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2024 PLATE TECTONICS

Across
BOUNDARY WHEN PLATES MOVE TOGETHER
A LONG NARROW HILLTOP OR MOUNTAIN RANGE
MASS DIVIDED BY VOLUME
SCIENTIST THAT STUDIES THE EARTH
LAYER OF THE EARTHS CRUST THAT MOVES, FLOAT AND FRACTURE
WHERE A LARGE NUMBER OF EARTHQUAKES AND VOLCANOS ERUPT
THESE RESULT FROM CONVECTIVE FLOW.
SCIENTIST THAT CAME UP WITH THE PANGAEA IDEA
THICKEST LAYER OF THE EARTH
COUNTRY WHERE MID ATLANTIC RIDGE IS VISIBLE ABOVE GROUND
BOUNDARY WHERE PLATES MOVE APART
Down
A MOUNTAIN THAT ERUPTS LAVA
TOP LAYER OF THE EARTH
A LONG NARROW DITCH ON THE OCEAN FLOOR
RIGID OUTER PART OF THE EARTH
THE SIDEWAY AND DOWNWARD MOVEMENT OF A PLATE.
SLOW MOVEMENT OF CONTINENTS ACROSS THE EARTHS SURFACE
THE STRONGEST EVIDENCE FOR PANGAEA
MOUNTAIN RANGE AT THE MIDDLE OF THE ATLANTIC COEAN
CENTER LAYER OF THE EARTH
NAME OF THE SUPER CONTINENT
BOUNDARY WHERE PLATES SLIDE PAST EACH OTHER