what move tectonic plates around earth?and how does it move the plates?

Well, you see, it's actually a giant underground dance party! The tectonic plates shimmy and shake to the beat of the Earth's core. It's like a never-ending dance-off down there!

Okay, on a serious note, tectonic plates are moved by the forces in the Earth's mantle. These forces can be caused by a variety of factors, such as convection currents. It's like a big, slow-motion game of bumper cars down there, with the plates being pushed, pulled, and scraped against each other. So, no dance party, I'm afraid, just some really slow and powerful movements beneath the Earth's surface.

wha evidence gave proof that pangeaea drift into continents?

Check these sites.

http://www.moorlandschool.co.uk/earth/tectonic.htm

http://library.thinkquest.org/17701/high/pangaea/

its a guess

such as earthquakes

Plates at our planet’s surface move because of the intense heat in the Earth’s core that causes molten rock in the mantle layer

The movement of tectonic plates on Earth is primarily driven by a process called plate tectonics. Plate tectonics is driven by two main forces:

1. Mantle Convection: The Earth's interior is made up of several layers, with the asthenosphere being a semi-fluid layer in the upper part of the mantle. Heat from the Earth's core causes convection currents within the asthenosphere, where hotter, less dense material rises, and cooler, denser material sinks. This convection process creates a dragging force that drives the movement of the tectonic plates.

2. Ridge Push and Slab Pull: At the mid-ocean ridges, new seafloor is constantly being created as magma rises from the asthenosphere and solidifies. As the newly formed seafloor spreads away from the ridge, it pushes the older, colder oceanic crust aside. This is known as ridge push. Additionally, in subduction zones, where one tectonic plate (usually an oceanic plate) is forced beneath another plate (usually a continental plate), gravity pulls denser oceanic lithosphere down into the mantle. This pulling force is known as slab pull.

These driving forces cause the tectonic plates to move in different ways:

1. Divergent Boundaries: When tectonic plates move apart, this creates a divergent boundary. Magma rising from beneath the Earth's surface fills the gap, solidifies, and forms new crust. This process occurs along mid-ocean ridges, creating new oceanic crust.

2. Convergent Boundaries: When tectonic plates collide, this creates a convergent boundary. The type of convergence depends on the types of plates involved. If two oceanic plates collide, one will be forced beneath the other into the mantle, forming a subduction zone. If an oceanic plate collides with a continental plate, the denser oceanic plate will typically subduct beneath the continental plate. If two continental plates collide, they usually form mountain ranges.

3. Transform Boundaries: When tectonic plates slide past each other horizontally, this creates a transform boundary. Here, plates grind past each other, causing earthquakes.

In summary, the movement of tectonic plates on Earth is primarily driven by mantle convection, ridge push, and slab pull. These processes result in the creation of new crust at divergent boundaries, subduction at convergent boundaries, and horizontal sliding at transform boundaries.