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Science

AB
mantle thickness29000 km, 16000 mi
core thickness3400 km, 2000 mi
crust thickness5 to 50 km 3-30 mi
outer coreliquid Fe and Ni
inner core solid Fe and Ni, hottest place on Earth (10000-18000 F), the pressure from the heat is so immense that the Fe and Ni cannot move freely
lithospherecomposed of the crust and the upper most part of the mantle, 60 - 100 km thick, cool solid brittle rock
asthenospherein upper part of the mantle, 200 (100 m) km thick, hot semi liquid rock
oceanic crustin ocean, made out of less dense rock, thicker (10-30m)
continental cruston land, less dense rock, is thinner (3-10 mi)
densityhow compact the atoms are (mass per volume)
Alfred Wegenergerman metorologist (weather) who proposed the cdt
1.1 byaRodinia, single cell bacteria and algae
850 myaRodinia into fragments
700 myaGonwanaland and Laurasia
550 myagon. and Laur. moving towards each other
300 myaPangea
200 myaPan. into Gonwanaland and Laurasia, dinosaurs
135 myaGon. into Afica, Australia, South America, Antarctica and India
40 myaLaur. into North America, Europre/Asia and Greenland
35 myaindia into Asia
evidence for cdt (6)looks like continents fit together, glaciers on tropical islands,tropical fossils on Antarctica, similar landscapes on different continents, rocks of the same age and type on continents, same fossils on different continents
2 reasons why sientists did not believe cdtchanged the ideas of the Earth, metorolist proposing a theory in geology
main weakness of cdtdid not explain how con. move
mid ocean ridgea long underwater moutain ridge with a deep valley in between, made by convection cells, new crust is made from magma
theory of PTTthe Earth's litho is divided into plates, plates float on the asten and are constantly movong b/c of convection cells
platebig chunk of litho
2 differences in Ptt and cdtcdt- only land moves, ptt- land and oceanic, cdt- could not explain how continents moved

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