sphere with a layered structure. Crust - the thinestouterlayer of solid rock, mantle- mostly solid but deep down can flow very slow like liquid. inner and outer core - made of iron and nickel.
earthsstructure2
The earths structure is made up or tectonic plates. Like big rafts that float on the mantle. they move very slowly like a cm a year, sometimes suddenly causing an earthquake, happeneing when tectonicplatesmeet
igneous rocks
formed from magma pushed up to the surface of the crust. They contain various minerals in randomly arranged interlockingcrystals. The size depends on the speed of the cooling. Type types of igneous, extrusive and intrusive. Example- basalt is extrusive and granite is intrusive.
sedimentary rocks
formed from layers of sediment laid down in lakes or seas over millions of years. the layers are cemented together by other minerals. fossils can form in these sediments.
fossil
These are long deadremains of plants and animals
Metamorphic rocks
These are the result of heat and increased pressure acting on existing rocks over long periods or time. They may have really tiny crystals and some layers
weathering
breaking down rocks into smaller bits. there are a few different ways this can happen. chemical, biological and physical weathering
erosion
wearing down rocks
transportation
moving the eroded bits of rock round the world by wind and water
deposition
layingdown of water
cementation
squeezing and compressing the layers , eventually forming into sedimentary rocks
the carbon cycle
photosynthesis removes carbon dioxide from the air. carbon is passed along the food chain when animals feed. respiration and combustion return carbon dioxide to the air.