Lecture 11_First billion years

Page 1: Introduction to Early History of Earth

  • Topic: Evolution of Earth and Life

  • Course: ECS 1213 Lecture – 11

  • Focus: Understanding what we know about the early history of planets

Page 2: Challenges in Reconstruction

  • Early events leave no physical records due to plate tectonics which destroy geological records.

  • Importance of studying events through indirect evidence.

  • The Moon as a significant source of information about Earth's history.

Page 3: Theoretical Understanding of Planet Formation

  • Solar System Dynamics:

    • All planets rotate around the sun in the same direction and plane.

    • Formed simultaneously from a singular rotating disk of material.

  • Sun's Nature:

    • A star, part of the galaxy, formed similarly to other stars.

  • Stellar Measurements:

    • Stars' distance can be calculated by measuring their angle relative to Earth at different times of the year using triangulation.

    • Speed of light is approximately 186,000 miles/second.

    • Events in the universe are recorded; e.g., a dying star's light reflects its past state.

Page 4: Observational Evidence of the Universe's Origin

  • Doppler Shift:

    • Indicates movement through changes in wavelength based on the object's velocity relative to the observer.

    • Red Shift:

      • An increase in wavelength signifies a distant galaxy's movement away from Earth.

      • Astronomers measure the red shift by comparing spectral lines against a reference.

Page 5: The Big Bang Theory

  • The universe is expanding, with galaxies moving apart.

  • Initially concentrated at a singular point (the Big Bang).

  • Estimated age of the universe: Approximately 15 billion years.

Page 6: Formation of the Solar System

  • Initial state:

    • A diffuse and roughly spherical nebula that slowly rotates.

    • Gravity causes the nebula to contract, forming a flat, rapidly rotating disk.

    • Proto-Sun forms in the center while gas and dust form planetesimals.

  • Planetary Formation:

    • Terrestrial planets form from collisions of planetesimals.

    • Giant outer planets primarily grow by accumulating gases.

Page 7: Formation of the Sun and Elements

  • Hydrogen cloud collapses under gravity, generating immense heat (millions of degrees).

  • Nuclear Fusion:

    • Occurs under extreme conditions; hydrogen nuclei collide to form heavier isotopes.

Page 8: Element Formation in Stars

  • Formation of helium from hydrogen results in loss of mass, converting to heat energy.

  • Increasing temperatures facilitate the formation of other elements on the periodic table.

Page 9: Formation of Elements Beyond Iron

  • Fusion up to iron releases energy; beyond iron, energy is consumed.

  • Neutron Capture:

    • Absorption of neutrons forms heavier elements, typically occurring in supernova explosions due to high energy conditions.

Page 10: Supernova Dynamics

  • Balance of Forces:

    • Gravity and nuclear reaction forces compete within a star.

    • When fusion ceases, gravity dominates, causing a collapse leading to a supernova.

  • Heavy elements are formed during this explosive process.

Page 11: Meteorites: Clues to Earth's Early History

  • Types of Meteorites:

    • Stony meteorites (rocky composition).

    • Iron meteorites (metallic composition).

    • Stony-iron meteorites blend rocky and metallic and serve as proxies for Earth's core.

  • Most meteorites date around 4.6 billion years, offering insights into primordial materials unaffected by Earth's erosion and tectonics.

  • Entry of meteoroids into the atmosphere creates identifiable streaks of light, representing ancient solar system materials.

Page 12: Lunar Rocks as Historical Clues

  • Missions (1969-1972): Six lunar landings conducted by astronauts who collected samples and mapped the moon's surface.

  • The moon's surface is characterized by numerous craters of varying sizes.

  • Craters and Age:

    • Crater counting reveals older surfaces have more craters, indicating significant impact history.

    • Larger craters suggest a longer existence while overlapping craters indicate more recent impacts.

  • This evidence leads to the inference of a "Heavy Bombardment" period.