Plates Asthenosphere and Lithosphere Volcanoes Third Layer Playdough or Putty Continental Crust Compass to Point North Oceanic Crust Pressure Increases Outermost Layer Outer Core Rocks Record Earth's History Iron and Magnesium Iron and Nickle Flow and Deform Inner Core Temp Oceans Rivers Thinnest Rocks/Dirt Outer Core Temp Solid Ball Crust Temp Mantle Continents Earth Science Mountains Geodynamo Second Layer Roughly 3/4 size of moon The Lithosphere Inner Core Fossils Thickest 4.6 Billion Years Atmosphere Reversed Polarity Liquid Soap/Hand Sanitizer Crust Innermost Layer Radiation Canyons Earthquakes Asthenosphere Caused by Pressure Tsunamis Geology Mantle Temp Constantly Changing Plates Asthenosphere and Lithosphere Volcanoes Third Layer Playdough or Putty Continental Crust Compass to Point North Oceanic Crust Pressure Increases Outermost Layer Outer Core Rocks Record Earth's History Iron and Magnesium Iron and Nickle Flow and Deform Inner Core Temp Oceans Rivers Thinnest Rocks/Dirt Outer Core Temp Solid Ball Crust Temp Mantle Continents Earth Science Mountains Geodynamo Second Layer Roughly 3/4 size of moon The Lithosphere Inner Core Fossils Thickest 4.6 Billion Years Atmosphere Reversed Polarity Liquid Soap/Hand Sanitizer Crust Innermost Layer Radiation Canyons Earthquakes Asthenosphere Caused by Pressure Tsunamis Geology Mantle Temp Constantly Changing
(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.
Plates
Asthenosphere and Lithosphere
Volcanoes
Third Layer
Playdough or Putty
Continental Crust
Compass to Point North
Oceanic Crust
Pressure
Increases
Outermost Layer
Outer Core
Rocks
Record Earth's History
Iron and Magnesium
Iron and Nickle
Flow and Deform
Inner Core Temp
Oceans
Rivers
Thinnest
Rocks/Dirt
Outer Core Temp
Solid Ball
Crust Temp
Mantle
Continents
Earth Science
Mountains
Geodynamo
Second Layer
Roughly 3/4 size of moon
The Lithosphere
Inner Core
Fossils
Thickest
4.6 Billion Years
Atmosphere
Reversed Polarity
Liquid Soap/Hand Sanitizer
Crust
Innermost Layer
Radiation
Canyons
Earthquakes
Asthenosphere
Caused by Pressure
Tsunamis
Geology
Mantle Temp
Constantly Changing