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Stack #1915322

GR. 7 OCEANS

QuestionAnswer
ABYSSAL PLAINS LARGE, FLAT AREAS ON THE SEAFLOOR THAT EXTEND ACROSS THE DEEPEST PARTS OF THE OCEAN BASIN
SEAWATER WATER FROM THE OCEAN THAT HAS AVERAGE SALINITY OF .35 PPT
TSUNAMI WAVE THAT FORMS WHEN AN OCEAN DISTURBANCE SUDDENLY MOVES A LARGE VOLUME OF WATER
MID OCEAN RIDGE LONG, NARROW MOUNTAIN RANGE ON OCEAN FLOOR FORMED BY MAGMA FROM DIVERGENT PLATE BOUNDARIES AT ITS CENTER
CONTINENTAL SLOPE PART OF THE CONTINENT BETWEEN THE CONTINENTAL SHELF AND THE OCEAN FLOOR
CONTINENTAL SHELF PART OF THE CONTINENT THAT SLOPES GENTLY AWAY FROM THE SHORELINE
CREST HIGHEST POINT OF A WAVE
EBB TIDE OUTGOING TIDE
FLOOD TIDE INCOMING OR RISING TIDE
GUYOT FLAT TOPPED SEAMOUNT AKA TABLEMOUNT
SALINITY THE AMOUNT OF DISSOLVED SALTS IN THE OCEAN WATER
SEAMOUNT VOLCANIC MOUNTAIN ON OCEAN FLOOR
TIDE REGULAR CHANGE IN THE WATER LEVEL OF EARTH'S OCEANS
TRENCH DEEP CRACK OR CANYON ON THE OCEAN FLOOR....OLD OCEAN FLOOR IS SUBDUCTED HERE
TROUGH LOWEST POINT OF A WAVE
WAVE REGULAR UP AND DOWN MOVEMENT OF WATER
RIFT VALLEY DEEP, V SHAPED VALLEY IN THE CENTER OF THE MID OCEAN RIDGE. NEW OCEAN FLOOR IS CREATED HERE.
Created by: harding48193
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