Earth Scie Flashcards
Intensity
Modified Mercalli’s Scale
Effects and Damages
Magnitude
Richter Scale
total energy released at its focus
Continental Plate
less Dense
Oceanic Plate
Denser
Focus
Origin of earthquake
Epicenter
above the focus
shape of the Earth
Oblate spheroid (flattened at the poled, bulging at the sides)
Diastrophism
Any movement of the Earth’s Crust
Layers of the Earth
Crust
Mantle
Outer Core
Inner core
Crust
Variety of igneous, metamorphic, sedimentary rocks
occupies less than 1% of Earth’s volume.
The upper part of the mantle is composed mostly of
peridotite, a rock denser than rocks common in the overlying crust.
Mohorovicic discontinuity
The boundary between the crust and mantle
Mantle
makes up a whopping 84% of Earth’s total volume.
silicates of iron and magnesium, sulphides and oxides of silicon and magnesium.
Molten material that surrounds the core
Mantle
Lithosphere
Solid outerpart of the Earth
included brittle upper mantle and the crust
most rigid (elastic but not viscous)
Coolest of the Earth’s layer
Asthenosphere
Much hotter and fluid than lithosphere
malleable
subduction zones
Outer Core
magma like liquid layer that surrounds the Inner Core and creates Earth’s magnetic field.
iron and some nickel
Inner Core
believed to be just as hot as the sun’s surface.
made up of an iron-nickel (metal) alloy.
Solid because of high pressures
siderophiles (gold, cobalt, platinum)
Continental Drift Theory
Alfred Wagner
Pangaea
Theory of Sea-floor spreading
occurs at mid-ocean ridges where new oceanic crust if formed through volcanic activity
support continental drift
Plate Tectonic Theory
Lithosphere is divided into tectonic plates
three types of plate boundaries
Divergent
Convergent
Transform
Mountain Ranges
formed by collision of two continental plates
Trenches
deepest part of the ocean formed by collision of continental and oceanic plate
mid-oceanic ridge
chain of mountains in the middle of the ocean
formed by spreading of the ocean floor
Faults
crack on Earth’s Crust when plates slip past each other
Volcanoes
collision of continental and Oceanic plate
molten rock, gases, pyroplastic debris erupt through the crust
magma
molten rocks beneath the crust
lava
molten rocks at the surface of the crust
Pyroplastic materials
mixtures of hot, dry rock fragment and hot gases
Mudflow
mixture of mud and water
Parts of a volcano
Crater Vent Side Vent Lava flow Pipe magma chamber
Type of Volcanoes
Cinder Cone Shield Volcano Lava Domes Stratovolcanoes Supervolcanoes Submarine volcanoes Subglacials volcanoes
Most common type
lava cools rapidly
fairly small, steep slope and builds over short periods of time
Cinder Cone