The mantle lies beneath the crust and extends to about halfway down into the planet.
The Earth's crust is the outermost layer, composed mainly of silicate minerals.
The core consists of two parts - an inner solid core and an outer liquid core.
The outer core is composed mainly of molten iron and nickel, while the inner core is solid.
Earth's magnetic field is generated by convection currents within the liquid outer core.
Natural process of breaking rocks into smaller pieces over time. Water, ice, acids, salts, plants, animals, and changes in temperature are all agents of __________
weathering
Water, in either liquid or solid form, is often a key agent of _____ and is also called physical weathering and disaggregation, causes rocks to crumble
mechanical weathering
changes the molecular structure of rocks and soil.
chemical weathering
process transporting weathered material to new locations
erosion
Heat from when the planet formed and accreted, which has
not yet been lost
2. Frictional heating, caused by
denser core material sinking to
the center of the planet; and
3. Heat from the decay of
radioactive elements.
These are the....
the three main sources of heat inside the earth
formed when mineral grains line up in parallel layers
foliated rocks
formed where mineral grains (crystals) grow and rearrange, but theydo not form layers
non-foliated rocks
this refers to the changes in mineral assemblage and texture that result from subjecting a rock to conditions such pressures, temperatures, and chemical environments different from those under which the rock originally formed.
metamorphism
comes from the greek word meta = after, morph = form
metamorphism
6 types of metamorphism:
type of metamorphism where rock minerals and texture are changed, mainly by heat, due to contact with magma
contact metamorphism
occurs over a wide area. the heat and pressure are created at converge are where plates are colliding. usually produced foliated rocks
regional metamorphism
a high pressure metamorphism resulting from the crushing and shearing of rock during tectonic movement, mostly along faults
calaclastic metamorphism
rocks that are altered at high temperature and moderate pressure by hydrothermal fluids are hydrothermally metamorphosed
hydrothermal metamorphism
when sedimentary rocks are buried to depths of several kilometers, temperatures greather than 300⁰C
burial metamorphism
when an extraterrestrial body, such as meteorite or comet impacts the earth or there is a very large volcanic exploision, ultrahigh pressures can be generated in the impacted rock
shock metamorphism
metamorphism of shale
SLATE, foliated rock type
metamorphism of slate, but under greater heat and pressure than slate
PHYLLITE, foliated rock type
Often derived from metamorphism of
claystone or shale; metamorphosed under
more heat and pressure than phyllite
SCHIST, foliated rock type
metamorphism of various different rocks, under extreme conditions of heat and pressure
GNEISS, foliated rock type
contact metamorphism of various different rock types
HORNFELS, non-foliated rock type
metamorphism of sandstone
QUARTZITE, non-foliated rock type
metamorphism of limestone
MARBLE, non-foliated rock type
is the forced applied to a rock
stress
stresses that push towards each other, causing a decrease in the space a rock takes up
compressional stress
stresses that pull material in opposite directions
tensional stresses
parallel stresses that move past each other in opposite directions
shear stress
stress from the weight of material above a buried object; reduces volume
confining stress
an acient greek word meaning ''all land'' or ''entire earth''
pangaea
is the idea that the continents move. from a single landmass called pangaea
continental drift
theory that the earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core
plate tectonics
the transfer of thermal energythrough the movement of a liquid gas
thermal convection
a massive, irregularly shaped slab of solid rock, generally composed of both continental and oceanic lithosphere
tectonic plate
the edges where two plates meet
boundaries
this is a boundary where plates meet. this happens when two tectonic plates moves towards each other