Earth Science Fundamentals: Crust, Plates, and Geologic Time

Earth’s Composition and Processes

Chapter 1 & 2: Earth’s Structure and Time

  1. Continental vs. Oceanic Crust

    How does continental crust differ from oceanic crust? All of the above (thicker, light color, less dense).

  2. The Lithosphere

    The rigid, brittle layer of the Earth that is broken into drifting plates is the: Lithosphere.

  3. Uniformitarianism

    That geologic processes have been consistent over time (“the present is the key to the past”) is the basis for the theory of: Uniformitarianism.

  4. Geologic Eras

    The four major eras of geologic time, from oldest to most recent, are: Precambrian, Paleozoic, Mesozoic, Cenozoic.

  5. North Carolina Earthquake

    Which of the following was NOT a result of the recent magnitude 5.1 earthquake in North Carolina? A tsunami or tidal wave.

  6. Crustal Elements

    Which of the following is among the most common crustal elements but not among the most common elements on a whole-Earth basis? Sodium (Na).

  7. Dinosaur Evidence

    Which of these is the overwhelming evidence that dinosaurs once roamed the Earth? Fossils of them, as found buried in sediment.

  8. Earth Profile

    A vertical slice or side view of a portion of the Earth is called a: Profile.

  9. Theory vs. Hypothesis

    What is the critical difference between a theory and a hypothesis? A theory is a hypothesis that has withstood time and the scrutiny of the scientific community.

  10. Topographic Maps

    A map that uses varying degrees of dark shading to convey the nature of the Earth’s surface is a: Topographic map.

  11. Quantitative Data

    Detailed field and laboratory information, with units of measurements, constitute: Quantitative data.

  12. Numerical Age

    The age of a rock, expressed in units of time, is its: Numerical age.

  13. Meteorite Insights

    Which of the following characteristics do meteorites suggest about the Earth’s interior? Composition and density.

  14. Deposition

    The dumping/dropping of eroded earth material from water, wind, glaciers and waves is known as: Deposition.

  15. Metamorphism

    Rocks undergo metamorphism because of: Exposure to heat and pressure deep in the crust.

  16. Sedimentary Rocks

    Earth materials such as mud, silt, sand and gravel form: Sedimentary rocks.

  17. Igneous Rocks

    Those rocks that form from crystallization of molten magma are: Igneous rocks.

  18. Rock Composition

    Which of the following is the correct relationship? Rocks are made of minerals that are made of elements.

  19. Earth’s Interior Information

    Which of these is NOT a source of information about the likely characteristics of the Earth’s interior layers? Deep drilling.

  20. Human Era

    Which geologic era is the one in which humankind has lived? Cenozoic.

Chapter 3 & 4: Plate Tectonics

  1. Diverging Plate Boundaries

    What is the relative motion of the two plates either side of a diverging plate boundary? Pulling apart from one another.

  2. Continental vs. Oceanic Lithosphere

    How does “continental” lithosphere differ from “oceanic” lithosphere? All of the above (continental is thicker, low density, and light color).

  3. The Asthenosphere

    Which of the following is true about the Earth’s “asthenosphere?” It’s a plastic layer than can bend and flow.

  4. Pangaea

    The name coined by Alfred Wegener for the original supercontinent was: Pangaea.

  5. Wegener’s Evidence

    Which of these was Wegener not able to use to support his theory of continental drift? The magnetic characteristic of rocks.

  6. Wegener’s Unanswered Question

    What was the one big question Wegener could not answer? What actually caused the continent to drift?.

  7. Magnetic Declination

    The difference in the location of the Earth’s geographic and magnetic poles (axes) is called: Declination.

  8. Magnetic Inclination

    The tendency for a compass needle to tilt downward in parallel to the lines of force of the Earth’s magnetic field is called: Inclination.

  9. Paleomagnetism

    Magnetic characteristics of the past, captured in iron-rich rocks, is called: Paleomagnetism.