#3 - Important terms and facts from #1 Flashcards
What are the patterns of propagation for all seismic waves?
Rayleigh - Retrograde-elliptical
P waves - ‘Push-pull’
S waves - Shear; Perpendicular to wave
Love waves - Slithering of a snake, also perpendicular to wave propagation
What is the demographic (population) transition cycle (Ch.1)
Before transition - Birth rates and death rates in equal ratio
During transition - Low death rates and high birth rates causes population to soar
After transition - Low death rates accompanied with low birth rates stabilizes the population
What are the main sources of Earth’s internal heat?
- Impact energy - Motion energy of converted into heat energy
- The radioactive atoms decay produces heat
- Frictional energy from differentiation of layers under gravity
Isostacy
The Earth’s ability to adjust for any mass stress placed upon it. The asthenosphere bends so the lithosphere can take stress without breaking
What is the boundary between low-density
continental rocks and high-density oceanic rocks
1800 m
Uniformitarianism
Natural laws are uniform through time and space, present characteristics were true for the past too.
Strike and Dip
Strike - The compass bearing direction of the horizontal fault line
Dip - Angle of inclination from horizontal line
How much faster do P-waves travel from S-waves and which wave can travel the greatest distance?
1.7 times. Rayleigh waves
How is the epicentre distance determined?
The time difference between the P and S waves recorded from several epistemological centres
Moment magnitude scale (Seismic Moment M0)
Shear strengthRupture areaDisplacement
Mercalli intensity scale
Quantify what people ‘feel’ during an earthquake.
Seismic gap method
A tool for predicting sites for future EQs. Faults fail in segments - If recent EQ - Low future probability. If non-recent EQ/failed segment - High future probability.
What buildings do you build on a hard bedrock vs soft bedrock base?
Hard - Tall and flexible
Soft - Short and sturdy/strong
Pyroclastic Flow
Fast-moving mixtures of hot gases, ash, and volcanic debris that travel downslope. The density and mobility of pyroclastic flows are influenced by factors such as gas content, fragmentation, and the presence of fine ash.
Plutonic vs. Volcanic rock
Plutonic - Magma cools slowly and solidifies beneath the surface
Volcanic - Magma erupts quickly and cools on surface.
Both are igneous rocks
What is the order of mineral crystallization in magma
OPABQ - Olivine, Pyroxene, Amphibole, Biotite Mica, Quartz
The 3 magmas from most peaceful to most explosive eruption
Basaltic (lower H2O content), Andesitic, Rhyolitic (higher H2O content)
Decompression melting.
Lowering pressure to melt rock (In relation to volcanic eruptions.)
What 3 things cause a rock to melt in a volcano?
- Decreased or lowering pressure
- Increasing temperature
- Raised water content
How does the volcano erupt?
1.Melted rock in the form magma in depths of volcano under high pressure.
2. As rocks are molten, the magma expands releasing all the trapped gases (primarily h2o, co2, siO2) due to lower pressure, which act to aggress the volcano to erupt.
3. H2O content impacts how explosive or peaceful the eruption will be.
4. Styles of eruption - Nonexplosive Icelandic and Hawaiian…Explosive Vulcanian and Plinian
5. Rhyolitic magma usually violent due to high H2O and high viscosity
The 3 V’s of Volcanology
Viscosity - How easy does the Magma flow
Volatility - How ‘gaseous’, or explosive
Volume - Impacts the intensity of eruption
Shield Volcanoes
‘Weakest type’ Low viscosity; Low volatility; Large volume. Great width compared to height
Flood Basalt Volcanic
Low viscosity; Low volatility; Very large volume. Largest volcanic events
Scoria cones Volcanic
Medium viscosity; Medium volatility; Small volume. Can have Summit Crater with lake
Stratovolcanoes
High Viscosity; High Volatiles; Large
Volume. Steep-sided, symmetrical volcanic peaks, Plinian type.
Lahars
‘Organic mudflow’. Steam blown up settles on the slopes and condenses. This comes down with heavy rainfall or melting snow in the form of dangerous mudflow full of debris. Also includes ash and debris on volcano slope/surroundings which comes down with rain.
Lava Domes Volcanic
High Viscosity; Low Volatiles; Small
Volume. Form when high-viscosity magma at vent of volcano cools quickly into hardened plug.
Calderas Volcanic
High Viscosity; High Volatiles; Very Large
Volume. Large (2 to 75 km) volcanic depressions. Formed by roof collapses into partially emptied magma reservoirs
Resurgent Caldera