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  1. The convection currents in the asthenosphere drive the process of plate tectonics. Below the mantle is Earth’s core, consisting predominantly of iron and nickel: a solid inner core surrounded by a liquid outer core. It is believed that the convection of the liquid metal outer core induces the earth’s magnetic field. Figure 3.2.

  2. The ages measured for Earth’s oldest rocks and oldest crystals show that the Earth is at least 4.3 billion years in age but do not reveal the exact age of Earth’s formation. The best age for the Earth (4.54 Ga) is based on old, presumed single-stage leads coupled with the Pb ratios in troilite from iron meteorites, specifically the Canyon ...

  3. 28 gru 2023 · Explain how oceanic hotspots create chains of volcanic islands. Compare hotspots to plate tectonic boundary types. Identify geographic examples of different plate tectonic boundaries and hotspots. Explain why plate tectonics theory is the unifying theory of geology.

  4. The geologic time scale organizes the Earth's history into a series of chronologic subdivisions that are defined by important geologic events in the Earths history (Figure 7-1). The largest of these time subdivision are eons, which define major developments in the Earth's evolutionary history (i.e., formation of the Earth, beginning of life).

  5. During this lesson students observe convection currents by performing a lab experiment. As a result of this activity, students develop an understanding of the process of convection as it relates to the movement of molten rock in Earth.

  6. To investigate the viscosity of a fluid and illustrate that the Earth's mantle can be thought of as a solid for short duration processes (such as the propagation of seismic waves), and as a very viscous fluid for long duration processes (such as mantle convection and plate tectonic movements). Materials: Part A: Thermal Convection Experiments.

  7. Throughout this lab manual, you will mainly see us referencing periods of geologic time. Figure 3.1 – The geologic time scale subdivided by eon, era, system, series, epoch, and stage. What do you observe about each period of time?