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  2. Learn what a transform boundary is and how it forms when two plates slide past each other horizontally. See examples of transform faults and plate boundaries, such as the San Andreas Fault and the Pacific Ocean Ring of Fire.

  3. Learn about the movement of tectonic plates and the three types of boundaries: convergent, divergent, and transform. A transform boundary is where two plates slide past each other, causing faults and earthquakes.

  4. As the plates move, they may converge, or come together; diverge, or spread apart; or slide past each other along fractures called transform faults. Convergent Boundaries. Plates move toward each other at convergent boundaries. Generally, if two plates are converging, the denser plate will be forced under, or subducted beneath, the less dense one.

    • Tectonic Plates Facts For Kids. Earth’s surface is divided into plates. Move a few cm yearly. There are 7 major plates. Cause earthquakes and volcanoes. Plates float on Earth’s mantle.
    • Plate Tectonics. The lithosphere, Earth’s outer layer, is composed of enormous solid rock pieces known as tectonic plates. These plates perpetually move at a snail’s pace, akin to the growth rate of human fingernails, propelled by the heat from the Earth’s core through a process called convection.
    • Earth’s Crust. Tectonic plates, massive segments of the Earth’s crust and the topmost mantle known collectively as the lithosphere are constantly in motion at a pace equivalent to the growth speed of human fingernails.
    • Continental Drift. Tectonic plates, large and irregularly shaped solid rock slabs composed of both continental and oceanic lithosphere, are in perpetual motion, albeit very slowly.
  5. Transform Plate Boundaries are locations where two plates slide past one another. The fracture zone that forms a transform plate boundary is known as a transform fault. Most transform faults are found in the ocean basin and connect offsets in the mid-ocean ridges.

  6. Jan 11, 2021 · Transform Plate Boundaries. Two plates may slide past each other in opposite directions. This is called a transform plate boundary. The plates meet at a transform fault. As you might imagine, plates do not slide past each other easily. These plate boundaries experience massive earthquakes.

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