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Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team members to teach themselves.
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Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Dec 14, 2015

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Page 1: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Dynamic Planet2nd year

Volcanoes and Earthquakes

I have approached this event by teaching a-q as individual sessions. Using the computer allows the team

members to teach themselves.

Page 3: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

http://wapi.isu.edu/EnvGeo/EG6_volcano/volcanoes.htmReview the powerpoint show and look at the links at the end of the reading.

http://www.scarborough.k12.me.us/wis/teachers/dtewhey/webquest/nature/volcanoes.htm

http://www.tulane.edu/~sanelson/geol111/igneous.htmExcellent site for rock information! Must see

Page 4: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Shield Volcano

A shield volcano  is is typically built by eruptions of fluid, basaltic lava. The take on the appearance of shield with the convex side facing upward. The Hawaiian Islands are an example of shield volcanoes.

Page 5: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Shield Volcano

Page 6: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Composite Volcano

A composite volcano is built by alternating eruptions of lava and pyroclastic material. Composite volcanoes, also called stratovolcanoes, form tall conical mountains.

Page 7: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 8: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Cinder Cone

Cinder cones  are constructed from the deposition of cinders and other pyroclastic material. Tend to be smaller in height than stratovolcanoes and have an asymetric cone.

Page 9: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Lava Dome

http://en.wikipedia.org/wiki/Lava_dome

Page 10: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Kinds of Eruptions

http://videos.howstuffworks.com/howstuffworks/231-how-volcanoes-work-video.htm (How volcanoes work 3:03)

http://library.thinkquest.org/17457/volcanoes/legend.php

Page 11: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Volcanic HazardsLava Flows

3 Major Types of Lava Flow

aa, pahoehoe, and pillow lavagood pictures at Wikipedia

http://library.thinkquest.org/17457/volcanoes/hazards.lavaflow.php

Page 12: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 13: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Volcanic Hazards - Lahar

Lahar mudflow of volcanic ash and dust created when pyroclastic material is mobilized by melting snow or rain. An extremely dangerous environmental hazard.

http://www.uwsp.edu/geo/faculty/ritter/glossary/Default.htm

Excellent site – GLOSSARY with Pictures

Page 14: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Volcano Hazards

http://www.cotf.edu/ete/modules/volcanoes/vhazards.html

Page 15: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Volcanic Features

Using Google video, research “crater lake”. A nice 1:04 video by Britannica.org is available from youtube.com.

Page 16: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Volcanic Features

Should be able to identify and explain how this feature became to be.

Page 18: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Rockshttp://www.scarborough.k12.me.us/wis/teachers/dtewhey/webquest/nature/rocks.htm

Page 19: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Seismograms and Characteristics of P, S,

and Love Waves

You should know which of the waves is the fastest, how the waves travels, which is considered body vs. surface waves,

and HOW to determine the epicenter!http://www.seismo.unr.edu/ftp/pub/louie/class/100/seismic-waves.html

http://www.scarborough.k12.me.us/wis/teachers/dtewhey/webquest/nature/seismic_waves.htm (Especially Seismic Images)

http://www.youtube.com/watch?v=7EgxHf0PMRU&feature=player_embedded

(Primary, Secondary, and Surface Waves)

Page 20: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Determine the Epicenterhttp://regentsprep.org/regents/earthsci/eqwaves.htm

Good starting site!

http://regentsprep.org/Regents/core/questions/question.cfm?Course=ESCI&TopicCode=05&QNum=1&Wrong=0 - Practice Questions

http://nemo.sciencecourseware.org/VirtualEarthquake/ - MUST DO!

Page 21: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Earth’s Interior

Be able to name the various layers

Why the layers are important?

Where are the layers found?

Page 22: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Moho Layer(Where and) Why is this layer important?

The boundary where Earth's crust meets Earth's upper mantle (approximately 31 mi/50 km below the surface), and where seismic waves travel at a different and more rapid rate than the crust or mantle.

Page 23: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Faults

http://facweb.bhc.edu/academics/science/harwoodr/GEOL101/study/structur.htm

Very good site with a lot of good pictures

Page 24: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 25: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 26: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 27: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 28: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Measuring Ground Movement

Mercalli Scale vs. Richter Scale

Intensity should not be confused with magnitude

http://earthquake.usgs.gov/learning/topics/richter.php

http://www.seismo.unr.edu/ftp/pub/louie/class/100/mercalli.html (Mercalli Scale)

http://www.seismo.unr.edu/ftp/pub/louie/class/100/mercalli.html

(Richter Scale)

Page 29: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Interpret Isoseismic Lineshttp://www.csulb.edu/~rodrigue/geog458558/labs/isoseism.html

Reinforces the difference between Richter Scale and Mercalli Scale and how to make and read

isoseismal map

Page 30: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Emergency Preparedness

http://www.fema.gov/areyouready/basic_preparedness.shtmhttp://www.hampton.gov/eoc/emergency_preparedness.html

Page 31: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Climate Change as related to volcanic activity

http://www.cotf.edu/ete/modules/volcanoes/vclimate.html

You should be able to understand the short term and long term effects. What gases are released and why are these gases important to the weather/climate? What level of the atmosphere does gases affected the climate? What is the “Year without a Summer”?

For help, you should be able to ask last year’s Meteorology team members.

Page 32: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Topographic Map

http://regentsprep.org/Regents/earthsci/units/mapping/topographic.cfm - Good background

http://www.cs.nmsu.edu/~jbj/index_auxil/idaho_virtual_campus/topo_profiles.htm - Creating topographic profile

http://www.geo.ua.edu/geowall/downloads/contour-student_guide.pdf - Topography and contouring (a good homework assignment – also great for ROAD SCHOLAR)

http://egsc.usgs.gov/isb/pubs/booklets/symbols/- also great for ROAD SCHOLAR

Page 33: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Plate Tectonics

Plate tectonics is the geophysical theory in which the earth's crust is broken into huge plates that move about laterally and vertically. The interaction of lithospheric plates creates second order relief features of the earth, e.g. mountain chains, deep valleys.

Page 34: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Plate Boundaries(1) Convergent, (2) Divergent and (3) Transform

Begins with slide no. 17http://www.sci.csuhayward.edu/~lstrayer/geol2101/2101_Ch19_03.pdf (excellent site, must see!)

http://www.indiana.edu/~g103/G103/week11/week11.htm

Page 35: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Plate Boundarieshttp://www.scarborough.k12.me.us/wis/teachers/dtewhey/webquest/nature/

plate%20boundaries.htm

Cross sectional Model of a plate boundary

Page 36: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Features of Various Plate Boundaries

http://www.indiana.edu/~g103/G103/week11/week11.htm

Page 37: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Should know what type of plate, why it is important, and what is occurring along the

Ring of Fire

Page 38: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Evidence of Continental Drift

(1) Fit of the Continents(2) Fossil Evidence(3) Rock Type and Structural Similarities(4) Paleoclimatic Evidence

http://www.sci.csuhayward.edu/~lstrayer/geol2101/2101_Ch19_03.pdf

Page 39: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

(2) Fossil Evidence (1) Fit of the Continents

Page 40: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Evidence of Sea Floor Spreading http://www.sci.csuhayward.edu/~lstrayer/geol2101/2101_Ch19_03.pdf

Nice Videos (Sea Floor Spreading 1:11, Mid Atlantic Ridge :57) http://videos.howstuffworks.com/science-channel/29268-100-greatest-discoveries-sea-floor-spreading-video.htmA lot of videos other good stuff…just need to look around

http://video.yahoo.com/watch/1595570/5390151Bill Nye’s Sea Floor Spreading for the Discovery Channel

Page 41: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 42: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Sea-floor spreading occurs where oceanic plates are diverging from one another. Magma rises along a rift zone and spreads out at the surface building new sea floor. As a result, the age of the rocks increases as one moves away from the rift zone. The mid-oceanic ridge is the primary site for sea-floor spreading. Earthquakes and volcanoes are where sea floor spreading is occurring.

Page 43: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 44: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Magnetic stripes record the magnetic polarization of iron-bearing rocks from a magnetometer. Deciphering magnetic stripes was one of the pieces of evidence to support the theory of sea floor spreading and plate tectonics.

Page 45: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 46: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

Tsunami

Earthquakes, volcanoes and mudslideshttp://en.wikipedia.org/wiki/Tsunami

http://web.mit.edu/12.000/www/m2009/teams/5/research.html

Page 47: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.
Page 48: Dynamic Planet 2 nd year Volcanoes and Earthquakes I have approached this event by teaching a-q as individual sessions. Using the computer allows the team.

http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/contents.htmlUnbelievable Great Site for a lot more events!