Title: Earth Science and M.E.A.P
1Earth Science and M.E.A.P
2EG. Geosphere Benchmark 2 Use the plate
tectonics theory to explain features of the
earths surface and geological phenomena, and
describe evidence for the plate tectonics
theory.
3Key concepts
Earth Composition
CrustMantle upper part is able to flow very
slowly Core interior at high temperature and
pressure
4starryskies.com/.../Earth/ under_the_surface.html
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7Key concepts
- Evidence of continental drift
- .
- Physical fit of continents
- Fossil evidence
- Measurements of movement
- Rock layer sequences
- Glacial evidence
Alfred Wegener
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9What is the theory of continental drift?
- the idea that the continents were once all joined
together in one super-continent called Pangaea
and slowly moved to their current positions
10http//wrgis.wr.usgs.gov/docs/parks/animate/A08.gi
f
11- What evidence supports the theory of continental
drift?
12Shoreline Fit of the Continents
http//www.abdn.ac.uk/zoohons/lecture1/img008.GIF
13Fossil Evidence
- The fossils from the exact same animals are found
on continents separated by vast oceans.
14Matching Rock Layers
15Glacier Evidence
Glaciers scars are found on continents which are
today too warm for glaciers.
16How fast are the plates moving?
17Bell Ringer
- Why are the continents moving?
18- During WWI scientists used sound waves to detect
submarines and discovered underwater systems of
ridges and valleys like those found on the
continents.
19Seafloor spreading is Hesss theory that new
seafloor is formed when magma is forced upward
toward the surface at a mid-ocean ridge.
20Seafloor Spreading
The oceans are widening along the mid-ocean
ridges.
21Volcanoes located along ocean ridges erupt,
creating new ocean floor.
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24Evidence for spreading
- In 1968, scientists aboard the research ship
Glomar Challenger began gathering information
about the rocks on the seafloor. They found that
the youngest rocks are located at the mid-ocean
ridges.
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26Key concepts
Platescontinental crust, oceanic crust
Featuresfaults, trenches, mid-ocean ridges,
folded mountains, hot spots, volcanoes Related
actions earthquakes, volcanic activity, seafloor
spreading, mountain building, convection in
mantle.
27The earths lithosphere is broken into huge
sections called plates that are in constant
motion.
28What are the plates made of?
- Ocean plates are made of basalt.
- Continental plates are made of granite.
29Divergent Plate Boundaries
- Two land or ocean plates move apart in
opposite directions. Magma flows to the surface
between them creating new crust.
30Mid-Atlantic Ridge Divergent Boundary
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32http//www.geo.lsa.umich.edu/crlb/COURSES/270/Lec
12/spreexamples.jpeg
33 Iceland a continent directly over the
Mid-Atlantic Ridge
34Subduction Zones
- An ocean plate and a continental plate hit
head-on. The ocean plate subducts under the
continent forming a trench. The subducting plate
melts. Magma rises to the surface creating a
string of volcanic mountains parallel to the
shoreline.
35Andes Mountains
- Subduction zones form chains of volcanic
mountains along the shoreline.
36Collision Zones
- Two continents hit head-on, crinkling up the
land into a high mountain chain.
37Indias Collision with Asia
Himalayas
38The Himalayas Are Born
39Island Arcs
- Two ocean plates hit head-on. One ocean plate
is forced to subduct under the other forming an
ocean trench. The subducting plate melts. Magma
rises to the surface forming a string of volcanic
islands parallel to the trench.
40The Aleutian Islands
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42Key concepts
Forcestension, compression shearing
Ask a Geologist
Ask an earth scientist
43How does tectonic activity affect the earths
crust?
- Builds mountains
- Creates deep ocean trenches
- Causes earthquakes
- Create volcanoes
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46Ocean Trenches
http//www.nhusd.k12.ca.us/ALVE/wow/Ocean/seafloor
.gif
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49Volcanoes
50Most volcanoes occur at plate boundaries
51http//www.thirteen.org/savageearth/hellscrust/ass
ets/images/ringoffire.jpg
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54Real-world contexts
Recent patterns of earthquake and volcanic
activities maps showing the direction of
movement of major plates and associated
earthquake and volcanic activity Compressional
boundaries folded mountains, thrust faults,
trenches, lines of volcanoes (e.g. Pacific ring
of fire) Tensional boundaries mid-ocean
ridges, rift valleys Shearing boundaries
lateral movement producing faults (e.g. San
Andreas Fault).
55http//www.gfz-potsdam.de/pb2/pb22/projects/mamba.
html
56Resources
- http//www.calstatela.edu/faculty/acolvil/plates/p
angaea.jpg - http//platetectonics.pwnet.org/img/wegener.jpg
- http//home.tiscalinet.ch/biografien/images/wegene
r_kontinente.jpg - http//library.thinkquest.org/17457/platetectonics
/comic.jpg - http//www.soc.soton.ac.uk/CHD/classroom_at_sea/carls
berg/images/fossil_correlation_lge.jpg - http//earthobservatory.nasa.gov/Library/Giants/We
gener/Images/plate_boundaries.gif - http//www.calstatela.edu/faculty/acolvil/plates/a
tlantic_profile.jpg - http//pubs.usgs.gov/publications/graphics/Fig16.g
if - http//cps.earth.northwestern.edu/SPECTRA/IMG/basa
lt.png - http//cc.usu.edu/sharohl/granite.jpg
- http//tlacaelel.igeofcu.unam.mx/GeoD/figs/tgondv
ana_ice.jpg - http//www.physics.uc.edu/hanson/ASTRO/LECTURENOT
ES/F01/Lec11/Pangaea.gif - http//www.poleshiftprepare.com/glacial_striation.
jpg
57- http//www.ggs.org.ge/plates.jpg
- http//earth.geol.ksu.edu/sgao/g100/plots/1008_wor
ld_volc_map.jpg - http//www.aeic.alaska.edu/Input/affiliated/doerte
/personal/aleutians/ak_map_big.jpg - http//www.4reference.net/encyclopedias/wikipedia/
images/Aleutians_aerial.jpg - http//www.avo.alaska.edu/gifs/2-3/02-95-03.jpg
- http//www.soc.soton.ac.uk/CHD/classroom_at_sea/carls
berg/images/island_arc.jpg - http//nte-serveur.univ-lyon1.fr/nte/geosciences/g
eodyn_int/tectonique2/himalaya/images/Fig5a_inde.g
if - http//terra.kueps.kyoto-u.ac.jp/sake/himalaya.jp
g - http//www.andes.org.uk/peak-info-5000/sabancaya.j
pg - http//www-step.kugi.kyoto-u.ac.jp/keizo/photos/a
ndes.JPG - http//www.letus.northwestern.edu/projects/esp/top
10/andespage/andesphysical.jpg - http//www.soc.soton.ac.uk/CHD/classroom_at_sea/carls
berg/images/atlantic_tectonics20.jpg