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Earth Structure
Four Main Layers Inner core Outer core Mantle Crust
Crust Thinnest Layer Two types of crust : Oceanic: made mostly igneous rock and Basalt. Found under ocean, thin Continental: made mostly of granite. Found under continents, thick
Mantle Located abovethe outer core  Below the crust is where the mantle starts Largest Layer 80% of Earth’s volume & 68% of Earth’s mass Composed of iron Density, Temperature, And pressure increases the deeper you go into the mantle Lithosphere :upper, solid part of mantle Asthenosphere: under lithosphere, solid rock flows very slowly
Outer Core Surrounds inner  core Temp. : 2200c-5000c Iron and Nickel, Liquid
Inner Core Solid, iron and nickel Temp. can reach to 5000c Solid, because of the pressure put on the core Solid core is the source of Earth’s magnetic field
Continental Drift
Alfred Wegener First proposed the theory of continental Drift Continental Drift was his theory that continents were joined together then drifted apart Named Pangaea a supercontinent Theory was rejected because he couldn’t explain which force pushes or pull continents Found pieces of evidence:       Geologic       Climate        Fossil 1940s: Technology was developed
Climate evidence in the changing climates during the past.
 Geologic  evidence in layers of rocks across continents.
Fossil Evidence of fossils are found in certain places
Fossil
Fossil Remains or physical evidence of an organism preserved by geological processes Preserved in sedimentary rock Sediment slows down decay Bones and shells are resistant to decay, more commonly preserved tissue
Examples Fossils in rock Fossils in Amber Petrification Fossils in asphalt Frozen fossil Trace Fossil Mold Cast Index Fossil
Amber Harden tree sap    Bugs, lizard, and frogs
Petrified Fossil A process in which minerals replace organism tissue Types: Space in bone/wood fills up with mineral Organisms are replaced  by minerals
Frozen Cold temperatures slow down decay Many frozen fossil are preserved from last ice age
Fossil in asphalt Wells up in sticky, thick pools Traps  and preserves fossil in asphalt
Trace Fossil Naturally preserved evidence of animal activity Footprints fill with sediment Shows how big their  Footprint was.
Molds And Cast Mold: a cavity in a rock  where a plant and animal was buried. Cast: an object created when sediment fills mold and becomes a rock.
Index Fossil Fossils of organisms that lived during a relatively short, well-defined geologic time span.
Geologic Time
Geologic scale Divisions  Largest division is epoch Second largest division- periods Third largest division- eras
Eras Three eras: Cenozoic: means “New Life” Mesozoic: means “middle animals” Paleozoic: means "ancient life"
Cenozoic
Mesozoic
Paleozoic

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Earth structure 2 m lucente

  • 2. Four Main Layers Inner core Outer core Mantle Crust
  • 3. Crust Thinnest Layer Two types of crust : Oceanic: made mostly igneous rock and Basalt. Found under ocean, thin Continental: made mostly of granite. Found under continents, thick
  • 4. Mantle Located abovethe outer core Below the crust is where the mantle starts Largest Layer 80% of Earth’s volume & 68% of Earth’s mass Composed of iron Density, Temperature, And pressure increases the deeper you go into the mantle Lithosphere :upper, solid part of mantle Asthenosphere: under lithosphere, solid rock flows very slowly
  • 5. Outer Core Surrounds inner core Temp. : 2200c-5000c Iron and Nickel, Liquid
  • 6. Inner Core Solid, iron and nickel Temp. can reach to 5000c Solid, because of the pressure put on the core Solid core is the source of Earth’s magnetic field
  • 8. Alfred Wegener First proposed the theory of continental Drift Continental Drift was his theory that continents were joined together then drifted apart Named Pangaea a supercontinent Theory was rejected because he couldn’t explain which force pushes or pull continents Found pieces of evidence: Geologic Climate Fossil 1940s: Technology was developed
  • 9. Climate evidence in the changing climates during the past.
  • 10. Geologic evidence in layers of rocks across continents.
  • 11. Fossil Evidence of fossils are found in certain places
  • 13. Fossil Remains or physical evidence of an organism preserved by geological processes Preserved in sedimentary rock Sediment slows down decay Bones and shells are resistant to decay, more commonly preserved tissue
  • 14. Examples Fossils in rock Fossils in Amber Petrification Fossils in asphalt Frozen fossil Trace Fossil Mold Cast Index Fossil
  • 15. Amber Harden tree sap Bugs, lizard, and frogs
  • 16. Petrified Fossil A process in which minerals replace organism tissue Types: Space in bone/wood fills up with mineral Organisms are replaced by minerals
  • 17. Frozen Cold temperatures slow down decay Many frozen fossil are preserved from last ice age
  • 18. Fossil in asphalt Wells up in sticky, thick pools Traps and preserves fossil in asphalt
  • 19. Trace Fossil Naturally preserved evidence of animal activity Footprints fill with sediment Shows how big their Footprint was.
  • 20. Molds And Cast Mold: a cavity in a rock where a plant and animal was buried. Cast: an object created when sediment fills mold and becomes a rock.
  • 21. Index Fossil Fossils of organisms that lived during a relatively short, well-defined geologic time span.
  • 23. Geologic scale Divisions Largest division is epoch Second largest division- periods Third largest division- eras
  • 24. Eras Three eras: Cenozoic: means “New Life” Mesozoic: means “middle animals” Paleozoic: means "ancient life"