fossils, climate, continents fit like puzzle pieces transform boundary volcanic islands turbine/generator renewable resource organic precipitation granite folded mountains weathering and erosion biomass mountains, volcanoes, and deep ocean trenches mantle hydroelectric energy divergent boundary oceanic crust sediment earthquakes and tsunamis Pangaea topsoil runoff subsoil wind energy Continentia Drift nonrenewable resource magma cooling mid-ocean ridge and rift valleys inner core igneous rock combustion solar energy outer core evaporation sedimentary rock subduction zone seafloor spreading continental crust fossil fuel heat and pressure geothermal energy Alfred Wegener condensation metamorphic rock decrease increase faults crust nuclear energy transpiration cementation and compaction basalt petroleum nitrogen fixation convergent boundary fossils, climate, continents fit like puzzle pieces transform boundary volcanic islands turbine/generator renewable resource organic precipitation granite folded mountains weathering and erosion biomass mountains, volcanoes, and deep ocean trenches mantle hydroelectric energy divergent boundary oceanic crust sediment earthquakes and tsunamis Pangaea topsoil runoff subsoil wind energy Continentia Drift nonrenewable resource magma cooling mid-ocean ridge and rift valleys inner core igneous rock combustion solar energy outer core evaporation sedimentary rock subduction zone seafloor spreading continental crust fossil fuel heat and pressure geothermal energy Alfred Wegener condensation metamorphic rock decrease increase faults crust nuclear energy transpiration cementation and compaction basalt petroleum nitrogen fixation convergent boundary
(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.
fossils, climate, continents fit like puzzle pieces
transform boundary
volcanic islands
turbine/generator
renewable resource
organic
precipitation
granite
folded mountains
weathering and erosion
biomass
mountains, volcanoes, and deep ocean trenches
mantle
hydroelectric energy
divergent boundary
oceanic crust
sediment
earthquakes and tsunamis
Pangaea
topsoil
runoff
subsoil
wind energy
Continentia Drift
nonrenewable resource
magma cooling
mid-ocean ridge and rift valleys
inner core
igneous rock
combustion
solar energy
outer core
evaporation
sedimentary rock
subduction zone
seafloor spreading
continental crust
fossil fuel
heat and pressure
geothermal energy
Alfred Wegener
condensation
metamorphic rock
decrease
increase
faults
crust
nuclear energy
transpiration
cementation and compaction
basalt
petroleum
nitrogen fixation
convergent boundary