Title: If you were lost, how could a dog help?
1If 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.
2Inside the EarthHow do scientists know?
3Earth in General
- 3 Layers
- Crust
- Mantle
- Core
- Diameter
- 12,750 km
4Cross Section Diagram
5Overview 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
6What 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
7Overview 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)
8Example of minor change a bit of New Hampshire
folklore
For A. Cleary
9Oceanic 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
10Overview 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
11Upper 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
12Overview of the Core
- Mostly iron nickel, metal
- Core is not rock or fire
- 3300 km thick
- Twice as dense as mantle
13Outer Core
- Liquid nickel and iron
- 2200 km thick
- Density 9.9 12.2 g/cm3
- 3800 C
14Inner 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?
15Where 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.
16Earths Layers
- How are the earths layers similar to an egg?
- Shellcrust
- Egg whitemantle
- Yolkcore
17Interactions between Layers
- 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)
18Interactions 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
19Vocabulary 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
20Vocabulary expected to know
- Lava melted rock touching atmosphere
- Magma melted rock below the crust
- Tectonic Plates broken pieces of the lithosphere
21Tectonic Plates
- Earths crust is broken into about 19 pieces
- These plates move on top of the asthenosphere
(thin layer of the upper mantle)