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Ice Age: Continental Drift | Ice Age 4: Scrat Continental Crack Up HD | Fox Family Entertainment

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Alfred Wegener, born in 1880, was a meteorologist and explorer. In 1910, he noticed that South America and Africa appeared to fit together like puzzle pieces. He was certainly not the first person to notice this. But he was intrigued by the idea and thought a lot about it. He wondered if the two continents were once joined and then moved apart? He set out to find evidence to support or refute this idea.

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Continental Drift: Alfred Wegener Song by The Amoeba People

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Deeper material is hotter and so it rises. Near the surface, it becomes cooler and denser so it sinks.

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Soon after the Earth formed billions of years ago, the Earth's rocky outer crust solidified. This crust is not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle.

The plates are made of rock and drift all over the globe hence called a continental drift. They move both horizontally and vertically. Over long periods of time, the plates also change in size as their margins are added to, crushed together, or pushed back into the Earth's mantle. It is the heat generated by radioactive decay inside the Earth which drives this process. These plates are from 80 to 400 km (50 to 250 miles) thick.

At some stage in history a process called continental drift began. We do not know when because the rocks have been squashed and changed so much since then, but it is important because it is still happening today. Some people think that it caused the Ice Ages.

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Ｓｅａｆｌｏｏｒ         Ｓｐｒｅａｄｉｎｇ  

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Ｓｅａｆｌｏｏｒ         Ｓｐｒｅａｄｉｎｇ  

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SEAFLOOR SPREADING happens when hot magma rises up into the rift valley at the mid-ocean ridges. The lava cools to form new seafloor. Later more lava erupts at the ridge. The new lava pushes the seafloor horizontally away from the ridge axis.

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The epicenter is the point on the Earth’s surface directly above the focus of the earthquake.

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A plate is a slab of Earth’s lithosphere that can move around on the planet’s surface.

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A seismometer is equipment that measures seismic waves and other ground motions.

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ᑕOᑎᐯEᑕTIOᑎ ᑕEᒪᒪ

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ᑕOᑎᐯEᑕTIOᑎ ᑕEᒪᒪ

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Hot things rise; Cool things sink in circular patterns.

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Ｓｅａｆｌｏｏｒ         Ｓｐｒｅａｄｉｎｇ 

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Ｓｅａｆｌｏｏｒ         Ｓｐｒｅａｄｉｎｇ 

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Seafloor Spreading is a mechanism for moving continents. The formation of new seafloor at spreading ridges pushes lithosphere plates on earths surface

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continental rifting is a divergent plate boundary within a continent. This will create continents.

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𝓓𝓲𝓿𝓮𝓻𝓰𝓪𝓷𝓽 𝓟𝓵𝓪𝓽𝓮 𝓑𝓸𝓾𝓷𝓭𝓪𝓻𝔂

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𝓓𝓲𝓿𝓮𝓻𝓰𝓪𝓷𝓽 𝓟𝓵𝓪𝓽𝓮 𝓑𝓸𝓾𝓷𝓭𝓪𝓻𝔂

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A divergent plate boundary IS A location where 2 lithospheric plates are spreading apart

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Tectonic Plates: The Skin of Our Planet | Down to Earth | Da Vinci