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How old is the Earth?
4.6 Billion years
What did we get the age of Earth from?
Meteorites
What was the big bang hypothesis for?
Formation of the galaxies
What was the Nebula hypothesis for?
formations of a solar system
What are three basic divisions of earth's interior?
Crust, mantle, core
Thin, rocky, outer skin of earth
Crust
composed of rock peridotite
mantle
iron nickel alloy, generates earths magnetic field
core
the rigid outer part of the earth, consisting of the crust and upper mantle.
lithosphere
the upper layer of the earth's mantle, below the lithosphere, in which there is relatively low resistance to plastic flow and convection is thought to occur.
asthenosphere
the region of the earth's atmosphere above the stratosphere and below the thermosphere, between about 30 and 50 miles (50 and 80 km) in altitude.
mesosphere
a liquid layer about 2,300 km (1,400 mi) thick composed of iron and nickel that lies above Earth's solid inner core and below its mantle.
Outer core
Earth's innermost part and according to seismological studies, it is a primarily solid ball with a radius of about 1220 kilometers, or 760 miles
Inner core
author of the continental drift hypothesis
Alfred Wegener
supercontinent formed in the paleozoic era
Pangea
Concept of seafloor spreading is by who?
Harry Hess
plates are separated along the crests of mid oceanic ridges
Seafloor spreading
Magnetic stripes are indicators of what?
magnetic reversals
red and white stripes parallel to oceanic ridges illustrate what?
magnetic reversals
lithosphere is broken into what?
plates
Plates move apart, constructive margins, zone of seafloor spreading, plates grow along these boundaries
Divergent plate boundaries
plates move toward each other, destructive margins, subduction zones in deep ocean trenches, plate is destroyed along the boundary
Convergent plate boundaries
what is an oceanic-oceanic convergent plate boundary? definition and example
two ocean plates converge. Aleutian island arc, North pacific ocean
what is an oceanic-continental convergent plate boundary? definition and example
an oceanic plate and a continental plate converge. Andes mountains
what is an continental-continental convergent plate boundary? definition and example
two continental plates converge. Himalaya mountains, tibet
what type of boundary has conservative margins and transform?
Transform fault boundaries
each plate is bounded by a combination of the
three types of boundaries
What is the basic driving force of plate tectonics
convective flow in the mantle
the convective flows export heat from deep in the mantle to the top of the
asthenosphere
two other mechanisms that drive plate motion
slab pull and slab suction
________ are building blocks of minerals
elements
________ are the building blocks of rocks
minerals
solid aggregate of minerals
rock
most common elements? 2
silicon and oxygen
most common minerals?
silicates
most common silicates?
quartz, clay minerals, and mica group (mineral muscovite)
most common non silicates?
Carbonates
what are carbonates composed of?
CaCO3- calcite
calcite is dissolved by what?
rain and ground water
what are two physical properties of minerals?
Cleavage and fracture
The tendency of a mineral to break along flat planar surfaces as determined by the structure of its crystal lattice.
Cleavage
The way a mineral breaks other than along a cleavage plane.
Fracture
What are the two types of igneous rocks?
Intrusive and extrusive
whats another name for an intrusive igneous rock?
plutonic
whats another name for an extrusive igneous rock?
volcanic
The size, shape, and arrangement of mineral grains
texture
what does texture tell us about the rock?
the origin
intrusive rocks have a _____ rate of cooling and form ________ crystals
slow, large
extrusive rocks have a _____ rate of cooling and form ________ crystals
fast, many small
very fast rates of cooling of rocks forms what?
glass
igneous rocks are composed primary of what?
silicate minerals
Dark silicates include which minerals?
Olivine, pyroxene, amphibole, and biotite
whats another name for dark silicates?
ferromagnesian
Light silicates include which minerals?
Quartz, muscovite, and feldspars
whats another name for light silicates?
nonferromagnesian
igneous composition of continental crust?
granitic
igneous composition of continental crust, stratovolcanoes?
andesitic
igneous composition of oceanic crust?
basaltic
composition of the mantle?
peridotite (ultramafic)
Largest type of volcano
shield volcano
example of a shield volcano
Hawaii
Medium sized volcano
composite cone (Stratovolcano)
Smallest volcano
Cinder cone
deadly pyroclastic flow
lahar
global distribution of igneous activity is not random, it is associated with these three things:
subduction zones, mid ocean ridges, and intraplate volcanism
what are subduction zones associated with?
convergent plate boundaries
what are mid ocean ridges associated with?
divergent plate boundaries
______ is related to mantle plums (below surface) and rift zones (at surface)
intraplate volcanism
Where is intraplate volcanism located?
lithospheric plate
What are the two types of weathering?
Mechanical and chemical
Breaking of rocks into smaller pieces
Mechanical weathering
breaks down rock components and internal structures of mineral
chemical weathering
______ and ______ are the end products of chemical weathering
clay and quartz
The rate of weathering depends on these three things:
surface area, rock characteristics, and climate
_______ and _______ climate most effectively disintegrates and decomposes rocks.
warm, moist
rounded corners, spots around minerals, and traces of dissolution show what about a rock or mineral?
evidence of weathering
what are the four steps that form a sedimentary rock?
transport, deposition, burial, and lithification
what are the two types of sedimentary rocks?
detrital and chemical
this type of sedimentary rock is formed from particles, which have been transported, deposited, and buried and undergone the lithification process
detrital
main two minerals in detrital rocks
clay and quarts
other common minerals in detrital rocks that are not the main rocks are
micas and feldspars
these sedimentary rocks precipitated from solution or through activities of water dwelling organisms
chemical
what are the three major textures of sedimentary rocks?
clastic, bioclastic, and nonclastic
texture made of inorganic particles, all detrital rocks have this texture
clastic
texture made of rocks containing parts of animal skeletons, shells, tests
bioclastic
crystalline structure (rock salt and rock gypsum have this texture)
nonclastic
three agents of metamorphism
heat, pressure, and active fluids
parent rock determines the ____________ of a metamorphic rock
chemical composition
two metamorphic textures?
foliated and non foliated
This texture is caused by the parallel orientation of microscopic grains. The name for the rock with this texture is slate , and the rock is characterized by a tendency to separate along parallel planes. Type of foliated texture
Slaty cleavage
This texture is formed by the parallel arrangement of platy minerals, usually micas, that are barely macroscopic (visible to the naked eye). The parallelism is often silky, or crenulated. The predominance of micaceous minerals imparts a sheen to the hand specimens. rocks associated with this are phyllite. type of foliated texture.
phyllitic
mode of foliation that occurs in certain metamorphic rocks . It reflects a considerable intensity of metamorphism—i.e., changes resulting from high temperatures, pressures, and deformation. rocks with this foliated texture are called schist.
schistosity
This is a coarsely foliated texture in which the minerals have been segregated into discontinuous hands, each of which is dominated by one or two minerals. These bands range in thickness from 1 mm to several centimeters. The individual mineral grains are macroscopic and impart a striped appearance to a hand specimen. Light-colored bands commonly contain quartz and feldspar. and the dark hands are commonly composed of hornblende and hiotite. Accessory minerals are common and are useful in applying specific names to these rocks. A rock with this foliated texture is called a gneiss.
gneissic
Metamorphic rocks with no visible preferred orientation of mineral grains have this texture
nonfoliated
relative dating has how many laws/principles?
5
the principle that in a series of stratified sedimentary rocks the lowest stratum is the oldest, and the younger rocks are on the top
Principle of superposition
the principle that fossils succeed each other in a definite order; any rock layer can be identified and dated on the basis of the fossil content
principle of faunal/fossil succession
the principle where sedimentary layers are initially deposited in horizontal layersThe forces of reality beat up on the earth and break it into small pieces, which then wash down rivers to the ocean and settle out on the seafloor in horizontal layers
principle of original horizontality
the principle in which the thing being cut is older than the thing doing the cutting
principle of cross cutting relationships
the principle where a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition was not continuous.
Unconformities