(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.
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Pacific Ring of Fire: Refers to the ring aroundthe Pacific Ocean where oceanic crust is being forced under continental crust creating much volcanic and seismic activity.
Mt. Saint Helens: Mt. St. Helens erupted in 1980, blanketing E. Washington in ash and providing scientists with an understanding of what is known as a lateral blast-an explosion that went outwards rather than upwards.
Columbia Basin: E. Washington region formed by lava flows-one of the great farming regions of the world.
Willapa Hills/Olympic Mountains: Land formed by oceanic crust being thrust upward, possibly by a huge seismic event.
Kootenay Arc: Continental Shelf caught between the Old NA Continent and the oncoming Okanogan Micro-Continent.
Anticline: A arched fold in layered rocks. Toppenish Ridge to the S., Rattlesnake R. to the N., are examples of anticlines.
Magma: Molten rock beneath the Earth’s surface-if it erupts from a volcano or otherwise vents it becomes known as lava.
Old North American Continent: Piece of the continent left after a portion of the continent broke off and drifted across the Atlantic Ocean.
Okanogan Highlands: Forested N.E. Washington region where people rely on resource related industries such as logging, mining, ranching as well as tourism as industries.
Cascade Volcanoes: Volcanoes that rose to start the creation of the Cascade Range, with the Pacific to the West
Cascade Mountains: Mountain range that splits E. Washington from W. Washington. Snowpack supplies water that people on both sides of the Cascades rely upon.
North Cascade Micro-Continent: Land that migrated across the Pacific and docked with the Okanogan Micro-Continent.
Fault: A fracture that separates blocks of the Earth’s crust that have slipped or slipping by each other. Zillah is close to two major faults.
Geology: Science that deals with Earth’s physical structure and substances, history, and the processes that act upon it.
Plate tectonics: The idea that the earth’s mantle is made of plates that are moving and shifting.
Columbia Plateau Lava Flows: Lava flows the emanated from NE Oregon that formed the Columbia Plateau, buried the inland sea and forced the Columbia R. into its course today.
Geography: The study of places and the relationships between people and their environment.
Great Floods: Floods that originated from glacier blocked Lake Missoula in MT that roared across E. Washington up to 40 times; effect can see up the Yakima R. to Zillah.
Puget Sound Trough: Land Gouged out by ice age glaciers to form Puget Sound as well as leaving large amounts of glacial till to the sounds and around it’s edges.
Syncline: A trough folded into layers. Zillah lies in a syncline between Toppenish Ridge, and Rattlesnake Ridge.
Okanogan Micro-Continent: Land that migrated across the Pacific and docked against the Old NA Continent, causing the rise of the Kootenay Arc.
Lithosphere: The relatively cool and rigid outer rind of the Earth, about 60 miles thick.
Coastal Region: Low range of hills to the South to the Olympic Mtns to the North-dominated by resource industries, logging, fishing as well as tourism.
Puget Sound Lowlands: Most heavily populated and urbanized region of WA, centering around Puget Sound.
