2. Core Case Study: The CrucialCore Case Study: The Crucial
Importance of Rare-Earth MetalsImportance of Rare-Earth Metals
Crucial to the technologies that supportCrucial to the technologies that support
today’s lifestyles and economiestoday’s lifestyles and economies
Used to make LCDs, LED light bulbs, fiberUsed to make LCDs, LED light bulbs, fiber
optic cables, cell phones, and digital camerasoptic cables, cell phones, and digital cameras
Without affordable supplies of rare earthWithout affordable supplies of rare earth
elements, we could not develop cleanerelements, we could not develop cleaner
technologiestechnologies
3. Core Case Study: The CrucialCore Case Study: The Crucial
Importance of Rare-Earth MetalsImportance of Rare-Earth Metals
4. GEOLOGIC PROCESSESGEOLOGIC PROCESSES
Earth is dynamic – due to processes on andEarth is dynamic – due to processes on and
below its surfacebelow its surface
Earth’s interior consists of:Earth’s interior consists of:
CoreCore – innermost zone with solid inner core and– innermost zone with solid inner core and
molten outer core that is extremely hotmolten outer core that is extremely hot
MantleMantle – solid rock with a rigid outer part (+ crust– solid rock with a rigid outer part (+ crust
== lithospherelithosphere) that is overlying melted pliable) that is overlying melted pliable
rock (rock (asthenosphereasthenosphere))
CrustCrust – outermost zone which underlies the– outermost zone which underlies the
continents (continental and oceanic [71% ofcontinents (continental and oceanic [71% of
earth])earth])
5. Fig. 14-3, p. 351
Spreading center
Oceanic crust Oceanic crust
Continental
crust
Continental
crust
Material cools
as it reaches
the outer
mantle
Cold dense
material falls
back through
mantle
Hot
material
rising
through
the
mantle
Mantle
convection
cell
Two plates move
towards each other.
One is subducted back
into the mantle on a
falling convection
current.
Mantle
Hot outer
core
Inner
core
AsthenosphereAsthenosphere
7. GEOLOGIC PROCESSESGEOLOGIC PROCESSES
Plate tectonicsPlate tectonics - huge volumes of heated- huge volumes of heated
and molten rack moving around the earth’sand molten rack moving around the earth’s
interior form massive solid plates that moveinterior form massive solid plates that move
extremely slowly across the earth’s surfaceextremely slowly across the earth’s surface
Tectonic platesTectonic plates – huge rigid plates moved by– huge rigid plates moved by
convection cellsconvection cells by floating onby floating on magmamagma (molten(molten
rock)rock)
9. The Earth’s Major Tectonic PlatesThe Earth’s Major Tectonic Plates
Slow movements of plates causes them toSlow movements of plates causes them to
grind into one another atgrind into one another at convergent plateconvergent plate
boundariesboundaries, move apart at, move apart at divergent platedivergent plate
boundariesboundaries and slide past atand slide past at transformtransform
plate boundariesplate boundaries
Figure 15-4Figure 15-4
11. GEOLOGIC PROCESSES ANDGEOLOGIC PROCESSES AND
NATURAL DISASTERSNATURAL DISASTERS
EarthquakesEarthquakes – releases pressure at plate– releases pressure at plate
boundariesboundaries
VolcanoesVolcanoes – at subduction zones when crust– at subduction zones when crust
meltsmelts
TsunamisTsunamis – walls of water up to 210 feet tall– walls of water up to 210 feet tall
– caused by underwater earthquakes,– caused by underwater earthquakes,
volcanoes, landslidesvolcanoes, landslides
Ex: March 11, 2011 Japan – meltdown ofEx: March 11, 2011 Japan – meltdown of
Fukushima Daiichi nuclear power plantFukushima Daiichi nuclear power plant
Ex: Dec. 26, 2004 Indian Ocean – 221,000 killedEx: Dec. 26, 2004 Indian Ocean – 221,000 killed
15. GEOLOGIC PROCESSES ANDGEOLOGIC PROCESSES AND
NATURAL DISASTERSNATURAL DISASTERS
Banda Aceh, Indonesia June 23, 2004 (beforeBanda Aceh, Indonesia June 23, 2004 (before
tsunami) and December 28, 2004 (after)tsunami) and December 28, 2004 (after)
Editor's Notes
Animated Figure 14.3 The earth is composed of a core, mantle, and crust, and within the core and mantle, dynamic forces have major effects on what happens in the crust and on the surface.