If you were lost, how could a dog help? - PowerPoint PPT Presentation

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If you were lost, how could a dog help?

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Title: Inside the Earth Author: Jenny Grabow Last modified by: Any User Created Date: 9/7/2006 2:42:51 AM Document presentation format: On-screen Show (4:3) – PowerPoint PPT presentation

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Title: If you were lost, how could a dog help?


1
If you were lost, how could a dog help?
A new study says that dogs choose the direction
they relieve themselves based on our planet's
magnetic field.
2
Inside the EarthHow do scientists know?
3
Earth in General
  • 3 Layers
  • Crust
  • Mantle
  • Core
  • Diameter
  • 12,750 km

4
Cross Section Diagram
5
Overview of the Crust
  • Solid Basalt and Granite
  • 5-100 km thick
  • Coolest in temperature
  • Least dense
  • 2.2-2.9 g/cm3
  • Like the shell of egg, is brittle and can break
  • Layer we live on

6
What is the difference between sediment and
bedrock?
Sediment is Smaller pieces of broken rock mixed
with organic material and remains
Bedrock is rock underneath the accumulated
sediment
7
Overview of Crust (continued)
  • Major changes
  • Plate Tectonics
  • Minor changes
  • Weathering erosion
  • Deposition of sediments
  • Two types of Crust
  • Oceanic (very dense, made of basalt)
  • Continental (less dense, made of granite)

8
Example of minor change a bit of New Hampshire
folklore
For A. Cleary
9
Oceanic and Continental Crust
  • Oceanic Crust
  • Mainly Basalt
  • Thinnest part of crust 5 km thick
  • Density 3.0 g/cm3
  • Ocean puddles on top
  • Youngest part of crust, new crust is made here
  • Continental Crust
  • Mainly Granite
  • Thickness varies but 30 km thick
  • 100 km thick under Himalayans Mts.
  • Density 2.7 g/cm3
  • Oldest part of crust

10
Overview of the Mantle
  • Like white of egg
  • Hot layer of semi solid rock
  • Contains more iron, magnesium and calcium than
    crust
  • Hotter denser temp and pressure increase
    w/depth
  • 2900 km thick
  • Density 3.4 5.6 g/cm3
  • Multiple layers which have
  • different densities

11
Upper Mantle and Lower Mantle
  • Upper Mantle
  • 720 km thick
  • Density 3.4 4.4 g/cm3
  • 1480 C, rock is near melting
  • Magma from some volcanoes can originate here
  • Lower Mantle
  • 2170 km thick
  • Density 4.4 5.6 g/cm3
  • 2600 C
  • Higher level of magnesium silicon oxides

12
Overview of the Core
  • Mostly iron nickel, metal
  • Core is not rock or fire
  • 3300 km thick
  • Twice as dense as mantle

13
Outer Core
  • Liquid nickel and iron
  • 2200 km thick
  • Density 9.9 12.2 g/cm3
  • 3800 C

14
Inner Core
  • Solid nickel and iron
  • 1250 km thick
  • Density 12.2 13.1 g/cm3
  • 4300 C

The inner core is solid but hotter than the
outer core why?
15
Where does the core get its heat?
  • Chunks of material collided and stayed together,
    (Heat from these collisions can be on the order
    of 10,000 kelvins about 18,000 degrees
    Fahrenheit).
  • Friction, when denser core material sinks
  • Decay of radioactive elements, mostly uranium and
    thorium according to physicists.

16
Earths Layers
  • How are the earths layers similar to an egg?
  • Shellcrust
  • Egg whitemantle
  • Yolkcore

17
Interactions between Layers
  • Lithosphere
  • Includes crust and solid, uppermost part of the
    mantle
  • Broken into about 19 pieces, these pieces are
    called PLATES
  • The plates move on top of the Asthenosphere
    (which is a thin layer of the upper mantle)

18
Interactions between Layers
Asthenosphere
  • Beneath the lithosphere, in the mantle, lies a
    soft, relatively weak region of rock that flows
    slowly (like soft plastic or hot asphalt)
  • Convection Currents that drive the movement of
    plates happen in the Asthenosphere

19
Vocabulary expected to know
  • Sphere shaped like a ball
  • Hemisphere half of a sphere
  • Interior inside
  • Exterior outside
  • Cross Section diagram that shows a piece cut
    out, so you can see the inside
  • Molten melted, usually referring to material
    that melts at very HIGH temperature

20
Vocabulary expected to know
  • Lava melted rock touching atmosphere
  • Magma melted rock below the crust
  • Tectonic Plates broken pieces of the lithosphere

21
Tectonic Plates
  • Earths crust is broken into about 19 pieces
  • These plates move on top of the asthenosphere
    (thin layer of the upper mantle)
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