The thinner oceanic plate is pushed down below the thicker continental plate
converge - plates come together
Mid-oceanridges form where molten rock pushes up from the interior of Earth
two plates push up against each other
transform - plates slide past one another
creates faults and earthquakes
seamounts - underwater volcanoes that do not come all the way out to the ocean’s surface
volcanic islands - Formed by volcanoes that grow all the way up to the ocean’s surface
continental shelf - Shallow areas around the edges of continents
mountains - two continental plates converge
Glaciers: large moving body of ice
Continental Glaciers: Cover vast areas of land (ice caps)
Valley Glaciers: form high up in the mountains and as they accumulate more snow & ice, they begin to move downthrough the high valleysbetween the mountain peaks
glacier growth
If it stays cold, the glacier will continue to buildup and move forward/advance (get larger)
If it warms up, meltingoccurs leading to the glacier melting back/retreating (get smaller)
moraines - A build up of rocks and gravel that form alongsides & at the end of a glacier
esker - Long,winding ridge of sand & gravel that forms when parts of the glaciersmelt
drumlins - Small hills with distinctive teardropshape; form when a glacier moves over moraines that had formed earlier
kettle lakes - Formed when largechunks of ice, left behind by a glacier, meltaway
striations - scratches on rocks from glaciers moving over them