Earth Science
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Created by:
sweettreatjs on June 9, 2011
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Finals Semester 2 Study Guide
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53 terms
Terms | Definitions |
|---|---|
Uniformitarianism | Geologic processes that happened in the past are happening today. |
Moho | Junction of the crust and mantle. |
Lithosphere | Crust and upper part of the upper mantle |
Asthenosphere | Lower part of the upper mantle |
Lithosphere v. Asthenosphere physical properties | Lithosphere: slightly elastic & rigid - will crack and break (rubber band)Asthenosphere: taffy, plastic it can permanently change shape |
Inner Core v. Outer Core | Inner core: solid, iron&nickel, hotterOuter core: liquid, iron& sulfur |
Geologists study earth's interior | 1. Volcanic eruptions2. seismic waves/shock waves from explosions 3. meteorites 4. gravitational studies 5. drilling |
Iron & Stony Meteorites | Iron: CoreStony: Mantle |
3 types of rocks | Metamorphic: forms from other rocks by high pressure&temperature - usually undergroundIgneous: from lava/magma cooling Sedimentary: particles cemented together |
Intrusive Igneous Rocks | Crystals |
Extrusive Igneous Rocks | Air bubbles |
Sedimentary rocks 3 types | 1. Chemical: form from precipitate2. Clastic: when particles are cemented 3. Organic: from animal matter |
Plate tectonics | Pieces of earth's lithosphere (plates) that move slowly on the asthenosphere |
Alfred Wegener's Theory & Observations | Continental drift, because of "jigsaw puzzle" & observations such as the look of the continents and fossils/rocks distribution |
Why was Wegener's theory rejected? | he was not a geologist - was meteorologist & could not explain how continents could move |
What proved Wegener's theory to be correct | - Echo sound mapping should ocean floor to have mountains and valleys- Heat emission showed magma ooze from earth - Reverse rock magnetism of the sea floor |
Convection Currents | Hot material rising and cooler material sinking in a circular pattern |
Convection in mantle causes? | all tectonic activity- earthquakes - volcanoes - mountains - hot spots |
What causes mantle convection currents | differential heating from radioactive decay |
Convergent, Divergent, Transform | convergent: come togetherdivergent: move apart transform: slide next to each other |
Sea floor spreading | Divergence of ocean plates |
Rifting | Divergence of continental plates |
Subduction | Convergence of a continental&oceanic plate |
Most tectonic activity | plate boundaries |
ridge | sea floor spreading |
trench | subduction zones |
san andreas fault, which plates? | North American and Pacific |
How much more energy is released if the difference in magnitude is one | 30 times (32 technically) |
Tectonic Stress | force that causes rock to move |
faults | cracks in the lithosphere |
folds | bend in rock layer |
how are folds and faults created | tectonic stress |
focus, epicenter | focus (point underground where earthquake begins)epicenter (above focus on surface) |
Richter | rates earthquakes based on times and size of waves |
Moment Magnitude | measures amount of energy released |
Meraclli | rates earthquakes based on observations * damage |
P wave | longitudinal, causes medium (ground) to move parallel to wave direction |
S Wave | Transverse, causes medium (ground) to move, perpendicular to wave motion |
Surface Waves | transverse waves, created when seismic waves reach the surface. rolling action |
find distance to an epicenter of an earthquake | - find sp lag time (seismogram)- Look up distance on a travel time graph |
how is earthquake's epicenter found | Triangulation (3 points) |
Determine magnitude | 1. sp lag time2. s wave amplitude |
5 parts of a volcano | 1. magma chamber: pocket of magma2. Pipe: narrow vertical channel 3. Vent: Opening in ground 4. Crater: bowl shaped pit on top of central vent 5. Caldera: huge depression formed if crater collapses |
quiet eruptions | - low silica- low viscosity (thin) - high water |
Explosive eruptions | - high silica- high viscosity - low water |
Hot spots | region where hot rock extends from deep within the mantle.usually away from a plate boundary |
Cinder cone volcano | small, steep volcano. Erupts ash and cinder (big) |
Shield volcano | broad and flat, erupts very quietly |
Composite | tall & steep. erupts explosively |
Batholith Igneous | large igneous rock feature formed in core of mountains |
Sills Igneous | layer of hardened magma parallel to existing rock |
dikes Igneous | layer of hardened magma perpendicular to existing rock |
volcanic neck Igneous | magma hardening in a pipe |
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