Lithosphere
Lithosphere
The lithosphere is made of the Earth’s crust and upper mantle.
It is broken into large pieces called plates.
These plates move, which is called plate tectonics.
Plate movement changes the shape of the ocean floor.
Geological Features on the Ocean Floor
Continental shelf: Shallow ocean area around the edges of continents.
Seamounts: Underwater volcanoes that do not reach the ocean surface.
Volcanic islands: Form when volcanoes grow all the way up from the ocean floor to the surface.
Trenches: Form where two plates move toward each other.
Ridges: Form where plates move apart and molten rock rises from inside Earth.
Continental Drainage Systems
Mountain ranges help decide where water flows.
Glaciers
Glaciers are large moving bodies of ice.
Continental glaciers cover large land areas.
When snow and ice build up, glaciers start to move.
Valley glaciers move through mountain valleys.
Glaciers on the Move
Valley glaciers carry rocks of different sizes.
These rocks shape the land as the glacier moves.
Climate effects:
Colder climate → glacier grows and moves forward (advances).
Warmer climate → glacier melts and moves back (retreats), leaving rocks behind.
Glacial Features
Moraines: Piles of rocks and gravel
Eskers: Ridges of sand and gravel.
Drumlins: Small teardrop-shaped hills.