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IS THERE A RELATIONSHIP BETWEEN
   TYPE OF PLATE BOUNDARY AND
       TYPE OF VOLCANOES?
            Period 1
PROCEDURE
• Obtain Excel data file of almost 1500
  volcanoes located around the world
• Group descriptions into the major types of
  volcanoes – cinder, shield, and composite
SMALL EXAMPLE OF THE DATA
                                  LOCATI
NUMBER     RN SN   VN     NAME ON          STATUS LATX   NS   VF   LONGX EW   ELEV   TYPE          TIMEFRAME
                          Kars             Holocen
0103-05-   01 03   -05-   Plateau Turkey   e?       40.75N    *       42.9E     3000Cinder cone    ?
                          Ghegam Armeni    Anthrop
0104-07-   01 04   -07-   Ridge a          ology   40.275N    *      44.75E     3597Cinder cone    D7
                                           Holocen                 42.5333
0201-124   02 01   -124   Gufa    Ethiopia e        12.55N    *          3E      600Cinder cone    U
                          Assab
                          Volc             Holocen                 42.4333
0201-125   02 01   -125   Field   Ethiopia e         12.95N   *          3E      987Cinder cone    U
                                           Holocen
0201-191   02 01   -191   Beru    Ethiopia e          8.95N          39.75E     1100Cinder cone    U
                          Chyulu           Anthrop       -         37.8833
0202-13=   02 02   -13-   Hills   Africa-E ology 2.68333S     *          3E     2188Cinder cone    D3
                          Ngaoun
                          dere    Africa- Holocen                  13.6666
0204-04-   02 04   -04-   Plateau W        e?         7.25N   *          7E          Cinder cone   ?
                          Biu     Africa- Holocen
0204-05-   02 04   -05-   Plateau W        e?        10.75N   *        12E           Cinder cone   ?
                          Tin
                          Zaouate
                          ne Volc          Holocen 19.8333         2.83333
0205-002   02 05   -002   Field   Africa-N e             3N   *          3E          Cinder cone   U
                          In
                          Ezzane
                          Volc             Holocen                 10.8333
0205-003   02 05   -003   Field   Africa-N e?           23N   *          3E          Cinder cone   ?
                                           Holocen
0205-007   02 05   -007   Haruj Africa-N e           27.25N   *       17.5E     1200Cinder cone    U
USING AEJEE PLOT THE DATA
PLATE BOUNDARIES
TEAM WORK
• Randomly teams of three students will be given a
  specific area of the world that has a lot of
  volcanic activity.
• It is the team’s responsibility to do the following:
   – ‘code’ the volcanoes and screen capture their area
   – Using Google Earth, map out the boundary and screen
     capture their area
   – Determine the type of plate boundary
   – Determine the main type of volcanic activity at this
     location
PRESENTATION
• Create powerpoint slides that show the screen
  capture from AEJEE and Google Earth
• Include a graphic that illustrates an example of
  this type of volcano from this area

• As a class, create one sentence that shows the
  relationship between that specific plate
  boundary and the main type of volcanic
  eruption
GROUP 1
• Alexis
• Daniel C
• Ashton
Aleutian Islands
GOOGLE EARTH



     NORTH
     AMERICAN
     PLATE –
     OCEANIC




PACIFIC PLATE - OCEANIC
TYPE OF PLATE BOUNDARY
• CONVERGENT
• OCEANIC-OCEANIC

• Composite – tall, steep sided volcanoes,
  explosive eruptions
TYPE OF VOLCANO: COMPOSITE




         MT. CLEVELAND
GROUP 2
• ASIA J
• CARLOS M
• JULIAN S
Andes, South America
GOOGLE EARTH


           SOUTH
           AMERICAN
           PLATE -
           CONTINENTAL

 NAZCA
 PLATE -
 Oceanic
TYPE OF PLATE BOUNDARY




 CONVERGENT – OCEANIC/CONTINENTAL
MAIN TYPE OF VOLCANO




         LASCAR VOLCANO
GROUP 3
• Mary S
• Tatiana R
• Juan R
Central America
VIEW via GOOGLE EARTH



       NORTH AMERICAN
       PLATE -
       CONTINENTAL
                    CARRIBEAN PLATE -
                    CONTINENTAL
  COCOS OCEANIC
  PLATE
TYPE OF PLATE BOUNDARY
• CONVERGENT PLATE BOUNDARY between the
  Cocos Plate on the west that is an oceanic
  plate and the Caribbean Plate on the east that
  is a continental plate
TYPE OF VOLCANO




 ARENAL VOLCANO, COSTA RICA
 is an example of the volcanoes
 here.
TEAM 4
• Taylor C
• Joel C
• Chanel S
East African Rift Zone
View from Google Earth
    AFRICAN
    PLATE



              AFRICAN PLATE
TYPE OF PLATE BOUNDARY
TYPE OF VOLCANO




    SHIELD VOLCANO
    MT. KILAMANJERO
GROUP 5
• Tyler F
• Marcus B
• Myles A
Cascades, Northwest US
Google Earth Screen Shot

    Juan de
              North
    Fuca
              American
    Plate -
              Plate -
    Oceanic
              Continental
TYPE OF PLATE BOUNDARY
TYPE OF VOLCANO




   MT. ST. HELENS
GROUP 6
• Alexandra C
• Caitlyn G
• Terrance E
Caribbean
Google Earth


           OCEANIC


 OCEANIC
TYPE OF PLATE BOUNDARY
TYPE OF VOLCANO




      MT. PELEE
GROUP 7
• Austin
• Ashley
• Chandler
Galapagos Islands
TYPE OF VOLCANO
TYPE OF PLATE BOUNDARY
• NONE – HOT SPOT
GROUP 8
• Kira M
• Cole P
Iceland
Google Earth


                          EURASIAN
                          PLATE



NORTH
AMERICAN
PLATE
TYPE OF PLATE BOUNDARY
      DIVERGENT
TYPE OF VOLCANO




  Eyafjallajökull volcano
GROUP 9
• Gustavo
• Brandon G
• Ricky
Indonesia
GOOGLE EARTH


           OCEANIC



OCEANIC
TYPE OF PLATE BOUNDARY
TYPE OF VOLCANO




  Mahameru (Semeru) above Mount
  Bromo, East Java
             COMPOSITE
GROUP 11
• COLE
• KATRINA
• COTY
Japan
GOOGLE EARTH

  CONTINENTAL
  North American


                   OCEANIC
                   Pacific Plate
TYPE OF VOLCANO




      MT. FUJI
TYPE OF PLATE BOUNDARY
GROUP 12
• Jeremy M
• Bryce M
• Andrew M
Juan De Fuca
GOOGLE EARTH



          JUAN
PACIFIC   DE
PLATE     FUCA
TYPE OF PLATE BOUNDARY
TYPE OF VOLCANO




PILLOW LAVAS – develop on the ocean
floor; if keep growing would be a shield
volcano
GROUP 13
• Shannen
• Callan
Mariana Trench
GOOGLE EARTH


             PACIFIC PLATE

PHILIPPINE
PLATE
TYPE OF PLATE BOUNDARY
TYPE OF VOLCANO




    PILLOW LAVA
CLASS FINDINGS
• DIVERGENT PLATE BOUNDARIES are
  characterized by pillow lavas and shield
  volcanoes. This is because the magma is
  coming from the mantle and is low in silica.
  This produces short, broad volcanoes with
  quiet eruptions.
• CONVERGENT BOUNDARIES produce very
  explosive volcanic eruptions characterized by
  composite volcanoes such as Mt. Fuji and Mt.
  St. Helens. These volcanoes are the result of
  the subducting plate being melted and coming
  back to the surface as a composite volcanic
  eruption either in islands or mountains.

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AEJEE Volcanoes and Plate Boundaries