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

TOO HOT TO HANDLE 100 A PERSON WHO STUDIES VOLCANOES VOLCANOLOGIST Return to board

TOO HOT TO HANDLE 200 AN AREA AROUND THE PACIFIC RIM WHICH HAS MANY ACTIVE VOLCANOES THE RING OF FIRE Return to board

TOO HOT TO HANDLE 300 A VOLCANO THAT’S BEEN KNOWN TO ERUPT WITHIN MODERN TIMES BUT IS NOW INACTIVE DORMANT VOLCANO Return to board

TOO HOT TO HANDLE 400 ONE IMPORTANCE IN KNOWING IF A VOLCANO IS ACTIVE, DORMANT, OR EXTINCT TO SAVE LIVES AND PROPERTY Return to board

TOO HOT TO HANDLE 500 A CRATER THAT’S BECOME SO LARGE THAT ITS WALLS HAVE COLLAPSED CALDERA Return to board

THE TYPE OF VOLCANO THAT FORMED THE HAWAAIN ISLANDS. TYPES OF VOLCANOES 100 THE TYPE OF VOLCANO THAT FORMED THE HAWAAIN ISLANDS. SHIELD VOLCANO Return to board

TYPES OF VOLCANOES 200 A VOLCANO BUILT OUT OF ALTERNATING LAYERS OF ROCK PARTICLES AND LAVA COMPOSITE VOLCANO Return to board

TYPES OF VOLCANOES 300 THIS VOLCANO HAS A NARROW BASE, STEEP SIDES AND FORMS FROM EXPLOSIVE ERUPTIONS CINDER CONE VOLCANO Return to board

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 Return to board

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? Return to board

ASHES TO ASHES 100 A PASSAGEWAY IN THE VOLCANO THROUGH WHICH THE LAVA RISES PIPE Return to board

ASHES TO ASHES 200 AN OPENING IN THE VOLCANO THROUGH WHICH THE LAVA ERUPTS VENT Return to board

ASHES TO ASHES 300 HARDENED LAVA, ASHES, AND CINDER FORM THE TOP OF THE VOLCANO, CALLED THE CONE Return to board

ASHES TO ASHES 400 A FUNNEL SHAPED PIT OR DEPRESSION AT THE TOP OF THE VOLCANIC CONE CRATER Return to board

ASHES TO ASHES 500 THESE MOLTEN VOLCANIC BOMBS HARDEN AS THEY TRAVEL THROUGH THE AIR AND ARE ABOUT THE SIZE OF GOLF BALLS CINDERS Return to board

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 Return to board

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 Return to board

IT’S GONNA BLOW! 300 A HUGE WAVE CAUSED BY AN UNDERSEA ERUPTION AND LANDSLIDE TSUNAMI Return to board

IT’S GONNA BLOW! 400 A MASS OF ROCK THAT FORMED WHEN A LARGE BODY OF MAGMA COOLED INSIDE EARTH’S CRUST BATHOLITH Return to board

IT’S GONNA BLOW! 500 LAYERS OF THIN, RUNNY LAVA THAT FLOW OVER A WIDE AREA BEFORE THEY COOL AND HARDEN LAVA PLATEAU Return to board

VOLCANO FORMATION 300 WEAK AREAS IN THE EARTH’S CRUST THROUGH WHICH MAGMA MAY ERUPT HOT SPOT Return to board

VOLCANIC SOILS ARE FERTILE BECAUSE THEY CONTAIN THESE ELEMENTS VOLCANO FORMATION 400 VOLCANIC SOILS ARE FERTILE BECAUSE THEY CONTAIN THESE ELEMENTS POTASSIUM & PHOSPHORUS Return to board

VOLCANO FORMATION 500 ASH, LAVA, AND GAS MOVING DOWN THE SIDE OF A VOLCANO PYROCLASTIC FLOW Return to board

VOLCANO FORMATION 100 A HOT LIQUID THAT EXISTS DEEP WITHIN THE EARTH MAGMA Return to board

VOLCANO FORMATION 200 MAGMA THAT HAS REACHED THE EARTH’S SURFACE LAVA Return to board