Title: Introduction to Physical Geology
1Lecture 2 Introduction to Physical Geology
2Lecture Outline
Physical Geology
I Geological Paradigms II Origins A) The Solar
System B) The Earth III Fundamental Concepts of
Physical Geology A) Geologic Time B) The
Earth's Structure i. Earth's
Layers ii. Plate Tectonics - From
Continental Drift to Plate Tectonics - Lithosp
heric Plates - Plate Boundaries C) The Rock
Cycle IV Planetary Geology V Conclusions
3Geological Paradigms
Physical Geology
paradigm, n a collection of beliefs shared by
scientists a set of agreements about how
problems are to be understood
James Ussher (1581-1656) catastrophism
James Hutton (1726-1797) uniformitarianism rock
cycle
Charles Lyell (1797-1875) geologic time
Alfred Wegener (1880-1930) continental drift
4Origin of the Solar SystemThe Nebular Hypothesis
Physical Geology
Palomar Observatory
5Origin of the Solar SystemThe Nebular Hypothesis
Physical Geology
6Origin of the Solar SystemThe Nebular Hypothesis
Physical Geology
gravity
physical collision
clumps of dust grains (cm)
Planetesimals (km)
planetesimals (10-100 km)
protoplanet (100-1000km)
7The Solar SystemWhat is a Planet?
Physical Geology
(1) A planet1 is a celestial body that (a) is
in orbit around the Sun, (b) has sufficient mass
for its self-gravity to overcome rigid body
forces so that it assumes a hydrostatic
equilibrium (nearly round) shape, and (c) has
cleared the neighbourhood around its orbit. (2)
A dwarf planet is a celestial body that (a) is
in orbit around the Sun, (b) has sufficient mass
for its self-gravity to overcome rigid body
forces so that it assumes a hydrostatic
equilibrium (nearly round) shape2 , (c) has not
cleared the neighbourhood around its orbit, and
(d) is not a satellite. (3) All other objects3
except satellites orbiting the Sun shall be
referred to collectively as Small Solar-System
Bodies.
8Origin of the EarthGeological Differentiation
Physical Geology
- Earth melted by
- gravitational energy left from formation of
planet - meteor bombardment
- radioactive decay
- Gravity concentrated denser materials (Ni Fe)
in center - Less dense materials (silicates) forced to outer
layers - Crust became stable after 1 billion years
- Compositional Zones
- Crust
- Continental
- Oceanic
- Mantle
- Core
- Outer (Liquid)
- Inner (Solid)
9Fundamental ConceptsEarth's Layers
Physical Geology
- Compositional Zones
- Core
- Solid inner core
- Liquid outer core
- Radius of 3500 km
- 16.2 of Earth's vol.
- 31.5 of Earth's mass
- Generates Earth's magnetic field
- Mantle
- Thickness 2900 km
- 82.3 of Earth's vol.
- 67.8 of Earth's mass
- Crust
- Oceanic 4-20km thick
- Continental 30-70km thick
- Mechanical Zones
- Core
- Mesosphere
- Lower mantle
- Rigid
- Very Hot
- Capable of gradual flow
- Asthenosphere
- "weak" layer
- Convecting mantle
- Soft and readily flows
- Lithosphere
- Crust and Upper Mantle
- Rigid
- Brittle
10Fundamental ConceptsGeologic Time
Physical Geology
- Phanerozoic Eon -"Eon of Evident Life"
- Paleozoic Era -"Era of Old Life"
- Mesozoic Era -"Era of Middle Life"
- Cenozoic Era -"Era of Modern Life"
Divisions Eon Era Period Epoch Age
11Fundamental ConceptsPlate Tectonics - The
Evidence
Physical Geology
12Fundamental ConceptsPlate Tectonics - The Ocean
Floor
Physical Geology
Mid-Ocean Ridge System
13Fundamental ConceptsPlate Tectonics - The Ocean
Floor
Physical Geology
Mid-Ocean Ridge System
- underwater mountain range
- 80,000 km long
- 1500-2500 km wide
- up to 3000 m above sea floor
- rift valley, 1-2 km deep, runs along axis
- 4000 km wide fracture systems
14Fundamental ConceptsPlate Tectonics - The Ocean
Floor
Physical Geology
magnetic striping
crustal age
15Fundamental ConceptsPlate Tectonics - The Ocean
Floor
Physical Geology
16Fundamental ConceptsPlate Tectonics - The Engine
Physical Geology
17Fundamental ConceptsPlate Tectonics -
Lithospheric Plates
Physical Geology
18Fundamental ConceptsPlate Tectonics Plate
Boundaries
Physical Geology
19Fundamental ConceptsThe Rock Cycle
Physical Geology
- Atmospheric Processes
- Weathering
- Physical Weathering
- Chemical Weathering
- Biological Weathering
- Sediment Transport
- Lithospheric Processes
- Burial
- Compaction and Cementation
- Heat and Pressure
- Stress
- Plate Tectonics
- Exposure
20Planetary Geology
Physical Geology
Venus
Jupiter
Europa
Magellan
Galileo
Io
Mars
Galileo
Viking 1
Voyager 1
21Planetary GeologyMars
Physical Geology
Physical Geology