Environmental Geology lecture outline
- Volcanology.
We can start with some initial questions
to ponder.
What
are the compositional variations and physical properties of lavas?
How
do you melt rocks to make magma that erupts as lava?
What
are the sources of magma?
What
are types of volcanic eruptions?
Two types of volcanic constructs and their
contrasting behavior:
- shield volcanos:
basaltic, low angle and very large typically, quieter eruptions,
small summit calderas, example Hawaiian islands.
- strato or composite volcanos: andesitic, high angle slopes, sometimes very large
calderas, potential for very devestating eruptions, example Mt.
Fuji.
- 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.
Slides
from Iceland - land of fire and ice, and lots of basalt: some
background info
- anomalous emergent portion of a spreading
ridge, so basalt dominated.
- case history of Heimay eruption.
- 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.
© Harmon D. Maher Jr.. This page
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use please contact me.
H.D. Maher Jr., 3/6/200
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