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Mount-Meager-Massiv

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Vorlage:Infobox mountain Mount Meager, originally known as Meager Mountain, is a volcanic massif in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Part of the Cascade Volcanic Arc of western North America, it is located Vorlage:Convert north of Vancouver at the northern end of the Pemberton Valley. Its maximum elevation is Vorlage:Convert. Meager is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits, including Mount Meager proper which is the second highest of the massif.

The Garibaldi Volcanic Belt (GVB) has a long history of eruptions and poses a threat to the surrounding region. Any volcanic hazard ranging from landslides to eruptions could pose a significant risk to humans and wildlife. Even though Mount Meager has not erupted for more than 2,000 years, it could again produce a major eruption; if this were to happen, relief efforts would be quickly organized. Teams such as the Interagency Volcanic Event Notification Plan (IVENP) are prepared to notify people threatened by volcanic eruptions.

Mount Meager is the site of the largest volcanic eruption in Canada in the past 10,000 years. About 2,400 years ago, an explosive eruption formed a volcanic crater on its northeastern flank and sent avalanches of hot ash, rock fragments and volcanic gases down the northern flank of the volcano. Evidence for more recent volcanic activity has been documented at the volcano, such as hot springs and earthquakes. Mount Meager has also been the source for several large landslides in the past, including a massive debris flow in 2010 that swept down Meager Creek and the Lillooet River.

Geography and geology

Regional geography

Mount Meager is situated in the Coast Mountains, a Vorlage:Convert long mountain range extending from Vancouver to the Alaskan Panhandle.[1][2] It is about Vorlage:Convert wide, cut by fjords created by glacial erosion. The Coast Mountains have a profound effect on British Columbia's climate; lying just east of the Pacific Ocean, they sheer off moisture-laden air coming off the ocean, causing heavy rainfalls on their western slopes. The precipitation is among the heaviest in North America, feeding a lush forest on the mountains' flanks.[2]

Valleys surrounding Mount Meager contain old-growth forests. The area also has wetland habitats, plants of the cottonwood-willow-thimbleberry family and glaucous willowherbs. Wildlife such as wolves, wolverine, moose, raptors, black-tailed deer, mountain goats and waterfowl inhabit the area, as well as grizzly and black bears.[3]

Regional geomorphology

Garibaldi Volcanic Belt

 
Area of the Cascadia subduction zone, with Mount Meager being the northernmost red triangle in the Cascade Volcanic Arc

Mount Meager is part of the Garibaldi Volcanic Belt, the northernmost segment of the Cascade Volcanic Arc. This volcanic belt includes cinder cones, calderas, stratovolcanoes and subglacial volcanoes that have been active in the Holocene period (10,000 years ago to present).[4][5][6][7] The latest explosive eruption in the Garibaldi Volcanic Belt occurred at a crater on the northeastern flank of Mount Meager, which forms a clearly defined depression.[8][9]

The GVB extends north from the Watts Point volcano to at least as far as Mount Meager.[10][11] Little is known about the volcanoes north of Meager, such as Silverthrone and the Franklin Glacier volcanic complex, leaving room for experts to disagree about their nature.[5][12] For example, some scientists regard the Silverthrone Caldera as the northernmost volcano of the Garibaldi Volcanic Belt, while others contend that the geology of Mount Meager more closely matches that of the GVB.[13][14] It is also unclear whether the Milbanke Sound Cones are part of the Garibaldi Belt or they are volcanoes formed by different tectonic processes than those in the Garibaldi Belt.[15] However, there is evidence the Silverthrone and Franklin Glacier complexes are related to Cascadia subduction. Geologically, these two volcanoes contain the same rock types as those found elsewhere in the Cascade Arc, including rhyolites, dacites, andesites and basaltic andesites. Such rock types are produced by subduction zone volcanism, indicating volcanism at Silverthrone and Franklin Glacier is probably related to subduction. If these two volcanoes are true Cascade Arc volcanoes, Mount Meager is not the northernmost volcano of the Garibaldi Belt or the Cascade Arc.[16]

Cascade Volcanic Arc

Volcanism in the Cascade Volcanic Arc is caused by subduction of the Juan de Fuca Plate under the North American Plate at the Cascadia subduction zone.[17] This is a Vorlage:Convert long fault zone running Vorlage:Convert off the Pacific Northwest from Northern California to southwestern British Columbia. The plates move at a relative rate of over Vorlage:Convert per year at an oblique angle to the subduction zone. Because of the very large fault area, the Cascadia subduction zone can produce large earthquakes of magnitude 7.0 or greater. The interface between the Juan de Fuca and North American plates remains locked for periods of roughly 500 years. During these periods, stress builds up on the interface between the plates and causes uplift of the North American margin. When the plate finally slips, the 500 years of stored energy are released in a massive earthquake.[18]

Unlike most subduction zones worldwide, there is no deep oceanic trench present along the continental margin in Cascadia.[19] The reason is that the mouth of the Columbia River empties directly into the subduction zone and deposits silt at the bottom of the Pacific Ocean, burying this large depression. Massive floods from prehistoric Glacial Lake Missoula during the Late Pleistocene also deposited large amounts of sediment into the trench.[20] However, as with other subduction zones, the outer margin is slowly being compressed like a giant spring.[18] When the stored energy is suddenly released by slippage across the fault at irregular intervals, the Cascadia subduction zone can create very large earthquakes, such as the magnitude 9.0 Cascadia earthquake on January 26, 1700.[21] However, earthquakes along the Cascadia subduction zone are less common than expected and there is evidence of a decline in volcanic activity over the past few million years. The probable explanation lies in the rate of convergence between the Juan de Fuca and North American plates. These two tectonic plates currently converge Vorlage:Convert to Vorlage:Convert per year. This is only about half the rate of convergence from seven million years ago.[19]

Local geography

 
The location and extent of the Garibaldi Volcanic Belt, showing its isolated volcanoes and related volcanic features

Six main summits constitute the Mount Meager massif. The highest and northernmost summit is Plinth Peak with an elevation of Vorlage:Convert.[22][23] Mount Meager proper is Vorlage:Convert in elevation.[23] Capricorn Mountain west of Mount Meager proper rises with an elevation of Vorlage:Convert. Mount Job, Vorlage:Convert, is situated just west of Capricorn Mountain.[22][23] Pylon Peak with an elevation of Vorlage:Convert is south of Capricorn Mountain and Mount Meager proper.[23] Devastator Peak, also known as The Devastator, has an elevation of Vorlage:Convert and is the lowest and southernmost summit of Mount Meager.[22][23]

Streams and glaciers have played a significant role in dissecting the massif and its upper slopes are covered by snow and ice.[24] Numerous feeder dikes to older units are exposed by deep erosion.[14] Perkin's Pillar, a vertical tower of brecciated lava, represented an erosional remnant of Meager until its collapse in June 2005.[8] More than 10 streams drain meltwater from Mount Meager, including Capricorn Creek, Job Creek, No Good Creek, Angel Creek, Devastation Creek, Canyon Creek and Affliction Creek.[24]

Local geomorphology

The geomorphology of the Mount Meager massif is similar to Glacier Peak, another Cascade Arc volcano, located in the U.S. state of Washington.[8] It consists of at least four overlapping stratovolcanoes that become progressively younger from south to north.[14] With a total volume of Vorlage:Convert, Mount Meager is older than most volcanoes in the Cascade Arc, tracing its history back to 2,200,000 years ago.[8][14] In the Cascade Range, the oldest volcanoes are generally no more than a million years old.[25] This includes Mount Rainier (500,000 years old),[26] Lassen Peak (25,000 years old),[14] Mount Jefferson (290,000 years old),[14] Mount St. Helens (50,000 years old)[14] and many more.[25] However, portions of Mount Meager formed in the last million years.[1] The volcano is made of volcanic rocks ranging from rhyodacite to basalt. Rhyodacite forms a series of eroded volcanic plugs, which represent the highest peaks of Meager. Their flanks are covered by their eruptive products and are the surface expressions of intrusions. As a result, they provide a unique opportunity to study the relationships between magma chambers and their lavas. The mafic, intermediate and felsic volcanic rocks of Meager were erupted from at least eight volcanic vents.[14]

Bridge River Vent

 
The glaciated northeastern flank of Plinth Peak. Also shown is the inconspicuous ice and debris-covered Bridge River Vent in the middle of the photo.

The Bridge River Vent is a relatively young volcanic crater that formed during an eruption about 2,400 years ago.[24][27] This eruption ranged in character from explosive to effusive, involving lava dome extrusion, pyroclastic flows, lahars and lava flows.[28] Eastward migration of the eruption column spread material across Western Canada to deposit the Bridge River Ash. In the Bridge River and Lillooet River area, the ash occurs as a coarse-textured deposit with blocks of pumice up to Vorlage:Convert in diameter. The texture rapidly becomes finer eastward from the Bridge River. At Big Bar on the Fraser River, pellets are up to Vorlage:Convert in diameter while pellets in the Messiter area have a maximum diameter of Vorlage:Convert.[29]

Situated on the northeastern flank of Plinth Peak, the Bridge River Vent has an elevation of Vorlage:Convert.[22][30] It has oversteepened walls covered with ice and debris from volcanic activity and slope collapses.[1][30] The crater is roughly bowl-shaped, although it is breached on the northern side.[30] Because the Bridge River Vent is located on the northern flank of Meager, it represents a satellite vent. The eruption that formed the Bridge River Vent was probably fed through a conduit from the magma chamber below Meager. A stress field controlled by regional tectonics has been commonly invoked to explain the dynamics of lateral flow of magma from a reservoir to produce such eruptions.[31]

Human history

Naming

The name Meager Mountain was adopted on May 6, 1924 as labelled on a 1923 British Columbia map. In 1966, the volcano was renamed to Mount Meager. According to a BC Geographical Names letter written in March 1983, "the local name, Cathedral, was duplicated elsewhere, so the mountain was renamed Meager after the creek of that name which lies to the south of it". Meager Creek is in turn named after J.B. Meager, who was an owner of timber licences on the creek.[32] Despite its official name, Mount Meager is sometimes mistakenly spelled Mount Meagre or Mount Meagher.[33]

 
The Mount Meager massif as seen from the Pemberton Valley

Meager's subsidiary peak names were submitted by Canadian mountaineer Neal M. Carter, who was a member of the British Columbia Mountaineering Club. Devastator Peak was officially named on August 3, 1977 in association with Devastation Glacier.[34] Plinth Peak was officially named on September 6, 1951 as identified in Carter's 1932 sketch map and article "Explorations in the Lillooet River Watershed".[35] Mount Job and Pylon Peak were both officially named on January 17, 1957 as labelled on Carter's 1954 sketch map of the Lillooet River.[36][37] Capricorn Mountain was originally identified as Mount Capricorn in the 1932 Canadian Alpine Journal, Vol XXI. According to Carter's 1932 Canadian Alpine Journal, Vol XXI, "the name chosen for the 8440-foot mountain was Mt. Capricorn, a variation of the all-too-common appellation "Goat Mountain", applied by Bert [Perkins] to the stream which drains the Capricorn glacier at its base". Subsequently, the peak was renamed to Capricorn Mountain on June 22, 1967.[38]

Mining and hydrothermal energy

A large pumice outcrop more than Vorlage:Convert long and Vorlage:Convert wide has been the subject of mining operations since at least the 1970s. The deposit was first held by J. MacIsaac. In the mid 1970s the second hirer, W.H. Willes, investigated and mined the pumice. It was crushed, removed, and stored close to the village of Pemberton. Later, the bridge that was used to access the pumice deposit was washed out and mining operations were not renewed. Mining resumed in 1988 when the deposit was staked by L.B. Bustin. In 1990, the pumice outcrop was bought by D.R. Carefoot from the owners B. Chore and M. Beaupre. In a program from 1991 to 1992, workers evaluated the deposit for its properties as a construction material and as an absorber for oil and stonewash. About Vorlage:Convert of pumice was mined in 1998 by the Great Pacific Pumice Incoporation.[39]

Mount Meager has been investigated as a potential hydrothermal energy resource. At least 16 geothermal sites have been identified in British Columbia, with the Mount Meager area being one of the five areas most capable for commercial development. At Meager Creek, there is potential for commercial development of a 100–200 megawatt power station. Nearby Pebble Creek also has "very good" potential for a 200 megawatt plant.[40] Because the two creeks offer the greatest potential for commercial development, the Mount Meager area is the most promising site for geothermal power development in British Columbia.[22][40]

Volcanic history

 
Diagrammatic representation of eruptive activity at Mount Meager in millions of years (Ma). Height of the histogram gives a very crude indication of the size of the event. The latest event about 2,400 years ago (shown in the histograph as the latest eruption) was similar to the 1980 eruption of Mount St. Helens. Eruptive events marked with question marks are those with uncertain idendity.

At least 54 eruptions have occurred at Mount Meager in the past 2,600,000 years, ranging in character from effusive to explosive.[8][9][41] Four primary eruptive periods in the history of Mount Meager have been identified, with individual eruptions separated by thousands of years.[14][41] Large northwest-southeast trending structures paralleling Harrison Lake and the Pemberton Valley may control volcanic activity at Mount Meager or at least create zones of crustal weakness that are exploited by rising magma batches.[8]

First record of activity

During the first eruptive period 2,200,000 to 1,900,000 years ago, eruption of intermediate to felsic pyroclastic rocks occurred at the southern end of the massif.[13][14] Basal breccia, which may be an exhumed vent, underlies andesite and tuffs, flows, lava domes and breccia of Devastator Peak.[13] It has a maximum thickness of Vorlage:Convert and overlies a Vorlage:Convert high ridge of bedrock that formed between 251,000,000 and 65,500,000 years ago of the Mesozoic era.[1]

At the southwestern end of Meager, dacite with sparse phenocrysts of quartz, plagioclase and hornblende, represents a Vorlage:Convert thick remnant of subhorizontal lava flows.[1] Although the first eruptive period is generally estimated to have started about 2,200,000 years ago, two andesite eruptions may have occurred about 2,400,000 and 2,600,000 years ago. The first might have produced lava flows and breccia whereas the later may have erupted mainly breccia.[41]

The Devastator and Pylon assemblage eruptive periods

The second eruptive period between 1,600,000 and 1,400,000 years ago produced rhyodacite tuff, breccia, lavas and domes of The Devastator Assemblage.[13][41] This Vorlage:Convert thick geological formation is located on the south and west flanks of Pylon Peak and Devastator Peak. Its western portion consists of roughly layered tephra while its eastern end represents the lava flows and subvolcanic intrusions of a partly preserved vent. Here, The Devastator Assemblage is massive and steeply truncates basal breccia from the first eruptive period.[1]

Between 1,100,000 and 200,000 years ago, a thick sequence of andesite lava flows were erupted from the volcanic plug of Devastator Peak, creating the Pylon Assemblage.[1][41] With a maximum thickness of over Vorlage:Convert, the Pylon Assemblage is the largest rock unit comprising Mount Meager.[9][13] The lava flows are layered, separated by a thin layer of lapilli tuff and reddened breccia. A concentration of subvolcanic intrusions and coarse volcanic breccia clasts over Vorlage:Convert in length suggest that Devastator Peak is a major vent.[1]

Formation of the Plinth, Job, Capricorn and Mosaic assemblages

The fourth and final eruptive period 150,000 to less than 3,000 years ago produced rhyodacite lava flows, domes, breccias and subvolcanic intrusions of the Plinth, Job and Capricorn assemblages.[13][14] Around Mount Job, porphyritic hornblende, biotite and quartz rhyodacite lava flows of the Job Assemblage were erupted. They are prominently layered and locally columnar jointed. On the east side of Affliction Glacier, they overlie porphyritic andesite lava flows of the Pylon Assemblage. Later, rhyodacite lava flows of the Capricorn Assemblage were erupted and flowed over biotite rhyodacite of the Job Assemblage. The upper Vorlage:Convert of Capricorn Mountain and Mount Job are formed by these lava flows.[1]

 
A geologist next to a tree trunk that was buried by ash-fall deposits and then overrun by a pyroclastic flow from the Bridge River Vent eruption about 2,400 years ago

Another sequence of rhyodacite lava flows were subsequently erupted and form the Plinth Assemblage. Mount Meager proper, a massive lava dome or volcanic plug, consists of steeply inclined flow layering and was the southern source of Plinth Assemblage lava flows and breccias. Plinth Peak was also formed during the Plinth Assemblage eruptive stage and is mostly composed of prominent columnar or partly jointed lava flows. Its north ridge and flat-topped summit contain three areas of steep flow layering and subhorizontally oriented columnar jointing. These areas are possibly the remains of volcanic plugs or lava domes that were the northern source of Plinth Assemblage lava flows.[1] The Mosaic Assemblage, a sparsely porphyritic plagioclase-augite-olivine basalt and trachybasalt formation, also formed during the fourth eruptive period. It is the remains of scoriaceous lava flows, breccias, volcanic bombs and pillow lavas.[1][13]

The best known and most documented eruption of Mount Meager is a large explosive eruption that occurred about 2,400 years ago.[24] This eruption, which likely reached 5 on the Volcanic Explosivity Index (VEI), was similar to the 1980 eruption of Mount St. Helens.[28][42] It sent a massive Plinian column at least Vorlage:Convert high into the atmosphere. Prevailing winds carried volcanic ash from this explosion eastwards to as far as Alberta. Nearby areas were devastated by heavy pyroclastic fall when parts of the Plinian column collapsed. Later, a series of pyroclastic flows were erupted and travelled Vorlage:Convert from their source. After this happened, a lava flow was erupted that repeatedly collapsed on Meager's steep flanks, creating a thick welded breccia deposit that blocked the Lillooet River. This created a lake just upstream and later collapsed to produce a massive outburst flood. Large boulders were carried downstream for over Vorlage:Convert, but the destructive floodwaters continued further. After this took place, a small dacite lava flow was erupted, which cooled into well preserved columnar joints.[9] The entire eruption cycle was erupted from the Bridge River Vent on the northeastern flank of Plinth Peak.[28][30] This is the latest known eruption of Mount Meager, as well as the largest known Holocene explosive eruption in Canada.[43] However, it is unknown when this eruption ended.[28]

In 1977, J. A. Westgate of the University of Toronto suggested that a smaller eruption may have occurred at the Bridge River Vent after the eruption 2,400 years ago, sending tephra to the southeast. A tephra deposit overlying the Bridge River Ash at Otter Creek shows strong genetic relationships with the Bridge River Ash, differing only by its absence of biotite. In earlier publications, this tephra is classified as part of the Bridge River Ash. However, it has been dated to be about 2,000 radiocarbon years old, indicating that this tephra is a few hundred years younger than the Bridge River Ash. Apparent absence of biotite and occurrence well to the south of the Bridge River Ash likewise favour a separate identity.[44] Large volume, fine grained, debris flows north of the volcano might have been caused by volcanic activity. If this is correct, the knowledge of eruptions at Mount Meager in the past 10,000 years is insufficient.[8]

Recent activity

 
A hot spring near Meager Creek related to volcanism at Mount Meager

Two small hot spring clusters are found at Mount Meager, indicating magmatic heat is still present.[9] These two clusters of hot springs, known as the Meager Creek Hot Springs and Pebble Creek Hot Springs, are most likely related to recent volcanic activity at Mount Meager.[22][23] Meager Creek Hot Springs, the largest in British Columbia, remain free of snow for most of the year.[23][45] The springs at Mount Meager might be evidence of a shallow magma chamber beneath the surface.[46]

Between 1970 and 2005, over 20 small earthquakes were recorded at the volcano. The magnitude of these events were generally no higher than 2.0 on the Richter magnitude scale and they originated Vorlage:Convert to less than Vorlage:Convert below the surface.[24] Other volcanoes in the Garibaldi Volcanic Belt with recorded seismicity include Mount Garibaldi, Mount Cayley and Silverthrone Caldera.[47] Seismic data suggest that these volcanoes still contain active magma chambers, indicating that some Garibaldi Belt volcanoes are probably active, with significant potential hazards.[47][48] The seismic activity corresponds with some of Canada's recently formed volcanoes and with persistent volcanoes that have had major explosive activity throughout their history, such as Mount Garibaldi, Mount Cayley and Mount Meager.[47]

Threats and preparedness

Eruptions

Mount Meager is a major volcanic hazard capable of producing highly explosive eruptions that threaten many populated areas throughout southern British Columbia and Alberta. Pemberton, a community some Vorlage:Convert downstream from Meager, is also at risk by the volcano.[9] If the volcano were to erupt again violently, it would have large-scale effects on the Lillooet River fishery and nearby mining and logging activity.[9] In addition, Mount Meager is situated in the immediate proximity of a major air traffic route.[49] Volcanic ash reduces visibility and can cause jet engine failure, as well as damage to other aircraft systems.[50]

 
This pyroclastic flow deposit forms the foreground canyon wall on the Lillooet River. It was erupted from the Bridge River Vent on the northeastern flank of Plinth Peak.

Jack Souther, a leading authority on geothermal resources and volcanism in the Canadian Cordillera, has expressed concern about the potential for another eruption:

At present the volcanoes of the Garibaldi Belt are quiet, presumed dead but still not completely cold. But the flare-up of Meager Mountain 2,500 years ago raises the question, "Could it happen again?" Was the explosive eruption of Meager Mountain the last gasp of the Garibaldi Volcanic Belt or only the most recent event in its on-going life? The short answer is nobody really knows for sure. So just in case I sometimes do a quick check of the old hot-spots when I get off the Peak Chair.[51]

Because of concerns about the potential for eruption and its danger to communities in the area, the Geological Survey of Canada is planning to create hazard maps and emergency plans for Mount Meager, as well as Mount Cayley to the south.[48]

Even though very few eruptions in Canada have been witnessed by people, it is nonetheless an area of intense volcanic activity. According to the Geologic Hazards '91 Workshop, "priority should be given to eruption impact studies of the two recently active volcanic centres closest to urban areas, Mount Baker and Mount Meager. The former case will require a combined US-Canada-Washington State-B.C. effort".[41] In addition, Mount Meager is not monitored closely enough by the Geological Survey of Canada to ascertain how active its magma system is. The Canadian National Seismograph Network has been established to monitor earthquakes throughout Canada, but it is too far away to provide a good indication of what is happening under the mountain. It may sense an increase in seismic activity if Meager becomes very restless, but this may only provide a warning for a large eruption. It might detect activity only once the volcano has started erupting.[52] If it were to erupt, relief efforts would probably be orchestrated. The Interagency Volcanic Event Notification Plan (IVENP) was created to outline the notification procedure of some of the main agencies that would be involved in response to an erupting volcano in Canada, an eruption close to the Canada–United States border or any eruption that will have effects in Canada.[53]

Although Mount Meager is a potentially active volcano, as of 2003 there was no evidence of an imminent eruption. Many shallow earthquakes normally occur before a volcano erupts. As magma rises to the surface, it will probably create much more vigour and heat at the regional hot springs, as well as the formation of new springs or fumaroles.[54] These signs generally occur for weeks, months or years before a potential eruption, although the possibility of an eruption occurring in the near future is low.[52][54]

Landslides

Scientists have argued that Mount Meager, made of altered volcanic rock which breaks apart easily, is the most unstable mountain massif in Canada,[24] and may also be its most active landslide area.[55] More than 25 landslides have occurred at Mount Meager in the past 8,000 years.[24] Debris flows, mainly from Mount Meager, have also filled Meager Creek valley to a depth of Vorlage:Convert.[1]

Large volcano-associated debris flows, known as lahars, can pose a threat to populated areas downstream from glaciated volcanoes.[56] Although lahars are typically associated with the effects of volcanic eruption, they can occur whenever the conditions are right to cause the collapse and movement of mud originating from existing volcanic ash deposits. Melting snow and ice, intense rainfall or the breakout of a summit crater lake are all potential causes. Landslides at Mount Meager may also be indirectly related to climate change. Several tension cracks extend up to the summit, and as global warming causes glaciers to melt, the meltwater makes its way deep into the massif. It then flows along the ruptured surfaces, making these landslide zones.[57]

Because Mount Meager is capable of producing large landslides, Meager Creek valley is probably the most dangerous valley in the Canadian Cordillera. Although some distance away from Meager, rapidly growing communities down the Lillooet River valley (such as Pemberton)[9] are vulnerable. As Pemberton continues to grow it will eventually get pushed into the surrounding mountains, causing a major hazard to people living there.[57]

Prehistoric

Event Source Years before present Volume Reference[24]
Rock avalanche/debris flow Pylon Peak 7900 450,000,000 m3 (16,000,000,000 cu ft) Friele and Clague (2004)
Rock avalanche/debris flow Job Creek 6250 500,000,000 m3 (18,000,000,000 cu ft) Friele et al. (2005)
Rock avalanche/debris flow Capricorn Creek 5250 Vorlage:Convert McNeely and McCuaig (1991)
Rock avalanche/debris flow/hyperconcentrated flow Pylon Peak 4400 200,000,000 m3 (7,100,000,000 cu ft) Friele and Clague (2004); Friele et al. (2005)
Rock avalanche/debris flow Job Creek, eruption precursor 2600 500,000,000 m3 (18,000,000,000 cu ft) Friele et al. (2005); Simpson et al. (2006)
Pyroclastic flow Syn-eruptive 2400 440,000,000 m3 (16,000,000,000 cu ft) Stasiuk et al. (1996); Stewart (2002)
Rock avalanche/outburst flood/debris flow/hyperconcentrated flow Syn-eruptive 2400 200,000,000 m3 (7,100,000,000 cu ft) Stasiuk et al. (1996); Stewart (2002)
Rock avalanche Syn- to post-eruptive 2400 44,000,000 m3 (1,600,000,000 cu ft) Stasiuk et al. (1996); Stewart (2002)
Debris flow Job Creek 2240 Vorlage:Convert Pierre, Jakob and Clague (2008)
Debris flow Devastation Creek 2170 Vorlage:Convert McNeely and McCuaig (1991)
Debris flow Angel Creek 1920 Vorlage:Convert McNeely and McCuaig (1991)
Debris flow Job Creek 1860 Vorlage:Convert McNeely and McCuaig (1991)
Debris flow Job Creek 870 Vorlage:Convert Jordan (1994)
Debris flow No Good Creek 800 Vorlage:Convert McNeely and McCuaig (1991)
Debris flow Job Creek 630 Vorlage:Convert Pierre, Jakob and Clague (2008)
Debris flow No Good Creek 370 Vorlage:Convert McNeely and McCuaig (1991)
Debris flow Angel Creek 210 Vorlage:Convert McNeely and McCuaig (1991)

Historic

 
These river valleys are filled with debris from the 2010 landslide of Mount Meager. Photo A is the collapsed debris dam near the intersection of Capricorn Creek and Meager Creek. Photo B is the debris flow at the junction of Meager Creek and the Lillooet River.
Event Source Year Volume Reference[24][58]
Debris flow Capricorn Creek 1850 Vorlage:Convert Jakob (1996); McNeely and McCuaig (1991)
Debris flow Capricorn Creek 1903 30,000,000 m3 (1,100,000,000 cu ft) Jakob (1996)
Debris flow Devastation Creek 1931 Vorlage:Convert Carter (1931); Decker et al. (1977); Jordan (1994)
Rock avalanche Capricorn Creek 1933 Vorlage:Convert Croft (1983)
Rock avalanche Devastation Creek 1947 Vorlage:Convert Read (1978)
Debris flow Capricorn Creek 1972 Vorlage:Convert Jordan (1994)
Rock avalanche Devastation Creek 1975 Vorlage:Convert Mokievsky-Zubot (1977); Evans (2001)
Debris flow Affliction Creek 1984 Vorlage:Convert Jordan (1994)
Rock avalanche Mount Meager 1986 Vorlage:Convert Evans (1987)
Debris flow Capricorn Creek 1998 Vorlage:Convert Bovis and Jakob (2000)
Debris flow Capricorn Creek 2009 Vorlage:Convert Friele (unpublished data)
Rock slide/debris flow Capricorn Creek 2010 48,500,000 m3 (1,710,000,000 cu ft) Guthrie et al. (2012)
1975 landslide

The main Mount Meager landslide with known casualties was a massive rock avalanche that occurred on July 22, 1975. With a volume of Vorlage:Convert, it buried and killed a group of four geologists at the confluence of Devastation Creek and Meager Creek.[59][60] The landslide originated on the western flank of Pylon Peak and flowed down Devastation Creek for Vorlage:Convert. Geologic studies have shown that the landslide was the result of a complex history of glacial erosion, loading and unloading of the toe of the slide mass caused by the Little Ice Age advance, and subsequent retreat of Devastation Glacier due to global warming.[59]

2010 landslide

On August 6, 2010, a massive lahar cascaded down from Capricorn Glacier at a speed of Vorlage:Convert per second.[57] Experts initially estimated that the volume of debris totaled Vorlage:Convert, which would make it the second largest landslide on record in Canadian history behind only the 1965 Hope Slide, which removed Vorlage:Convert of rock from Johnson Peak.[57][61] However, the Meager landslide was later estimated to be over Vorlage:Convert, making it perhaps the largest of all time in Canada.[57]

The 2010 landslide at Mount Meager was Vorlage:Convert wide and Vorlage:Convert long, creating a dam across Meager Creek and the Lillooet River. This resulted in the creation of a lake just upstream. Early concerns that the dam might collapse and flood the Lillooet River valley ended a day later, when part of the dam ruptured and slowly released the accumulated water. An evacuation alert was rescinded, and nearly 1,500 residents were allowed to return to their homes on the weekend after the landslide occurred. No injuries were reported.[57]

See also

Portal: Volcanism of Canada – Volcanoes

References

Vorlage:USGS Vorlage:Reflist

Vorlage:Commons category

Vorlage:Pacific Ranges Vorlage:Garibaldi Volcanic Belt Vorlage:Cascade volcanoes

  1. ↑ a b c d e f g h i j k l Peter B. Read: Mount Meager Complex, Garibaldi Belt, Southwestern British Columbia. In: Articles. 17. Jahrgang, Nr. 3. St. John's, Newfoundland, 1990, ISSN 1911-4850, S. 167, 168, 169, 170.
  2. ↑ a b Coast Mountains. In: BC Geographical Names (englisch).
  3. ↑ Upper Lillooet Provincial Park. BC Parks, abgerufen am 20. Juli 2011.
  4. ↑ Opal Cone. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 10. März 2009, abgerufen am 6. Juli 2010. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  5. ↑ a b Silverthrone Caldera. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 10. März 2009, abgerufen am 6. Juli 2010. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  6. ↑ Mount Price. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 10. März 2009, abgerufen am 6. Juli 2010. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  7. ↑ Cauldron Dome. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 10. März 2009, abgerufen am 6. Juli 2010. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  8. ↑ a b c d e f g J.W.H. Monger: Geology and Geological Hazards of the Vancouver Region, Southwestern British Columbia. Natural Resources Canada, Ottawa, Ontario 1994, ISBN 0-660-15784-5, Character of volcanism, volcanic hazards, and risk, northern end of the Cascade magmatic arc, British Columbia and Washington State, S. 231, 241, 242.
  9. ↑ a b c d e f g h Garibaldi volcano belt: Mount Meager volcanic field. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 1. April 2009, abgerufen am 6. Juli 2011.
  10. ↑ Garibaldi volcanic belt. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 2. April 2009, abgerufen am 6. Juli 2010. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  11. ↑ Garibaldi Volcanic Belt. In: Map of Canadian volcanoes. Natural Resources Canada, 20. August 2005, abgerufen am 6. Juli 2010. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  12. ↑ Flanklin Glacier. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 10. März 2009, abgerufen am 4. November 2011. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  13. ↑ a b c d e f g Pete Stelling, David S. Tucker: Floods, Faults, and Fire: Geological Field Trips in Washington State and Southwest British Columbia. Geological Society of America, Boulder, Colorado 2007, ISBN 978-0-8137-0009-0, S. 2, 14, 15.
  14. ↑ a b c d e f g h i j k Charles A. Wood, Kienle, Jürgen: Volcanoes of North America: United States and Canada. Cambridge University Press, Cambridge, England 2001, ISBN 0-521-43811-X, S. 113, 141, 149, 161, 177, 218.
  15. ↑ Anahim Volcanic Belt: Milbanke Sound cones. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 14. April 2009, abgerufen am 4. November 2011. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  16. ↑ Stephen Blakes, Tom Argles: Growth and Destruction: Continental evolution at subduction zones. The Open University, Milton Keynes, United Kingdom 2003, ISBN 0-7492-5666-4, S. 55.
  17. ↑ Alan R. Gillespie, Stephen C. Porter, Brain F. Atwater: The Quaternary period in the United States. Elsevier, Amsterdam, Netherlands 2004, ISBN 0-444-51471-6, S. 351.
  18. ↑ a b Cascadia Subduction Zone. In: Geodynamics. Natural Resources Canada, 15. Januar 2008, abgerufen am 6. März 2010.
  19. ↑ a b Pacific Mountain System – Cascades volcanoes. United States Geological Survey, 10. Oktober 2000, abgerufen am 5. März 2010.
  20. ↑ Steven Dutch: Cascade Ranges Volcanoes Compared. University of Wisconsin, 7. April 2003, abgerufen am 21. Mai 2010.
  21. ↑ The M9 Cascadia Megathrust Earthquake of January 26, 1700. Natural Resources Canada, 3. März 2010, abgerufen am 6. März 2010.
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  25. ↑ a b Jeff Smoot: Climbing the Cascade Volcanoes. Globe Pequot Press, Guilford, Connecticut 1999, ISBN 1-56044-889-X, S. 9.
  26. ↑ Peter Aleshire: Mountains. Infobase Publishing, New York City, New York 2008, ISBN 0-8160-5918-7, S. 97.
  27. ↑ Bridge River Vent. In: Catalogue of Canadian volcanoes. Natural Resources Canada, 10. März 2009, abgerufen am 9. Oktober 2011. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
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  31. ↑ V. Acocella, M. Neri: What makes flank eruptions? The 2001 Etna eruption and its possible triggering mechanisms. Springer-Verlag, Berlin, Germany 2003, S. 518.
  32. ↑ Mount Meager. In: BC Geographical Names (englisch).
  33. ↑ Halstead, E.C.: Ground water supply – Fraser Lowland, British Columbia. National Hydrology Research Institute, Saskatoon, Saskatchewan 1986, S. 60.
  34. ↑ Devastator Peak. In: BC Geographical Names (englisch).
  35. ↑ Plinth Peak. In: BC Geographical Names (englisch).
  36. ↑ Mount Job. In: BC Geographical Names (englisch).
  37. ↑ Pylon Peak. In: BC Geographical Names (englisch).
  38. ↑ Capricorn Mountain. In: BC Geographical Names (englisch).
  39. ↑ Mount Meager, Lillooet River Pumice, Pum, Great Pacific, Mt. Meager Pumice. In: MINFILE Mineral Inventory. Government of British Columbia, 4. Dezember 1998, abgerufen am 16. März 2010.
  40. ↑ a b Vorlage:Cite paper
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  43. ↑ Vorlage:Cite gvp
  44. ↑ Identification and significance of late Holocene tephra from Otter Creek, southern British Columbia, and localities in west-central Alberta. In: Canadian Journal of Earth Sciences. 14. Jahrgang. NRC Research Press, 1977, ISSN 0008-4077, S. 2595.
  45. ↑ Matthew Gardner: Western Canada. Footprint Handbooks Ltd, Bath, England 2008, ISBN 978-1-906098-26-1, S. 157.
  46. ↑ Glenn J. Woodsworth: Geology and Geothermal Potential of the AWA Claim Group, Squamish, British Columbia. Gold Commissioner's Office, Vancouver, British Columbia, S. 10.
  47. ↑ a b c David Etkin, Haque, C.E. and Brooks, Gregory R.: An Assessment of Natural Hazards and Disasters in Canada. Springer Science+Business Media, Berlin, Germany 2003, ISBN 978-1-4020-1179-5, S. 569, 582, 583.
  48. ↑ a b Volcanology in the Geological Survey of Canada. In: Volcanoes of Canada. Natural Resources Canada, 10. Oktober 2007, abgerufen am 6. Juli 2010.
  49. ↑ Volcanic hazards. In: Volcanoes of Canada. Natural Resources Canada, 2. April 2009, abgerufen am 23. Juli 2011.
  50. ↑ Christina A. Neal, Thomas J. Casadevall, Thomas P. Miller, James W. Hendley II, Peter H. Stauffer: Volcanic Ash–Danger to Aircraft in the North Pacific. United States Geological Survey, 14. Oktober 2004, abgerufen am 23. Juli 2011.
  51. ↑ CanGEA Honourary Member 2008 Dr. Jack Souther. (PDF) Canadian Geothermal Energy Association, abgerufen am 4. März 2010.
  52. ↑ a b Monitoring volcanoes. In: Volcanoes of Canada. Natural Resources Canada, 26. Februar 2009, abgerufen am 15. Juni 2011. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  53. ↑ Interagency Volcanic Event Notification Plan (IVENP). In: Volcanoes of Canada. Natural Resources Canada, 4. Juni 2008, abgerufen am 15. Juni 2011. Fehler beim Aufruf der Vorlage:Cite web: Archiv im Parameter URL erkannt. Archive müssen im Parameter Archiv-URL angegeben werden.
  54. ↑ a b K.A. Simpson, M.V. Stasiuk, J.J. Clague, S.G. Evans, P. Friele: Preliminary drilling results from the Pemberton Valley, British Columbia. Geological Survey of Canada, 2003, ISSN 1701-4387, S. 6.
  55. ↑ J. Knight, S. Harrison: Periglacial and Paraglacial Processes and Environments. Geological Society of London, London, United Kingdom 2009, ISBN 978-1-86239-281-6, S. 229.
  56. ↑ What Are Volcano Hazards? United States Geological Survey, 24. August 2010, abgerufen am 18. August 2011.
  57. ↑ a b c d e f Vivian Luk: Flooding averted after landslide blocked Meager Creek, The Vancouver Sun, 9. August 2010, S. 1, 2 
  58. ↑ Vorlage:Cite paper
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  60. ↑ K.A. Simpson, M. Stasiuk, K. Shimamura, J.J. Clague, P. Friele: Evidence for catastrophic volcanic debris flows in Pemberton Valley, British Columbia. In: Canadian Journal of Earth Sciences. 43. Jahrgang. NRC Research Press, 2006, ISSN 0008-4077, S. 688.
  61. ↑ Photograph of Hope Slide. Natural Resources Canada, 27. März 2007, abgerufen am 6. Juli 2011.
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