Comprehensive 8th Grade Earth Science and Seismology Study Notes

Fundamentals of Geology and Earth Structure

  • Geology: The scientific study of the earth.
  • Crust: The earth's outer layer of solid rock.
    • Oxygen: The most abundant element in the earth's crust.
    • Moho (Mohorovičić Discontinuity): The lower boundary of the earth's crust.
  • Sediments: Deposits of sand, mineral fragments, or organic materials usually left by wind or water.
  • Mantle: The middle layer of the earth.
    • Asthenosphere: Plastic rock located in the lower portion of the upper mantle.
    • Transition Zone: The portion of the mantle located between 400km400\,\text{km} and 1050km1050\,\text{km} beneath the surface.
    • Core-Mantle Boundary: The portion of the earth that makes up the bottom of the mantle.
  • Core: The central part of a planet.
    • Inner Core: The innermost part of the earth, said to be solid iron or nickel.

Mountain Formation and Structural Geology

  • Volcanic Mountain: A mountain that formed when molten rock erupts from a hole in the earth's crust.
  • Folded Mountain: A mountain believed to have formed when the edges of two tectonic plates were pushed together.
  • Domed Mountain: Formed when molten rock is forced beneath an overlaying rock layer.
  • Anticline: An arch-like structure formed when rocks buckle upward during folding.

Tectonic Features and Fault Dynamics

  • Fault: A fracture zone formed when a layer of rocks breaks and moves due to the strain of forces upon it.
  • Thrust Fault: A fault that results when rocks on one side of the fault are shoved on top of the rocks on the other side.
  • Tectonic Earthquake: A sudden movement of rock beneath the earth's surface.
  • Catastrophic Plate Tectonics: A Creationist model in which the earth's crust broke into tectonic plates at the beginning of the flood.
  • Elastic Rebound Theory (Elastic Rebound): A theory stating that rocks on either side of a fault spring back to a position of little or no strain at the moment of an earthquake.

Seismology and Earthquake Characteristics

  • Seismology: The scientific study of earthquakes.
  • Hypocenter: The underground point at which an earthquake begins.
  • Epicenter: The point on the earth's surface directly above an earthquake's hypocenter.
  • Shallow-Focus Earthquakes: Account for about 85%85\% of all earthquakes and originate at depths of less than 20km20\,\text{km}.
  • Primary (P) Waves: A type of earthquake wave that consists of a rhythmic push-pull motion in the direction of wave travel.
  • Aftershock: Any of the smaller earthquakes or tremors that often follow an earthquake.
  • Global Earthquake Belts:
    • Circum-Pacific Belt: The most active earthquake zone, which borders the Pacific Ocean.
    • Alpide Belt: An earthquake zone that stretches from the mountains of northern Africa through parts of Europe.

Measurement, Equipment, and Data Systems

  • Seismometer: A device that detects the earth's movements.
  • Seismograph: An instrument used to record and study earthquake waves. Scientists use a seismograph to determine the exact point where an earthquake begins.
  • Moment Magnitude Scale: An earthquake magnitude scale based on measuring the size of the earthquake's source.
  • Modified Mercalli Scale: A scale used to describe and evaluate the effects of an earthquake on man.
  • Geographic Information System (GIS): A computer system that stores and processes geographic data.
  • Topographic Map Review: Includes map examples located on pages 3636 and 3737 for test review.

Volcanology Concepts

  • Ring of Fire: A narrow zone of active volcanoes that parallels the Circum-Pacific earthquake belt.
  • Pyroclast: A particle or block of solid volcanic ejecta.
  • Volcanic Explosivity Index (VEI): A scale used to measure the explosiveness of a volcano's eruption (covered across pages 5151 through 6565).