Title: A View of Earth
1A View of Earth
Luc Ikelle 2012
2A View of Earth (Apollo 17)
Dry lands (deserts)
oceans
Wetter climate
Antarctica Glacial ice
Ocean and atmosphere
3Earths spheres (1)
- The most dynamic portion of Earth
- Atmosphere
- Thin gaseous envelope surrounding Earth
- Hydrosphere
- Water dominated by the oceans
- Biosphere
- All living things on the planet
- Lithosphere
- Rocky outer shell
4Earths spheres the atmosphere (2)
- Composition is unique in the solar system
- Provides Air we breathe and protects from the
Suns intense heat. - Thin (90 in 16 km) and tenuous
- 78 nitrogen
- 21 oxygen (not present in early atmosphere)
- Minor amounts of carbon dioxide, argon and water
vapor
5Earths spheres the hydrosphere (3)
(blue planet)
- Total mass of water on or near Earths surface
- Covers 71 of Earths surface
- 98 in oceans
- 2 in glaciers, groundwater, lakes and streams
(fresh water)
6Earths spheres the biosphere (4)
- All life on Earth
- Animals plants on land, in the sea and air
(tree roots, flying insects and birds, ) - There life in ocean floor the pressure
- is extreme and no light penetrate.
- Microorganisms - the most common form of life
- Evolved within narrow zone near the Earths
surface
7A view of Earth
- Earths spheres
- Earths interior description
- Earths interior evidence
- Major features of Earths surface
8Earths internal structure
- Solid Earth has a layered structure
- Layers defined by composition and physical
properties - Compositional layers
- crust - mantle - core
- Physical layers
- lithosphere - asthenosphere - mesosphere - outer
core - inner core
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11Compositional Layers
- Crust
- Outermost compositional layer
- Definite change in composition at the base of the
crust - 2 types
- Continental crust (up 75 km thick in Himalaya),
- Oceanic crust ( 8 km thick)
12Compositional Layers
- Mantle
- Largest layer in the earth
- 2900 km thick
- 82 by volume
- 68 by mass
- Composed of silicate rocks with abundant iron and
magnesium - Density ranges from 3.2 to 5 g/cc
13Compositional Layers
- Core
- Central mass about 7000 km in diameter
- Average density of 10.8 g/cc
- 16 by volume, 32 of mass
- Indirect evidence of composition
- Metallic iron
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15Lithosphere/asthenosphere
Lithosphere crust uppermost part of the
mantle Astenosphere part of the mantle beneath
the lithosphere
Continental crust
Oceanic crust
Lithosphere mantle
Asthenosphere
Lithosphere
The uppermost part of the mantle is strong and
solidly attached to crust).
16Physical layerslithosphere
- Crust upper portion of the mantle
- Solid rigid
- Thickness ranges from 10 km beneath oceans to 300
km in continental areas
17Physical layerscontinental crust
- Thick - up to 75 km
- Lower density - 2.7 g/cm3
- Strongly deformed
- Much older - may be billions of years old
18Physical layersoceanic crust
- Thinner - about 8 km
- More dense - 3.0 g/cm3
- Comparatively undeformed
- Much younger lt 200 million years old
19A view of Earth
- Earths spheres
- Earths interior description
- Earths interior evidence
- Major features of Earths surface
20Waves
- Elastic waves are generated whenever there is
- a sudden deformation
- a sudden movement of a portion of the medium
21Waves
- Examples of man-made seismic sources
- Explosion
- Weight drop
- Drilling
- Vibroseis (tractions), ...
22Two types of deformations
- Volumetric change
- (P-waves, compressional waves)
- Change of shape
- (S-wave, shear waves)
Source Duan (2010)
23P-waves (compressional waves)
- P-waves (i) similar to sound waves, (ii) series
of contractions and relaxations, (iii) fastest,
5 km/sec (depends on rock type), (iv) travel
through solid, liquid and gas
24S-waves (shear waves)
- S-waves motion is (i) right angles to direction
of wave, (ii) about half the speed of P waves,
and (iii) travel only through solids
25P-wave
S-wave
Source Duan (2010)
26Horizontal source
Source petroleum-seismology.com
27Sea surface (marine/offshore)(Air/water/solid)
Source petroleum-seismology.com
28Free surface (land/onshore)(Air/solid/solid)
Source petroleum-seismology.com
29Exploring Earths interior with seismic waves
- Seismic waves travel at different speeds in
different rocks
30Seismic waves ground shaking
- Surface waves propagate near the Earth surface,
slower than body waves - L-waves Love, move back/forth (snake)
- R-waves Rayleigh, move like ripples on a pond
Source Duan (2010)
31Source Duan (2010)
32Recording seismic waves seismograms
- Seismograms records of ground shaking
- Waves arrive in sequence.
- P waves first
- S waves second
- Surface waves last (cause most of the property
damage in an earthquake).
Source Duan (2010)
33Interior with seismic waves
- Discovery of Core-Mantle boundary P-waves do not
arrive in the P-wave shadow zone (103 143)
Source Duan (2010)
34Interior with Seismic Waves (cont.)
- Discovering two parts of the core liquid outer
core solid inner core - S-waves do not arrive in the S-wave shadow zone
- P-wave reflection within the core
Source Duan (2010)
35Source Duan (2010)
36refraction
Source Duan (2010)
37A View of Earth
- Earths spheres
- Earths interior description
- Earths interior evidence
- Major features of Earths surface
38World map
39World map
40World map
41North and Central Americas
42Central America
Caribbean sea
43South America
44Europe
45Africa
46Asia
47Oceania
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50Some Additional Statistics
Average land elevation 840 m Average ocean
depth 3,800 m
Average ocean temperature 3.9oC
About 50 of Earths population lives lt240 km
from the ocean
- In Japan, 96 of the population lives lt100 km
from the ocean
51- Kola Superdeep Borehole (KSDB)
- A scientific drilling project in the USSR to
drill into the Earth's crust - goal 15 km
- began digging in 1970
- in 1992, reached a final depth of 12 km
lt1/500 of Earths radius
52Problems
- How do we know that the outer core is liquid?
- Is the core a constituent of the asthenosphere?
- List and briefly describe the four spheres that
constitute our environment. - Can P-wave velocity be greater than S-wave
velocity? - Can S-wave propagate in the sea water?
- Is Guatemala in North, Central, or South America?
- Where is the Gulf of Aden?
- Which one of these components (crust, mantle,
core) of Earth is the heaviest? - Which one of these components (crust, mantle,
core) occupies the largest volume of Earth. - Which one of these components (oceans and
continents) occupies the largest portion of the
surface Earth.