Earths Interior - PowerPoint PPT Presentation

1 / 10
About This Presentation
Title:

Earths Interior

Description:

Oceanic crust beneath the ocean (basalt-dense rock, dark, fine texture) ... the continents (granite-dense rock, light color, larger crystals than basalt) ... – PowerPoint PPT presentation

Number of Views:43
Avg rating:3.0/5.0
Slides: 11
Provided by: janast5
Category:

less

Transcript and Presenter's Notes

Title: Earths Interior


1
Chapter 1-1
  • Earths Interior

2
Geologist
  • Scientists who study the forces that make and
    shape planet Earth.
  • Describe landforms, the features formed in rock
    and soil by water, wind, and waves.
  • Search for clues about Earths history
  • Rock material that forms Earths hard surface

3
Surface Change
  • Constructive forces shape the surface by
    building up mountains and landmasses
  • Destructive forces slowly wear away mountains
    and, eventually, every other feature on the
    surface
  • Continent seven great land masses, surrounded
    by oceans

4
Finding Indirect Evidence
  • Whats inside the Earth?
  • Cant observe this directly
  • Use seismic waves to study interior
  • Seismic waves produced from earthquakes
  • Geologists study how fast they travel through
    Earth and their paths

5
Journey to Center of Earth
  • Temperature surrounding rock is initially cool,
    20 meters down begins getting warmer, for every
    40 meters after that the temperature rises 1
    degreeit gets very hot down there!
  • Pressure The deeper you go, the pressure
    increases (this is the force pushing on a surface
    or area)

6
Three Layers
  • Crust, mantle, coreeach layer has its own
    conditions and materials.

7
Crust
  • Layer of rock that forms Earths outer skin
  • Rocks and mountains, soil and water
  • Thinnest beneath oceans and thickest beneath
    mountains
  • Oceanic crust beneath the ocean (basalt-dense
    rock, dark, fine texture)
  • Continental crust beneath the continents
    (granite-dense rock, light color, larger crystals
    than basalt)

8
Mantle
  • 5-40 kilometers
  • Layer of hot rock
  • Lithosphere upper mantle and crust
  • Asthenophere below lithosphere hotter rock and
    higher pressure (increase with depth)
  • Material is hot, soft, and bendable material
    can flow slowly
  • Lithosphere floats on top of asthenosphere

9
Core
  • Liquid outer core, solid inner core
  • Outer core molten metal that surrounds inner
    core, enormous pressure, behaves like thick
    liquid
  • Inner core dense ball of solid metal, extreme
    pressure
  • Make up about 1/3 of Earths mass

10
Earths Magnetic Field
  • Currents in the liquid outer core force the solid
    inner core to spin at a slightly faster rate than
    the rest of the planet.
  • Currents create Earths magnetic field
  • How a compass works
Write a Comment
User Comments (0)
About PowerShow.com