Paleocene- Eocene Thermal Maximum Magnetic North Eccentricity Little Ice Age Shield Volcano Obliquity Arkose Mastodon Fold-and- Thrust Belt Marble Swamp Trilobite Andesite Great Oxygenation Event Chicxulub Impact Abyssal Plain Marsh Brittle- Ductile Transition Moho Lower Mantle Shale Younger Dryas Pseudosuchus Sauropod Esker Turritella Precession Lithosphere Conodont Rhyolite Pliohippus Terabutulid Plateau Rhynchonella Azolla Event Conglomerate Gutenberg Discontinuity Mesozoic Marine Revolution Gabbro Quartzite Continental Shelf Hanging Valley Multituberculae Megalodon Alluvial Fan Aesthenosphere Outer Core Oceanic Crust The Archean Moraine Permo- Triassic Mass Extinction Granite Continental Crust Foreland Phyllite Atoll Schist Gneiss Assembly of Gondwana Dickinsonia Stratovolcano Inner Core Closing of the Tethys Seaway Canyon Closing of Western Interior Seaway Upper Mantle Hadrosaurus Cambrian Explosion Limestone Tiktaalik Great Ordovician Biodiversity Event Placoderm Breakup of Pangea Breccia Paleocene- Eocene Thermal Maximum Magnetic North Eccentricity Little Ice Age Shield Volcano Obliquity Arkose Mastodon Fold-and- Thrust Belt Marble Swamp Trilobite Andesite Great Oxygenation Event Chicxulub Impact Abyssal Plain Marsh Brittle- Ductile Transition Moho Lower Mantle Shale Younger Dryas Pseudosuchus Sauropod Esker Turritella Precession Lithosphere Conodont Rhyolite Pliohippus Terabutulid Plateau Rhynchonella Azolla Event Conglomerate Gutenberg Discontinuity Mesozoic Marine Revolution Gabbro Quartzite Continental Shelf Hanging Valley Multituberculae Megalodon Alluvial Fan Aesthenosphere Outer Core Oceanic Crust The Archean Moraine Permo- Triassic Mass Extinction Granite Continental Crust Foreland Phyllite Atoll Schist Gneiss Assembly of Gondwana Dickinsonia Stratovolcano Inner Core Closing of the Tethys Seaway Canyon Closing of Western Interior Seaway Upper Mantle Hadrosaurus Cambrian Explosion Limestone Tiktaalik Great Ordovician Biodiversity Event Placoderm Breakup of Pangea Breccia
(Print) Use this randomly generated list as your call list when playing the game. 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.
H-Paleocene-Eocene Thermal Maximum
E-Magnetic North
E-Eccentricity
H-Little Ice Age
T-Shield Volcano
E-Obliquity
R-Arkose
A-Mastodon
T-Fold-and-Thrust Belt
R-Marble
T-Swamp
A-Trilobite
R-Andesite
H-Great Oxygenation Event
H-Chicxulub Impact
T-Abyssal Plain
T-Marsh
E-Brittle-Ductile Transition
E-Moho
E-Lower Mantle
R-Shale
H-Younger Dryas
A-Pseudosuchus
A-Sauropod
T-Esker
A-Turritella
E-Precession
E-Lithosphere
A-Conodont
R-Rhyolite
A-Pliohippus
A-Terabutulid
T-Plateau
A-Rhynchonella
H-Azolla Event
R-Conglomerate
E-Gutenberg Discontinuity
H-Mesozoic Marine Revolution
R-Gabbro
R-Quartzite
T-Continental Shelf
T-Hanging Valley
A-Multituberculae
A-Megalodon
T-Alluvial Fan
E-Aesthenosphere
E-Outer Core
E-Oceanic Crust
H-The Archean
T-Moraine
H-Permo-Triassic Mass Extinction
R-Granite
E-Continental Crust
T-Foreland
R-Phyllite
T-Atoll
R-Schist
R-Gneiss
H-Assembly of Gondwana
A-Dickinsonia
T-Stratovolcano
E-Inner Core
H-Closing of the Tethys Seaway
T-Canyon
H-Closing of Western Interior Seaway
E-Upper Mantle
A-Hadrosaurus
H-Cambrian Explosion
R-Limestone
A-Tiktaalik
H-Great Ordovician Biodiversity Event
A-Placoderm
H-Breakup of Pangea
R-Breccia