Geoscience Flashcards
Layers of the Earth’s interior
Crust
Mantle
Outer core
Inner core
Plate tectonics
Aka the geological Grand Unifying Theory
- describes how plates and continents contained by them are pushed and pulled around the surface of the earth
- explains processes that build mountains
- explains patterns of distribution of earthquakes and volcanoes
Three types of tectonic plate boundaries
Convergent (colliding)
Divergent (spreading)
Transform (sliding)
Convergent boundary outputs
Oceanic-oceanic
- volcanic island chains
Continental-oceanic
- mountain ranges along edge of continent
- oceanic plate is always subducted below (oceanic crust is denser)
Continental-continental
- mountain ranges
Rocks
Naturally occuring aggregates of minerals
*manmade objects are never considered rocks or minerals
Mineral
A naturally occuring homogenous solid with a definite (but generally not fixed) chemical composition and a crystalline structure
Formed by inorganic processes
*manmade objects are never considered rocks or minerals
Gemstone
A valuable mineral that originated from an original source rock
Exceptions
- broadly, any mineral highly valued for its beauty, durability, and rarity
- can include non-minerals (organic or biological origin), eg. pearl, amber
- can include some rocks
Relationship between rocks, minerals, and gemstones
Rocks = aggregates of minerals
Gems = highly valued minerals (and some non-mineral materials)
Igneous rock
Crystallizes when molten material (melt/magma) cools
- rock is composed of interlocking crystals
- can be volcanic/extrusive or plutonic/intrusive
Volcanic/extrusive rock
Rock formed from melt cooling at the surface of the Earth
Plutonic/intrusive rock
Rock formed from melt cooling and solidifying inside the Earth
Metamorphic rock
Formed by the alteration of pre-existing rocks
Rock transformation involves heat and/or pressure, and often fluid percolating through subsurface; does not involve melting
- compression can generate heat
- compression often results from plate collision
- pressure and temperature increases with depth
- newly generated minerals may be more stable at new temperature/pressure conditions
Sedimentary rock
Physical - erosion
- weathering forms clastic sedimentary rock (eg sandstone, siltstone, mudstone –> fragments and grains of eroded rock)
Chemical - precipitation
- evaporite formed when body of water evaporates to form layers of salt
Biological - precipitation
- production of coral reefs, sediments composed of shells, and deposition of plant material in swamps (forms coal)
Diagenesis/lithification
Processes that physically cements sedimentary grains together
Involves heat, pressure, and percolating fluids (like metamorphism), but not to the extent of drastic transformation of mineralogy or structure
Rock cycle
Rock in mantle –> magma
Magma –> igneous rock (solidification)
Igneous rock –> metamorphic rock -or- sediment (weathering and erosion)
Metamorphic rock –> sediment -or- magma (partial melting)
Sediment –> sedimentary rock (lithification)
Sedimentary rock –> sediment -or- metamorphic rock (metamorphism)