1. VOLCANO JEOPARDY Volcano Formation It’s Gonna Blow! Ashes to Ashes
100
200
300
400
500
It’s Gonna Blow!
100
200
300
400
500
Ashes to Ashes
100
200
300
400
500
Types of Volcanoes
100
200
300
400
500
Too Hot to Handle
100
200
300
400
500

2. TOO HOT TO HANDLE 100 A PERSON WHO STUDIES VOLCANOES VOLCANOLOGIST
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3. TOO HOT TO HANDLE 200 AN AREA AROUND THE PACIFIC RIM WHICH HAS
MANY ACTIVE VOLCANOES
THE RING OF FIRE
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4. TOO HOT TO HANDLE 300 A VOLCANO THAT’S BEEN KNOWN TO ERUPT WITHIN
MODERN TIMES BUT IS
NOW INACTIVE
DORMANT VOLCANO
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5. TOO HOT TO HANDLE 400 ONE IMPORTANCE IN KNOWING IF A VOLCANO
IS ACTIVE, DORMANT, OR
EXTINCT
TO SAVE LIVES AND
PROPERTY
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6. TOO HOT TO HANDLE 500 A CRATER THAT’S BECOME SO LARGE THAT ITS WALLS
HAVE COLLAPSED
CALDERA
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7. THE TYPE OF VOLCANO THAT FORMED THE HAWAAIN ISLANDS.
TYPES OF VOLCANOES 100
THE TYPE OF VOLCANO THAT FORMED THE HAWAAIN ISLANDS.
SHIELD VOLCANO
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8. TYPES OF VOLCANOES 200 A VOLCANO BUILT OUT OF ALTERNATING LAYERS OF
ROCK PARTICLES AND
LAVA
COMPOSITE VOLCANO
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9. TYPES OF VOLCANOES 300 THIS VOLCANO HAS A NARROW BASE, STEEP
SIDES AND FORMS FROM
EXPLOSIVE ERUPTIONS
CINDER CONE VOLCANO
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10. A GENTLY SLOPING, DOME- SHAPED MOUNTAIN WITH RUNNY LAVA AND QUIET
TYPES OF VOLCANOES 400
A GENTLY SLOPING, DOME-
SHAPED MOUNTAIN WITH
RUNNY LAVA AND QUIET
ERUPTIONS
A SHIELD VOLCANO
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11. The magma’s silica content and the properties of its magma,
TYPES OF VOLCANOES 500
The magma’s silica content
and the properties of its magma,
such as; temperature.
What are the factors that effect the force of a volcanic eruption?
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12. ASHES TO ASHES 100 A PASSAGEWAY IN THE VOLCANO THROUGH
WHICH THE LAVA RISES
PIPE
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13. ASHES TO ASHES 200 AN OPENING IN THE VOLCANO THROUGH WHICH THE LAVA
ERUPTS
VENT
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14. ASHES TO ASHES 300 HARDENED LAVA, ASHES, AND CINDER FORM THE TOP
OF THE VOLCANO, CALLED
THE
CONE
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15. ASHES TO ASHES 400 A FUNNEL SHAPED PIT OR DEPRESSION AT THE TOP
OF THE VOLCANIC CONE
CRATER
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16. ASHES TO ASHES 500 THESE MOLTEN VOLCANIC BOMBS HARDEN AS THEY
TRAVEL THROUGH THE AIR
AND ARE ABOUT THE SIZE
OF GOLF BALLS
CINDERS
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17. PAHOEHOE AN aa ARE PRODUCED DURING THESE TYPES OF ERUPTIONS
IT’S GONNA BLOW! 100
PAHOEHOE AN aa ARE PRODUCED DURING THESE TYPES OF ERUPTIONS
QUIET
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18. FORMEND WHEN THE PLATE MOVEMENTS CAUSE THE CRUST TO BEN DOWNWARD.
IT’S GONNA BLOW! 200
FORMEND WHEN THE PLATE MOVEMENTS CAUSE THE CRUST TO BEN DOWNWARD.
BASIN
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19. IT’S GONNA BLOW! 300 A HUGE WAVE CAUSED BY AN UNDERSEA ERUPTION
AND LANDSLIDE
TSUNAMI
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20. IT’S GONNA BLOW! 400
A MASS OF ROCK THAT FORMED WHEN A LARGE BODY OF MAGMA COOLED INSIDE EARTH’S CRUST
BATHOLITH
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21. IT’S GONNA BLOW! 500
LAYERS OF THIN, RUNNY LAVA THAT FLOW OVER A WIDE AREA BEFORE THEY COOL AND HARDEN
LAVA PLATEAU
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22. VOLCANO FORMATION 300 WEAK AREAS IN THE EARTH’S CRUST THROUGH
WHICH MAGMA MAY
ERUPT
HOT SPOT
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23. VOLCANIC SOILS ARE FERTILE BECAUSE THEY CONTAIN THESE ELEMENTS
VOLCANO FORMATION 400
VOLCANIC SOILS ARE FERTILE BECAUSE THEY CONTAIN THESE ELEMENTS
POTASSIUM & PHOSPHORUS
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24. VOLCANO FORMATION 500 ASH, LAVA, AND GAS MOVING DOWN THE SIDE
OF A VOLCANO
PYROCLASTIC FLOW
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25. VOLCANO FORMATION 100 A HOT LIQUID THAT EXISTS DEEP WITHIN THE EARTH
MAGMA
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26. VOLCANO FORMATION 200 MAGMA THAT HAS REACHED THE EARTH’S SURFACE LAVA
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