Volcanic hazards
Environmental Geology lecture outline
We can start with some initial background questions
about volcanism in general.
Two types of volcanic constructs and their
contrasting behavior:
- shield volcanos:
basaltic, low angle slopes and often very large, quieter eruptions,
small summit calderas, example Hawaiian islands.
-
- Example above is of the small Belknap shield volcano that is part of the Cascade chain of volcanism. The foreground is relatively young basalt lava flow. Below is a small image of the top of the Mauna Loa shield volcano. Image source USGS website: http://pubs.usgs.gov/gip/volc/types.html
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- strato or composite volcanos: andesitic, high angle slopes, sometimes very large
calderas, potential for very devestating eruptions, example Mt.
Fuji.
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-
- what
is determining these two different types of volcanic constructs?
- constructive and destructive phases of
some composite volcanos.
What
plate settings do different types of volcanism occur in?

View
of Mount Hecla in the background (low white ridge) taken during
1986 UNO field trip to Iceland. Mt Hecla is one of the most active
volcanic constructs in Iceland (most recent flows in 1970s), and
is also the site of descent into the interior in Jules Verne's
Journey to the Center of the Earth.
Iceland - land of fire and ice, and lots of basalt:
- anomalous emergent portion of a seafloor spreading
ridge, so basalt dominated.
Map below shows the position of the active rift and related volcanoes (as red triangles). Imagefrom USGS website: http://pubs.usgs.gov/gip/dynamic/understanding.html
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- case history of Heimay eruption.
Images below of houses destroyed by 1973 Heimay flow and air fall material from USGS web site: http://pubs.usgs.gov/gip/heimaey/
- fire + ice = jokulhaups.
- hot springs and geothermal energy.
-
Figure of a geysir in Iceland, with a jet
of steam just erupting through the overlying water and initiating
an eruption. This feature erupted about every 5 minutes. Note
the light colored cinter around that represents silica precipitating
out of the hot waters. This activity is fed by magma and hot
volcanic rocks at depth.
Volcanos
on the web. Fun, extensive web resource - many others.
Next lecture outline on volcanos.
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H.D. Maher Jr., 3/6/200
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