Geological Hazards Notes

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15 Terms

1
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What are the primary chemical components of the Earth's crust?
Oxygen, Silicon, Aluminum, Iron, Calcium, Sodium, Potassium, Magnesium.
2
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What is the density formula for calculating density?
Density (p) = Mass (m) / Volume (V).
3
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What is Earth’s average density based on accepted values for its volume and mass?
5.42 g/cm^3.
4
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What are the two main types of crust on Earth?
Oceanic crust and Continental crust.
5
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What is the dominant rock type found in Earth’s shallow interior?
Peridotite.
6
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What is isostasy in relation to Earth's crust?
Isostasy is the equilibrium between gravity and the buoyancy force, describing how pieces of Earth's crust float on the asthenosphere.
7
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Who is Arthur Holmes and what was his contribution to geochronology?
Arthur Holmes was a British geologist known as the father of modern geochronology who pioneered the use of radiometric dating.
8
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What does the elastic rebound theory describe?
It describes how stress applied to rock results in strain, which builds up until it exceeds static friction, resulting in an earthquake.
9
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What are the characteristics of a normal fault?
In a normal fault, the hanging wall drops down relative to the footwall, associated with extensional stress.
10
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What is a strike-slip fault characterized by?
A strike-slip fault is characterized by side-to-side movement with no fault scarp, footwall, or hanging wall.
11
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What is the relationship between temperature and depth in the Kola Borehole?
At a depth of 12.3 km, temperatures reach up to 180 degrees Celsius.
12
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Why can't scientists directly sample the Earth's interior?
Due to extreme heat and high pressure.
13
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What minerals dominate peridotite?
Olivine and pyroxene.
14
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How do seismic waves contribute to understanding Earth’s interior?
Seismic waves provide information about the physical states and structure of materials within the Earth.
15
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What determines the buoyancy of continental versus oceanic crust?
Continental crust is more buoyant due to its greater thickness and mass/area compared to oceanic crust.