Earth Science WIP Flashcards
Continental Drift Theory
continents were once joined as one supercontinent and slowly drifted apart
Alfred Wegener
proposed the continental drift theory
Seafloor Spreading Theory
a process that occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge
Plate Tectonic Theory
the Earth’s crust is divided into different plates; occurrences of volcanoes and mountains are widespread in the boundaries of each plate
Plate Boundaries
caused by convection currents in the mantle
Convergent Boundaries
2 plates slide towards each other
Mountain Ranges and high plateaus
Continental-continental convergent
(the older plate subducts under the younger plate)
Trenches, Island and Volcanic Arcs
Oceanic-oceanic convergent (the older plate subducts under the younger plate)
Trenches and Volcanic Arcs
Continental-oceanic convergent (the denser oceanic plate subducts under the less dense continental plate)
Divergent Boundaries
plates slide apart from each other
Rift Valley
Continental-continental divergent
Mid-ocean ridge
Oceanic-oceanic divergent
Transform Boundaries
plates slide pass each other
Earthquakes
Transform
Crust
outermost layer of the Earth
Mantle
middle layer of the Earth; composed of molten rock called magma
Outer core
layer of molten substance
Inner core
layer of solid substance (due to pressure)
Thinnest layer
Crust
SiAl (Silicon and Aluminum)
Continental Crust
1/3 of Earth’s surface
Continental Crust
Mostly granite
Continental Crust
2/3 of Earth’s surface
Oceanic Crust
Mostly Basalt
Oceanic Crust
SiMa (Silicon and Magnesium)
Oceanic Crust & Mantle
84% of Earth’s Volume
Mantle
NiFe (Nickel and Iron)
Core
Lithosphere
rocky and stony part covering the surface of the Earth
Asthenosphere
dense, weak layer below the crust with high temperature and pressure which makes rocks soft, semi-molten and ductile.
Conrad Discontinuity
hydrosphere-crust
Mohorovicic Discontinuity
crust-mantle
Repetti Discontinuity
upper mantle-lower mantle
Guttenberg Discontinuity
lower mantle-outer core
Lehmann Discontinuity
outer core-inner core