https://padlet.com/alec_brown2/f0ccmco1j0nd en-us 2019-04-05 17:31:54 UTC 2019-04-08 17:37:00 UTC hello@padlet.com alec_brown2 https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349024843 Description: Transform boundaries slide horizontally. These plates do not move very smoothly. Instead, they slide slowly and build up pressure. Then they move very suddenly to release this energy.]]> 2019-04-05 17:35:59 UTC https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349024843 alec_brown2 https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349025195 Description: Divergent boundaries have plates moving away from each other. The tension occurs as the plates move away from each other, and the lithosphere thins. New lithosphere is created as the magma cools, and old lithosphere is destroyed in subduction zones.]]> 2019-04-05 17:36:44 UTC https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349025195 alec_brown2 https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349025256 Description: The collision of 2 boundaries. 
Continental-Ocean: The ocean plate is denser than the continental plate, so it goes under the continental plate. Example: Nazca Plate and South America Plate. 
Ocean-Ocean: Subduction will occur on the denser plate. Example: Pacific Plate and Antarctic Plate. 
Continental-Continental: Plates push against each other, and buckle. Example: Eurasian Plate and African Plate.  ]]> 2019-04-05 17:36:52 UTC https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349025256 alec_brown2 https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349274253 2019-04-07 17:39:16 UTC https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349274253 alec_brown2 https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349274681 2019-04-07 17:42:23 UTC https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349274681 alec_brown2 https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349274908 2019-04-07 17:44:16 UTC https://padlet.com/alec_brown2/f0ccmco1j0nd/wish/349274908