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Along the Plate Edge (Quiz 2.1)
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Michoacan
,
Mexico
Eruption of
Mt.
Paricutin
(1943-1952)
Located in Trans-Mexican Volcanic Belt
Tohoku, Japan
A
9.0
- magnitude earthquake on
March 11, 2011
Originated below the sea near subduction zone that causes tsunami
Christchurch, New Zealand
A
6.3
- magnitude earthquake on
February 22, 2011
Caused by the movement of 15-km shallow fault
Chile
8.2 earthquake
Feb. 27, 2010
and
April 1, 2014
Luzon, Philippines
Mt. Pinatubo eruption last 1991 after more than 500 years.
It released tons of SO2 into the atmosphere.
Ring of Fire
These countries lie near a zone in Pacific Ocean characterized with active volcanoes and frequent earthquakes.
Plate movements
Convergent
Divergent
Transform fault
Divergent Boundary
2 plates are moving away from one another, creating a gap between them which widens to become rift valleys
Divergence Impacts
2 continental plates produce
rift
valleys
2 oceanic plates produce
mid-ocean
ridges
Divergent Boundary
Volcanic islands are formed when lava fills the gap and later on becomes part of ocean floor.
Example of a divergent boundary
Great East African Rift Valley
Convergent Boundary
2 plates are moving toward one another, forming a subduction zone and orogenic belt.
Oceanic-Oceanic
Subduction happens, descending plate melts and rise to form volcanoes
Ex: Pacific-Philippine Plate
Oceanic-Continental
Oceanic Plate subducts, melts and rise to volcanoes. Continental Plate deforms. Trenches are also formed
Continental-Continental
Sutured, creating mountain ranges. Examples are Alps and Himalayas.
Transform Fault
2 plates sliding against each other
In opposite direction
No landforms produced --> Earthquakes produced
Earthquake
shaking of the earth resulting in the breaking and shifting of rocks
Releases seismic energy
Creates cracks called
faults
Types of faults
Reverse
Normal
Strike-slip
Oblique
Reverse Fault
The original wall goes up, and the other hangs
Normal Faults
The original wall is hanging
Strike-slip fault
Two plates slide horizontally past each other
Oblique Fault
combination of normal/reverse fault and strike slip fault
most destructive
Hypocenter
aka
focus
, source of seismic waves
Epicenter
directly above the focus
Depth of focus:
Shallow
- 10-100 km
Intermediate
- 70-300 km
Deep
- 300 km deeper
How do scientists locate earthquakes?
Triangulation Method
Triangulation Method
the intersection of 3 circles is the epicenter
Orogenesis
process of forming mountains through collision and compression
Fold Mountains
formed through plate convergence with forces of compression
Ex. Himalayas
Volcanic mountains
produced by hotspots, constructed from accumulated lava flow
Erosion-formed mountains
formed by rock erosion and weathering
Erosion
transfer of weathered rocks from one place to another
Weathering
breaking down or dissolving of rocks
Dome mountain range
upwarping of tectonic plates
Not accompanied by collision of plate boundaries
Fault-block Mountain
displacement of crust produces numerous cracks while slides down.
WVF -
West Valley Fault
PHIVOLCS -
Philippine Institute of Volcanology and Seismology
West Valley Fault
- home of the fault we have in manila
K2
- second highest mountain
Mt. Everest
- highest mountain
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