British diplomat. Vancouver's expedition did not, however, name
9216-525: Was subducting under east Asia and North America, while the Farallon plate was subducting under South America and the Pacific plate was subducting under east Asia. About 70 to 65 million years ago, the Farallon plate was subducting under South America, the Kula plate was subducting under North America and north-east Asia, and the Pacific plate was subducting under east Asia and Papua New Guinea. About 35 million years ago,
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