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EAS 210: Chapter 1
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20 Terms
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1
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Define Geology
Study of the earth
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Define Physical Geology
Study of the earth's materials and properties
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Geological Time: Absolute Dating
- How we measure the time of the earth
-Radioactivity can allow for the measurement for the age of rocks
- Age of the earth is 4.567 billion years old
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Inner Core
- Innermost part of the Earth
- Contains solid iron
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Outer Core
- A layer formed outside of the inner core.
- Mostly contains liquid iron
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Mantle
- A layer formed between the Earth's Crust and the Outer Core
- Formed by silicate mineral with Fe and Mg
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Crust
- The outermost layer of the Earth
- Formed by silicate minerals with Na, Ca, and Al
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What is the difference between the crust and the mantle
The chemical distinction changes between the layers of the Earth
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What are the two types of crust
The crust is thin beneath the ocean and thick and beneath the continents
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Plate Tectonics
A theory stating that the Earth is comprised plates which shift and move to form our continents
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Lithosphere
-Rigid outer layer of the Earth
-150-250 km thick
-Broken into 16 major tectonic plates
-Important geological processes occur at plate boundaries
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Asthenosphere
- Soft layer below the lithosphere that behaves as a liquid
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Divergent Plate Boundary
-Plates move apart
-Rift valleys and mid-ocean ridges
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Convergent Plate Boundary
-Plates move towards each other
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Oceanic Plate and Continental Plate Convergent Boundary
-Subduction zone
-The dense ocean crust is pushed under the continental crust
-brings water into the mantle and allows for volcanos to form
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Two Continental Plate Convergent Boundary
-Crusts have same density's and create continent-continent collisions
-Crust piles up to form mountains and large plateaus
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Transform Plate Boundary
-Plates move against each other
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Mid-Ocean Ridge
-Linear mountain range on the seafloor
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Subduction Zone
-Contain a line of volcanos
-Offshore is a trench that can be filled with sediment
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Transform Faults
-Offset mid-ocean ridges on the seafloor
-linear feature on continents
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