Title: Section 1: Earth
1Section 1 Earths InteriorWho Studies Earths
Interior?
- Geologists
- Scientists who study the forces that make and
shape planet Earth. - They study the processes that create Earths
features and search for clues about Earths
history.
2What kind of evidence do scientists use to learn
about the interior of the earth?
- Direct vs. Indirect
- Direct evidence from rock samples. Scientists
drill up to 12 km into the earth. Forces blast
rock from as deep as 100 km. - Indirect evidence from seismic waves
3How do scientists study the Earth?
- To reach the Earths core you would have to
travel over 6,000 km (3,728 miles)! - Scientists record Seismic Waves a vibration
that travels through Earth carrying the energy
released during an earthquake - Types of seismic waves
- P waves travel through crust (6km/sec) and
mantle (8km/sec) - S waves will not travel through liquid
- http//aspire.cosmic-ray.org/labs/seismic/seismic.
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4What is the Earths structure?
- The Crust
- The Mantle
- Lithosphere
- Asthenosphere
- The Core
- Outer Core
- Inner Core
5What is the structure of the crust?
- A layer of rock that forms the Earths outer skin
including the rock under the ocean - Two types of crust
- Continental Crust
- Granite less dense crust
- Oceanic Crust
- Basalt more dense rock
6What is the structure of the mantle?
- Two major parts
- Lithosphere upper part of crust and mantle
together floats on top of the asthenosphere - Asthenosphere softer than the mantle due to
increasing temperature and pressure - The mantle is nearly 3,000 kilometers thick!
(1,864 miles)
7What is the structure of the core?
- Two parts
- Outer Core liquid behaves like a thick liquid
forces the solid inner core to spin causing
Earths magnetic field - Inner Core solid extreme pressure squeezes the
atoms of iron and nickel so that they cannot
spread out to become liquid - Inner core and outer core are just slightly
smaller than the moon
8Chemical Layers
Physical Layers
9Section 2 Convection and the Mantle How does
Heat transfer?
- Radiation heat transfer through empty space
ex. sunlight - Conduction heat transfer through direct contact
- Convection- heat transfer by movement of heated
fluids
10How do convection currents affect the Earth?
- Heating and cooling a fluid changes its density
warmer fluids have a lower density and float
colder fluids have a higher density and sink
11Section 3 Drifting ContinentsWere the
continents once together?
- Alfred Wegener hypothesized that all the
continents had moved from a supercontinent known
as Pangaea.
12What is the evidence for Wegeners idea?
- Evidence of Continental Drift
- Landforms similar mountain ranges
- Fossils similar fossils of a fernlike plant
existed on both continents - Climate tropical pl ant fossils found in cold
climates
13Section 4 Sea-Floor SpreadingWhat is happening
in the ocean?
- Using sonar scientists discovered mountains under
the ocean - The longest chain of mountains in the world is
under the ocean and is known as the Mid- Ocean
ridge!
14Side-scan sonar image of the remains of the
submarine USS O-9 (SS-70) off the Isle of Shoals,
New Hampshire in more than 400 feet of
water.Courtesy of NOAA.
Side-scan sonar locates missing planeCourtesy of
NOAA.
15What is sea-floor spreading?
- Harry Hess suggested that at the mid-ocean ridge
molten material rises from the mantle and erupts
pushing older rock to both sides - This process is known as sea-floor spreading!
16What is the evidence for Sea-floor spreading?
- Evidence from Molten Material
- Evidence from Magnetic Strips
- Evidence from Drilling Samples
17How can the ocean floor keep from getting wider
and wider?
- The older ocean floor plunges into deep-ocean
trenches in a process known as subduction - Sea-floor spreading and subduction work together
like a giant conveyer belt!
18Section 5 What is the theory of plate tectonics?
- The Earths lithosphere is cracked into separate
sections known as plates - Geological theory states that these plates are in
constant, slow motion, driven by the convection
currents in the mantle
19How is the theory of plate tectonics different
from continental drift?
- Continental drift is based on the movement of the
continents DUE to plate tectonics - Continents are NOT the same as plates
- Tectonic plates can be made up of both oceanic
crust and continental crust
20What happens where the plates meet?
- Plate Boundaries where the edges of the
lithosphere meet faults form along these
boundaries - Transform
- Divergent
- Convergent
21What are Transform boundaries?
- The place where two plates slip past each other,
moving in opposite directions - Earthquakes occur frequently at these boundaries
22What are Divergent Boundaries?
- The place where two plates move apart, or diverge
and create a rift valley - Most occur at the mid-ocean ridge although some
can occur on land
23What are Convergent boundaries?
- The place where two plates come together, or
converge creating a collision - Subduction occurs at convergent boundaries
- The density of the crust determines which crust
will be on top if both plates are the same
density they form a mountain range