Download Volcano ppt

Survey
yes no Was this document useful for you?
   Thank you for your participation!

* Your assessment is very important for improving the workof artificial intelligence, which forms the content of this project

Document related concepts

Post-glacial rebound wikipedia , lookup

Earthquake wikipedia , lookup

Large igneous province wikipedia , lookup

Volcano wikipedia , lookup

Tectonic–climatic interaction wikipedia , lookup

Transcript
What is the Elastic Rebound Theory?
•
Explains how energy is
stored in rocks
– Rocks bend until the
strength of the rock
is exceeded
– Rupture occurs and
the rocks quickly
rebound to an
undeformed shape
– Energy is released in
waves that radiate
outward from the
fault
The Focus and Epicenter of an Earthquake
•
•
The point within Earth
where faulting begins is
the focus, or
hypocenter
The point directly above
the focus on the surface
is the epicenter
Where Do Earthquakes Occur and How Often?
~80% of all earthquakes occur in the circum-Pacific belt
– most of these result from convergent margin activity
– ~15% occur in the Mediterranean-Asiatic belt
– remaining 5% occur in the interiors of plates and on
spreading ridge centers
– more than 150,000 quakes strong enough to be felt are
recorded each year
The Economics and Societal Impacts of EQs
•
•
•
•
Damage in Oakland, CA, 1989
Building collapse
Fire
Tsunami
Ground failure
How is an Earthquake’s
Epicenter Located?
•
•
•
Three seismograph stations
are needed to locate the
epicenter of an earthquake
A circle where the radius
equals the distance to the
epicenter is drawn
The intersection of the
circles locates the
epicenter
Why do earthquakes occur?
epicenter
• Fractures, faults
• Energy released
and propagates
in all directions
as seismic waves
causing
earthquakes
focus
Crater Lake, Oregon
The Stump of Mount Mazama
What comes out of a volcano?
Ash
What comes out of a volcano?
Gas
Most common:
H2O
CO2
SO2
HCl
What comes out of a volcano?
Lava
Mauna Loa (Hawai’i): A typical shield volcan
Mt. St. Helens: A typical composite volcano
Mt. St. Helens after its 1980 eruption
How Calderas Form
Plate-tectonic setting of volcanism
Explosive (andesitic) volcanoes form at subduction
zones.
Plate-tectonic setting of volcanism
At spreading centers, low pressure triggers
mantle melting—fluid basaltic magma rises.
Plate-tectonic setting of volcanism
Within plates, rising plumes of hotter mantle feed
hot spots; varied volcanoes result (basaltic on Hawaii).
Mt. St. Helens
Pyroclastic
Eruption
Mount Saint Helens- after
Mt. Saint Helens before
Phreatic (vapor) eruption
Bulge
After the eruption
Pyroclastic eruption
Volcanic landscape:
A Caldera (Crater Lake)