Midterm #1 Flashcards
Geology
the study of the Earth
scientific method
the derivation of an answer from a series of Qs
scientific method steps (8)
- Q
- collect info
- generalize (eg. line of best fit)
- present an answer to hypothesis
- test it
- revise your answer
- theory
- law (rare)
why study geo? (4)
- scientific curiosity
- env protection
- natural resources
- natural hazard awareness
earth parts (4)
- crust
- mantle
- outer core
- inner core
oceanic crust features (6)
- location: ocean basins
- mafic
- black
- 7-10km thick (thinner)
- melting point of about 1300 deg C (higher)
- higher density (about 3.0g/cm^3)
continental crust features (6)
- location: emergent land masses
- felsic
- white
- 25-70km thick (thicker)
- melting point of about 700 deg C (lower)
- lower density (about 2.7g/cm^3)
plate techtonics
the theory that the eths crust is broken up to pieces/plates that move
mineral
a natural substance composed of a specific ratio of chem elements arranged in a reoccurring crystalline structure
rock
an aggregate of one or more minerals
magma
melted rock inside the eth
lava
melted rock at or near the surface of the eth
igneous rocks
form when melted rock cools and solidifies
rock types (3)
- igneous
- sedimentary
- metamorphic
sedimentary rocks
form when a pre-existing rock is weathered, eroded, transported, deposited, or precipitated, and then lithified
weathering
how a rock falls apart/disintegrates
erosion
the way rock fragments are set in motion
transport
the way in which rock fragments move once they are in motion
deposition
how a rock fragment stops moving
precipitation
the creation of a new mineral crystal from elements in solution
lithification
the transformation of loose sediment into solid rock
metamorphic rock
form when a pre-existing rock is altered by heat and pres (w/ no sig melting)
geological time scale (definition)
system of chronological measurement of the history of life (and extinctions) on eth
anthropocene epoch (5)
- radiation (5:45am July 21 1945 first test of nuclear weapon)
- carbon
- charcoal
- concrete
- plastic
how fast do plates move?
about 1-6cm per yr
1500’s
European exploration of the atlantic ocean (maps)
1700-1800’s
industrial revolution; exploration for resources
1915
Alfred Wegener publishes The Origin of Continents and Oceans (continental drift)
continental drift theory was at first not well received b/c Wagener could not explain (2)
- the driving force btwn plate motion
- what was going on in the oceans
1945-1960
improvements in tech and understanding -> today
the driving force behind plate motion
temp diffs
how plates move (4)
- hot, liq rock rises by convection
- rising body of rock cools as it approaches the surface (slows and is pushed sideways by rock beneath it)
- cooler, heavier rock sinks back into the mantle
- overlying crust is broken and pulled apart
convection currents
- cycle of moving rock in the mantle
- driving force behind plate motion
4 types of plate margins
- convergent
- divergent
- transform
- passive
3 types of convergent plate margins
- oceanic vs continental
- oceanic vs oceanic
- continental vs continental
continental vs oceanic convergent plate margin
- oceanic plate is subducted b/c it is heavier
- continental plate thickens
- mountains created
oceanic vs oceanic convergent plate margin
- chain of volcanic islands on the non-subducted plate is an island arc
- japan & aleutan islands in alaska
continental vs continental convergent plate margin
- no subduction, melting, or volcanism
- himalayas
divergent plate margin
where plates pull apart
what happens at the rift between diverging plates?
as magma/lava is introduced into the rift and cools, new oceanic crust is created, which is then carried away by plate motion
transform plate margin
- plates move past each other side to side
- no subduction melting or volcanism
passive plate margin
non active plate margin where 2 plates are joined and moving as a single unit
you can tell the orientation of the eths magnetic field by looking at what?
the arrangement of Fe in the rocks made at that time
what causes plate motion? (3)
- convection currents
- ridge push
- slab pull
ridge push
as the ridge is pushed up, gravity pulls down and outward
slab pull
thick, old, heavy crust slides back into the mantle, pulling the rest of the plate w/ it
hot spots
areas of increased volcanism unrelated to plate margin (eg. volcanism in Hawaii)
asthenosphere
a layer of semi-liquid rock found in the lower crust and upper mantle over which continental crust can move
what is the asthenosphere based on?
density of mineral content
where does the asthenosphere form?
a depth where minerals begin to melt (between the mantle and crust)
what controls the melting of minerals?
heat and pres
heat
- geothermal grad
- causes minerals to melt
- inc w/ depth inside the eth
- near the surface the rate of temp inc is 25 deg C/km