volcanoes and volcanism
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Volcanoes and volcanism. *Volcanoes represent venting of the Earth’s interior *Molten magma rises within the Earth and is erupted either quietly (lavas) or violently (pyroclastics). *Quiet eruptions tend to produce lava flows , which are not so dangerous - PowerPoint PPT PresentationTRANSCRIPT
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Volcanoes and volcanism
*Volcanoes represent venting of the Earth’s interior
*Molten magma rises within the Earth and is erupted either quietly (lavas) or violently (pyroclastics)
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Quiet vs. violent activity
*Quiet eruptions tend to produce lava flows, which are not so dangerous
*Explosive eruptions produce fragmental, or pyroclastic, material; these are dangerous
*Two controls on explosivity are (1) the silica content and (2) the gas content of the magma
Basalt: 50% SiO2, gas-poor
Andesite: 60% SiO2, gas-rich
Rhyolite: 70% SiO2, gas-rich
*Magmas with higher silica contents are more viscous
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Global distribution of volcanoes
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Magma generation at mid-ocean ridges
In these zones, the mantle rises and melts, producing magma of silicate composition
the magma continues to rise, and erupts mainly as basaltic lava flows
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Magma generation at hot spots
Magmas at hot spots are derived from deep within the mantle
The magmas are fed by deep mantle plumes which are stationary relative to the drifting tectonic plates
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Magma generation at subduction zones
During subduction, the subducted oceanic plate is heated as it plunges into the mantle
At a depth of 80-120 km, melting begins, and volcanoes are produced which parallel the subduction zone
Andesitic magmas are typical of these volcanoes
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Plate tectonics and volcanism
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Volcanic hazards of North America
“Active” volcanoes have erupted at least once in the past 10,000 years
The most active volcanoes (in red) are those associated with subduction zones
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Volcanic hazards of Canada
Canada has “active” volcanoes (black triangles) which pose a potential threat in B.C.
Another major hazard is ashfall from explosive eruptions of Cascade volcanoes in Washington state
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Volcano types
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Volcano types: cinder cones
Cinder cones are volcanoes which erupt only during one episode
They are explosive, but small in size
The cone is a pile of pyroclastic debris which piles up at the angle of repose
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Volcano types: cinder cones
The cinders are generally of basaltic composition
The eruptive activity typically lasts a few months or years
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Cinder cones: Parícutin
Parícutin volcano in Mexico is a classic cinder cone
The region contains many cinder cones
It consists of both pyroclastics and lava
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Parícutin - lava flows
These images shows the development of lavas in 1943 and in 1951-52
Red areas show new lava flows
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Parícutin - five views taken from Luhr and Simkin (1993)
The eruption was preceded by about 1½ months of felt seismicity
The eruption began in a farmer’s field on 20 February 1943
It erupted for a comparatively long (?) time (1943-1951)
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Parícutin
Here is a photo of the volcano showing the classic form of cinder cones
In the foreground is the obviously distressed farmer, Dionisio Pulido
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Parícutin
•This is a view of the volcano in
March 1944
•In the foreground, note the flat-lying
lava flows from the volcano
lava
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Parícutin
The partly unfinished towers of San Juan Parangaricutico surrounded by 1944 lava flows from the volcano
Note how the lava fills, but does not destroy, the church
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Parícutin
Note how the percentage of pyroclastic material declines steadily with
time…
while the opposite is observed for lava
The daily mass eruption rate also declines steadily
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From:http://www.meteo.mcgill.ca/195-250/2008/ppt/volcanoes.ppt
من ضمن Volc1 to Volc 6العرض موجودةعلى أعاله الموضح الموقع على أخرى عروض . الموقع تصفح الطالب من آمل األنترنت شبكة
أيضا