precipitation fossils, climate, continents fit like puzzle pieces basalt nonrenewable resource subduction zone nuclear energy transpiration igneous rock turbine/generator increase crust organic condensation runoff convergent boundary combustion solar energy evaporation sediment inner core wind energy fossil fuel nitrogen fixation volcanic islands earthquakes and tsunamis granite mantle Pangaea faults biomass folded mountains mountains, volcanoes, and deep ocean trenches petroleum metamorphic rock renewable resource oceanic crust mid-ocean ridge and rift valleys continental crust transform boundary cementation and compaction heat and pressure Continentia Drift topsoil decrease hydroelectric energy sedimentary rock weathering and erosion Alfred Wegener subsoil outer core divergent boundary geothermal energy magma cooling seafloor spreading precipitation fossils, climate, continents fit like puzzle pieces basalt nonrenewable resource subduction zone nuclear energy transpiration igneous rock turbine/generator increase crust organic condensation runoff convergent boundary combustion solar energy evaporation sediment inner core wind energy fossil fuel nitrogen fixation volcanic islands earthquakes and tsunamis granite mantle Pangaea faults biomass folded mountains mountains, volcanoes, and deep ocean trenches petroleum metamorphic rock renewable resource oceanic crust mid-ocean ridge and rift valleys continental crust transform boundary cementation and compaction heat and pressure Continentia Drift topsoil decrease hydroelectric energy sedimentary rock weathering and erosion Alfred Wegener subsoil outer core divergent boundary geothermal energy magma cooling seafloor spreading
(Print) Use this randomly generated list as your call list when playing the game. There is no need to say the BINGO column name. Place some kind of mark (like an X, a checkmark, a dot, tally mark, etc) on each cell as you announce it, to keep track. You can also cut out each item, place them in a bag and pull words from the bag.
precipitation
fossils, climate, continents fit like puzzle pieces
basalt
nonrenewable resource
subduction zone
nuclear energy
transpiration
igneous rock
turbine/generator
increase
crust
organic
condensation
runoff
convergent boundary
combustion
solar energy
evaporation
sediment
inner core
wind energy
fossil fuel
nitrogen fixation
volcanic islands
earthquakes and tsunamis
granite
mantle
Pangaea
faults
biomass
folded mountains
mountains, volcanoes, and deep ocean trenches
petroleum
metamorphic rock
renewable resource
oceanic crust
mid-ocean ridge and rift valleys
continental crust
transform boundary
cementation and compaction
heat and pressure
Continentia Drift
topsoil
decrease
hydroelectric energy
sedimentary rock
weathering and erosion
Alfred Wegener
subsoil
outer core
divergent boundary
geothermal energy
magma cooling
seafloor spreading