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Continents are moving across the Earth's Surface under the Continental drift One continent is moving significantly more slowly than the others because of plate tectonics.
Volcanoes are caused by geothermal energy bursting through the surface of the earth.Continental drift is caused by geothermal energy moving the continents very slowly across the surface of the earth.
Yes. The tectonic plates are still moving, erosion is still taking place, some mountains continue to grow, and volcanoes continue to erupt new material.
Wind and moving water reshape the Earth's surface through the process of erosion.
Energy
depends, but on mine yes
Advection fog results when moist air moved across a cold surface. When moving across a cold surface, the air is cooled to its dew point.
Advection fog results when moist air moved across a cold surface. When moving across a cold surface, the air is cooled to its dew point.
Both forces shape the surface of the earth. They are always changing and moving.
Continents are moving across the Earth's Surface under the Continental drift One continent is moving significantly more slowly than the others because of plate tectonics.
Any object moving at a certain speed relative to the surface with which it is in contact. (A car moving on a road)
lava moving in between the cracks of the earths surface and pushing rocks together and apart.
rocks
Rapidly moving air moving horizontally across the earth's surface which causes injury or harm that reduces value or usefulness.
If the bag is sliding across the countertop (i.e., the same surface of the bag is always in contact with the counter), then no. Rolling friction is only relevant when the surface of an object in contact with the surface it moves across always changes.
The tendency of fluids moving across the Earth's surface to be deflected from a straight line path.
Assuming you mean water in a pipe, the speed of the moving water can be changed by changing the pressure, the force pushing the water. It can also be changed by changing the characteristics of the pipe (larger, smoother inner walls, etc.)