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Introduction to Physical Geology

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Presentation on theme: "Introduction to Physical Geology"— Presentation transcript:

1 Introduction to Physical Geology
Lecture 2 Introduction to Physical Geology

2 Lecture Outline I Geological Paradigms II Origins
Physical Geology Lecture Outline 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 - Lithospheric Plates - Plate Boundaries C) The Rock Cycle IV Planetary Geology V Conclusions

3 Geological 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 ( ) catastrophism James Hutton ( ) uniformitarianism rock cycle Charles Lyell ( ) geologic time Alfred Wegener ( ) continental drift

4 Origin of the Solar System The Nebular Hypothesis
Physical Geology Origin of the Solar System The Nebular Hypothesis Palomar Observatory

5 Origin of the Solar System The Nebular Hypothesis
Physical Geology Origin of the Solar System The Nebular Hypothesis

6 Origin of the Solar System The Nebular Hypothesis
Physical Geology Origin of the Solar System The Nebular Hypothesis physical collision gravity clumps of dust grains (cm) Planetesimals (km) planetesimals ( km) protoplanet ( km)

7 The Solar System What is a Planet?
Physical Geology The Solar System What is a Planet? (1) A “planet”1 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”.

8 Origin of the Earth Geological Differentiation
Physical Geology Origin of the Earth Geological Differentiation 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)

9 Fundamental Concepts Earth's Layers
Physical Geology Fundamental Concepts Earth's Layers 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 Brittle

10 Fundamental Concepts Geologic Time
Physical Geology Fundamental Concepts Geologic Time 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

11 Fundamental Concepts Plate Tectonics - The Evidence
Physical Geology Fundamental Concepts Plate Tectonics - The Evidence

12 Fundamental Concepts Plate Tectonics - The Ocean Floor
Physical Geology Fundamental Concepts Plate Tectonics - The Ocean Floor Mid-Ocean Ridge System

13 Fundamental Concepts Plate Tectonics - The Ocean Floor
Physical Geology Fundamental Concepts Plate Tectonics - The Ocean Floor Mid-Ocean Ridge System underwater mountain range 80,000 km long km wide up to 3000 m above sea floor rift valley, 1-2 km deep, runs along axis 4000 km wide fracture systems

14 Fundamental Concepts Plate Tectonics - The Ocean Floor
Physical Geology Fundamental Concepts Plate Tectonics - The Ocean Floor magnetic striping crustal age

15 Fundamental Concepts Plate Tectonics - The Ocean Floor
Physical Geology Fundamental Concepts Plate Tectonics - The Ocean Floor

16 Fundamental Concepts Plate Tectonics - The Engine
Physical Geology Fundamental Concepts Plate Tectonics - The Engine

17 Fundamental Concepts Plate Tectonics - Lithospheric Plates
Physical Geology Fundamental Concepts Plate Tectonics - Lithospheric Plates

18 Fundamental Concepts Plate Tectonics – Plate Boundaries
Physical Geology Fundamental Concepts Plate Tectonics – Plate Boundaries

19 Fundamental Concepts The Rock Cycle
Physical Geology Fundamental Concepts The Rock Cycle Atmospheric Processes Weathering Physical Weathering Chemical Weathering Biological Weathering Sediment Transport Lithospheric Processes Burial Compaction and Cementation Heat and Pressure Stress Plate Tectonics Exposure

20 Planetary Geology Physical Geology Venus Europa Jupiter Mars Io
Magellan Galileo Mars Io Galileo Viking 1 Voyager 1

21 Planetary Geology Mars
Physical Geology Physical Geology Planetary Geology Mars


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