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Earths History

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Sun is probably a third generation star. Probably takes 10-100 ... 'Life is what dies when you stomp on it'--Dave Barry. A self-replicating chemical system ... – PowerPoint PPT presentation

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Title: Earths History


1
Earths History
2
Formation of Sun
  • Formation of Universe 13 billion years
  • Formation of Galaxy 11 billion Years
  • Formation of Solar System 4.6 billion years
  • Sun is probably a third generation star
  • Probably takes 10-100 million years for planets
    to form

3
Formation of Planets
  • Planets made of same material as Sun, minus
    elements that remain mostly in gases
  • Inner Rocky Planets iron and magnesium silicates
  • Outer gas giants and moons water ice
  • Very far from sun methane, ammonia, nitrogen ice

4
Formation of Earth
  • Planets formed by accretion of smaller objects
    impact
  • Very tiny objects hold together by atomic forces
  • Objects kilometers across hold together by
    gravity
  • How do objects the size of a refrigerator hold
    together?
  • As planets get bigger, gravity gets stronger,
    impacts get more violent
  • Big impacts throw out ejecta, trap heat
  • Magma ocean
  • Formation of core early in earth history as iron
    sinks

5
Formation of Moon
  • It's very hard to account for the Moon
  • Very big compared to its parent planet
  • Orbits nearly in plane of earth's orbit, not over
    equator.
  • Co-creation with Earth?

6
Unstable Early Earth
  • May have been several moon-forming events
  • 1000-km impactors can melt crust
  • 100-km impactors create temporary atmosphere of
    vaporized rock, vaporize oceans
  • Life not possible until large impacts cease
  • To have life on Earth, we need Jupiter?
  • Sweeps up debris and reduces impacts
  • Stabilizes orbits of other planets
  • To have life on Earth, we need Moon?
  • Stabilizes changes in earth's axis tilt

7
Conditions on Early Earth
  • Oldest existing earth materials 4.1 billion
    years old
  • Oldest rocks 3.9 billion years old
  • Oxygen-poor atmosphere (present oxygen is created
    by life)
  • Faint Early Sun perhaps 30 per cent less bright
  • Evidence for liquid water from very early on
  • Atmosphere and sun must have evolved in tandem

8
How The Earth Works
9
Earth Systems
  • Geosphere
  • Rock Cycle
  • Plate Tectonics
  • Biosphere
  • Atmosphere
  • Cryosphere
  • Hydrosphere

10
GEOSPHERE
The geosphere is the solid Earth that includes
continental and oceanic crust as well as the
various layers of the Earth's interior. Ninety-fou
r percent of the earth is composed of the
elements oxygen, iron, silica, and magnesium.
11
The Solid Earth
  • Core-solid in the center, molten outside layer,
    mostly Fe with a little nickel
  • Mantle-thick, solid
  • Athenosphere-inner zone partially molten
  • Crusts-outer most, thin layer
  • 8 elements-98.5
  • fossil fuels minerals

12
The Rock Cycle
  • New Rocks Exposed by Erosion
  • Rocks Broken Down Mechanically and Chemically
    (Weathering)
  • Components Transported by Erosion
  • Components Cemented into Sedimentary Rocks
  • Burial and Heating creates Metamorphic Rocks
  • Melting Creates Igneous Rocks

13
The Rock Cycle
14
Plate Tectonics
  • The geospheres surface (crust) is in a constant
    state of motion that gives rise to movement of
    the continents.
  • The unifying theory that explains how continental
    drift is possible is called plate tectonics,
    which was developed by geologists in the 1960s.
  • Supercontinents
  • Rodinia 800 million years
  • Gondwana
  • Laurasia
  • Pangaea 250 million years, only lasted 70 million
    years

15
Biosphere
  • The biosphere is the
  • life zone of the Earth
  • and includes all living
  • organisms, including
  • man, and all organic matter that has not yet
  • decomposed. Life evolved on earth during its
    early
  • history between 4.5 and 3.8 billion years go and
    the
  • biosphere readily distinguishes our planet from
    all others in the solar system

16
Life
  • What Is It?
  • "Life is what dies when you stomp on it"--Dave
    Barry
  • A self-replicating chemical system

17
How Did Life Originate?
  • Certainly not as complex as anything now alive
  • Lots of candidates for first self-replicators
  • Role of minerals as catalysts and templates?
  • Simplest organisms are extremophiles
  • At least since 3 billion years, probably much
    earlier

18
Major Events in the History of Life
  • Oxygen levels in atmosphere
  • Plants release waste oxygen
  • Eventually organisms developed a way to utilize
    oxygen
  • Sex Who Needs It?
  • We are a team Mitochondria
  • Snowball Earth what survived and how?
  • Cambrian "Explosion"

19
Mass Extinctions
Causes ?
  • Climate Change
  • Disease
  • Mountain-building
  • Sea Level Change
  • Competing Organisms
  • Over-specialization
  • Volcanism
  • Meteor Impact

20
Atmosphere
  • Gasesous envelope that
  • surrounds the Earth and
  • constitutes the transition
  • between its surface and
  • the vacuum of space.
  • The atmosphere consists of
  • a mixture of gases composed primarily of
    nitrogen,
  • oxygen, carbon dioxide, and water vapor.

21
Atmosphere
  • Troposphere - weather occurs
  • Stratosphere - where the ozone layer is
    located

22
Cryosphere
  • The word "cryosphere
  • originates from the greek word
  • kryos, meaning frost or icy cold.
  • The cryosphere is the portion of
  • the Earth's surface where water
  • is in a solid form, usually snow
  • or ice. This includes sea ice,
  • freshwater ice, snow, glaciers,
  • and frozen ground (or permafrost).

23
Hydrosphere
  • The hydrosphere includes
  • all water on Earth.
  • Not a drop of liquid water
  • can be found anywhere
  • else in the solar system.
  • Hydrologic Cycle

24
Water
  • Principal Agent in Modifying Earths Surface
  • Medium for Storing and Distributing Global Heat
  • The Universal Solvent
  • Essential for Life
  • Destructive to Rocks
  • Lowers Melting Point of Rocks
  • Reduces Strength of Rocks Under Pressure

25
FRAMEWORK FOR EARTH SYSTEMS EDUCATION
26
Understanding 1
  • Earth is unique, a planet of rare beauty and
    great value.

27
Understanding 2
  • Human activities, collective and individual,
    conscious and inadvertent, affect planet Earth.

28
Understanding 3
  • The development of scientific thinking and
    technology increases our ability to understand
    and utilize Earth and space.

29
Understanding 4
  • The Earth system is composed of interacting
    subsystems of water, rock, ice, air, and life.

30
Understanding 5
  • Planet Earth is more than 4 billion years old and
    its subsystems are continually evolving.

31
Understanding 6
  • Earth is a small subsystem of a solar system
    within the vast and ancient universe.

32
Understanding 7
  • There are many people with careers that involve
    study of Earth's origin, processes, and
    evolution.
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