lecture 2: understanding earth. the science of geology the science of geology geology - the science...
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Lecture 2:Lecture 2:Understanding EarthUnderstanding Earth
The Science of GeologyThe Science of Geology
Geology - the science that pursues an Geology - the science that pursues an understanding of planet Earth understanding of planet Earth
Physical geologyPhysical geology - examines the - examines the materials composing Earth and seeks materials composing Earth and seeks to understand the many processes that to understand the many processes that operate beneath and upon its surface operate beneath and upon its surface
Historical geologyHistorical geology - seeks an - seeks an understanding of the origin of Earth understanding of the origin of Earth and its development through time and its development through time
The Science of GeologyThe Science of Geology
The Nature of Scientific InquiryThe Nature of Scientific Inquiry
How or why things happen is explained How or why things happen is explained using a using a
Hypothesis Hypothesis – a tentative (or untested) – a tentative (or untested) explanation explanation
TheoryTheory – a well-tested and widely – a well-tested and widely accepted view that the scientific accepted view that the scientific community agrees best explains certain community agrees best explains certain observable facts observable facts
Evolution of Solar SystemEvolution of Solar System
Nebular hypothesisNebular hypothesis Rotating cloud called the solar nebulaRotating cloud called the solar nebula Nebula began to contract about 5 billion years agoNebula began to contract about 5 billion years ago 99.9 % of mass is in the Sun (composed mainly of 99.9 % of mass is in the Sun (composed mainly of
hydrogen and helium) hydrogen and helium)
Planets in two groups:Planets in two groups:• Inner planetsInner planets (Mercury, Venus, Earth, Mars) begin to form (Mercury, Venus, Earth, Mars) begin to form
from metallic and rocky substances. They are mostly O, from metallic and rocky substances. They are mostly O, Si, Fe, Mg.Si, Fe, Mg.
• Larger outer planetsLarger outer planets (Jupiter, Saturn, Uranus, Neptune) (Jupiter, Saturn, Uranus, Neptune) began forming from fragments of ices (Hbegan forming from fragments of ices (H22O, COO, CO22,, and and others) and gases.others) and gases.
Evolution of the Solar SystemEvolution of the Solar System
Evolution of the Solar SystemEvolution of the Solar System
Evolution of the Solar SystemEvolution of the Solar System
Evolution of the Solar SystemEvolution of the Solar System
The Solar SystemThe Solar System
A view of EarthA view of Earth
Earth is a planet that is small and self-Earth is a planet that is small and self-containedcontained
Earth’s four spheres Earth’s four spheres HydrosphereHydrosphere AtmosphereAtmosphere BiosphereBiosphere Solid EarthSolid Earth
Earth Internal StructureEarth Internal Structure
Layers defined by composition Layers defined by composition CrustCrust MantleMantle CoreCore
Layers defined by physical propertiesLayers defined by physical properties LithosphereLithosphere AsthenosphereAsthenosphere MesosphereMesosphere Inner and Outer CoreInner and Outer Core
Earth’slayeredstructure
The face of EarthThe face of Earth
Earth’s surface Earth’s surface ContinentsContinents OceansOceans
ContinentsContinents Mountain beltsMountain belts• Most prominent feature of continentsMost prominent feature of continents
The stable interiorThe stable interior• Composed of Composed of shieldsshields and stable and stable platformsplatforms
The ContinentsThe Continents
The face of EarthThe face of Earth
Ocean basinsOcean basins Oceanic ridge systemOceanic ridge system• Most prominent topographic feature on Most prominent topographic feature on
EarthEarth• Composed of igneous rock that has been Composed of igneous rock that has been
fractured and uplifted fractured and uplifted
Oceanic Ridge SystemOceanic Ridge System
Dynamic EarthDynamic Earth
The theory of The theory of plate tectonicsplate tectonics Involves understanding the workings of Involves understanding the workings of
our dynamic planet our dynamic planet Began in the early part of the twentieth Began in the early part of the twentieth
century with a proposal called century with a proposal called continental drift – the idea that continental drift – the idea that continents moved about the face of the continents moved about the face of the planet planet
Dynamic EarthDynamic Earth
The theory of plate tectonicsThe theory of plate tectonics Theory, called Theory, called plate tectonics,plate tectonics, has now has now
emerged that provides geologists with emerged that provides geologists with the first comprehensive model of Earth’s the first comprehensive model of Earth’s internal workings internal workings
Plate boundariesPlate boundaries All major interactions among individual All major interactions among individual
plates occurs along their boundariesplates occurs along their boundaries
Tectonic PlatesTectonic Plates
Dynamic EarthDynamic Earth
Plate boundariesPlate boundaries Divergent boundaryDivergent boundary – two plates – two plates
move apart, resulting in upwelling of move apart, resulting in upwelling of material from the mantle to create material from the mantle to create new seafloor new seafloor
Convergent boundaryConvergent boundary – two plates – two plates move together with subduction of move together with subduction of oceanic plates or collision of two oceanic plates or collision of two continental platescontinental plates
Iceland is being Iceland is being pulled apart as it sits pulled apart as it sits astride the Mid-astride the Mid-Atlantic RidgeAtlantic Ridge..
San San Andreas Andreas
FaultFault
Dynamic EarthDynamic Earth
Plate boundariesPlate boundaries Transform boundaries -Transform boundaries - located where located where
plates grind past each other without plates grind past each other without either generating new lithosphere or either generating new lithosphere or consuming old lithosphere consuming old lithosphere
Changing boundariesChanging boundaries - new plate - new plate boundaries are created in response to boundaries are created in response to changes in the forces acting on the changes in the forces acting on the lithosphere lithosphere
Geologic timeGeologic time
The magnitude of geologic time Involves vast The magnitude of geologic time Involves vast times – millions or billions of yearstimes – millions or billions of years
An appreciation for the magnitude of An appreciation for the magnitude of geologic time is important because many geologic time is important because many processes are very gradualprocesses are very gradual
The big difference between geology and The big difference between geology and other sciences: TIME (Geologically speaking, other sciences: TIME (Geologically speaking, not much happens in a human lifetime!)not much happens in a human lifetime!)
Therefore, geologists use millions of years Therefore, geologists use millions of years as the standard unit of timeas the standard unit of time
Age of EarthAge of Earth
~ 4,600 million years~ 4,600 million years Radioactive mineralsRadioactive minerals• Radium, uranium, lead Radium, uranium, lead
Salts in the oceans and its Salts in the oceans and its accumulation (not accurate)accumulation (not accurate)
Fro younger ages, deposits and CFro younger ages, deposits and C1414
Thegeologic
timescale