midterm Flashcards
hypothesis
an idea on how something might work
theory
explains everything seen with no contradictions
declination
offset of magnetic birth from geographic north
external heat sources
climate and weather
internal heat sources
driven by radioactive decay and original heat from the nebular cloud, drives plates
theory of uniformitarianism
present is the key to the past. can look at present geological processes and extrapolate the past
age of earth
4.56 bya
pangea
supercontinent that broke up about 225mya
convection
movement of rock in mantle
lithosphere
crust and upper mantle
asthenosphere
part of the mantle that is partially molten where convection occurs
isotherm
boundary between solid and partially molten rock
divergent plate boundaries
two plates move apart from each other. create rift valleys, small volcanoes, and small, shallow earthquakes. Often associated with seafloor spreading
convergent ocean-ocean
oceanic trench, volcanic island arcs, deep earthquakes (asymmetrical)
convergent ocean-continent
volcanic mountain chain, folded mountains, deep earthquakes. oceanic plates subducts because it’s denser
convergent continent-continent
crystal thickening, folded mountains, earthquakes
transform boundaries
strike-slip faults, small earthquakes, no volcanoes, linear feature on terrain
electrostatic attraction
two types of particles have opposite charges, creating a mutual attraction
metallic bond
not very strong, atoms bonded by a “sea of electrons. allows atoms to pack closely, soft and malleable
crystal lattice
regular 3D repeated arrangement of atoms. creates cleavage in minerals
mineral
naturally occurring inorganic compound that doesn’t contain C-H-O. crystalline solid
how to identify minerals
color, hardness, cleavage, density, reaction to HCL, magnetism, luster, diapgenity
sulfur mineral group
yellow, no cleavage
silicate mineral group
most common mineral class
SiO
silicate tetrahedron
building blocks of all silicate minerals
single chain
-pyroxene
double chain
-amphibole
sheet silicates
-muscovite, biotite
framework silicates
-don’t break in cleavage
- pure SiO2
-includes quartz
most common elements in crustal rock
silicon, oxygen, aluminum
rock
naturally forming, non-living, firm, coherent aggregate of matter
igneous
formed form molten lava or magma
sedimentary
formed by particles of other rocks that are eroded, deposited, and recemented at the surface
metamorphic
sedimentary or igneous rocks that have been altered by heat and pressure
rock cycle
rocks are continually changing and evolving as result of surface and tectonic processes
weathering
chemical or mechanical breakdown of rock at the surface
erosion
sediment moved by running water, glaciers, wind, etc
extrusive igneous rock
formed above ground by lava, ash, ash flow, or an ash cloud
intrusive igneous rock
formed below ground by magma
cools slower than extrusive
xenolith
rock incorporated into another rock
rhyolitic lava
made of rhyolite, high in silica, cool, sticky, and explosive
andesitic lava
made of andesite, moderate amount of silica, cool, sticky, and explosive
basaltic lava
made of basalt, low in silica, hot, fluid, not effusive
shield volcanoes
mainly basaltic, gentle sides, long duration of activity, non-violent
pahoehoe lava
ropey, slow cooling
aa lava
produces very sharp rocks
strato volcanoes
highly explosive volcanoes along subduction zones that produce pyroclastic debris and large layers of ash
volcano earthquake techniques
eruptive history, earthquakez, ground tilting, temp, gas
mountain stream (sedimentary rocks)
high energy deposition
eruption rates > deposition rates
conglomerate
rock containing cobble
breccia
conglomerate with angular rocks
rocky beaches
large coasts indicates higher energy processes
delta deposition
stream or river loses everything in the ocean and drops the sediment it carrie’s
pluton
deep-seated intrusion of an igneous rock
dikes
igneous intrusions that cut across the layers of rock that they inteude
batholith
large igneous intrusion extending deep into the crust
sills
bed of volcanic lava between older sedimentary rock
nuee ardente volcano
highly explosive volcano that produces pyroclastic flow
lahar
violent type of mudflow/debris
joints
fracture in a rock with no offset
fault
fracture in a rock with offset
slates
very flat cleavage, common to build with
phylite
slight shine, slightly wrinkled surface
schist
obvious layering, mostly muscovite or biotite
gneiss
bands of felsic and magic minerals (layers of light and dark)
migmatite
part of rock (quartz and feldspar) has melted and recrystalized