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Chapter 22 Science

Chapter 22 Science

AB
Geology is the studyof planet earth, including its composition and structure
Scientists who study earth and the processes that haveshaped earth over time are called geologists
uniformitarianismis the idea that the geologic processes that operate today also operated in the past
ancient rocks can be understoodby observing present-day geologic processes
earth can be divided into three main layers,the crust, the mantle and the core - based on the materials tha tmake up each layer
the rocky outer layer of Earth is thecrust
much of the crust is made up ofsilicates, which are rocks made of compounds silicon and oxygen and often contain metals such as aluminum, iron or calcium
beneath the crust is themantle
the mantle is athick layer of hot but solid rock
the mantle is divided intothree layers
one layer of the mantle is the lithosphere, the lithosphereis a layer of relatively cool, rigid rock that includes the uppermost part of the mantle as well as the earth's crust
Beneath the lithosphere (in the mantle)is the asthenosphere
the asthenosphere is a layerof softer, weaker rock that can flow slowly, the way taffy does
Beneath the asthensphere (in the mantle)is the stronger lower part of the mantle called the mesosphere
Beneath the mantle is thecore
the coreis a large sphere of metal that occupies the earth's center.
what are the two types of forces studied by geologistsconstructive forces and destructive forces
what are the three main layers of earththe crust, the mantle and the core
a rock is a solid combinationof minerals ormineral materials
a mineral is a naturally ocurring, inorganic solidwith crystal structure and a characteristic chemical composition
minerals areinorganic, meanting that living things did not produce them
describe three properties of minerals that can be used to describe them?the properties by which minerals can be identified include their crystal structure, color, streak, luster, density, hardness, fracture and cleavage
crystal structureis the way that atoms are arranged in a particular geometric shape
some minerals can be identifiedby color
the color of a mineral's oowderis know as its streak
the luster of a mineralis the way in which its surface reflects light
the density of a mineraldepends on its chemical composition
hardness is theresistance of a mineral to scratching
the fracture of a mineral is howthe mineral breaks
cleavage is atype of fracture in which the mineral tends to split along regular, well defined planes (flat surfaces) where the bonds are weakest
What are the three groups into which rocks are classified?igneous, sedimentary, and metamorphic - based on how they form
An igneous rock isa rock that is formed from magma
magma is a mixtureof molten rock and gases, including water vapor, which forms underground
magma that flows out of volcanoesis called lava
igneous rocks formwhen molten material cools and solidifies inside Earth or at the surface
an igneous rock that forms underground from hardened magma iscalled an intrusive rock
an igneous rock that forms at the earth's surfaceis called an extrusive rock
sediment issmall, solid pieces of material that comes from rocks or living organisms
a sedimentary rockis a rock that forms over time as sediment is squeezed and cemented together
the three main groups that geologists classify sedimentary rocks areclastic rock, chemical rocks and organic rocks
sedimentary rocks that form from thebroken fragments of other rocks are called clastic rocks
chemical rocks form when mineralsprecipitate out of a solution, like out of ocean water
organic rocks form whenorganic marine animals die and rocks form from their shells and skeletons
metamorphic rock forms whenrock is transformed by heat, pressure or chemical reactions
most metaphoric rocks form underhigh temperatures and pressures deep underground
metamorphic rocks with crystals arranged in parallel layers or bands arefoliated rocks
in the rock cycle forces within earthand at the surface cause rocks to change form
the theory of plate tectonicsexplains the formation and movement of Earth's plates
German scientist Wegener hypothesized that the continents wereonce joined in a single supercontinet which then broke apart
the supercontinent was calledPangaea
According to Wegener's hypothesis, the continentsmoved slowly across Earth's surface in a process called continental drift
the mid-ocean ridgeis a chain of underwater mountains that extends into all of the earths oceans
sea-floor spreadingis the process by which new oceanic crust is created at mid-ocean ridges as older crust moves away and magma pushes upward
as sea-floor spreading occurs, old oceanic plates sink into the mantle in the process calledsubduction
as a plate sinks through a subduction zone, it bends,forming a depression in the ocean floor called a trench
the three types of plate boundaries aredivergent boundaries, convergent boundaries and transform boundaries
plates move away from each otheralong a divergent boundary
plates come together, or collide,at a convergent boundary
at a transform boundaryplates slide past each other, moving in opposite directions.
rock is neither created or destroyedat a transform boundary
geologists found that most mountains move alongplate boundaries
an earthquake is a movement of Earth's lithosphere that occurswhen rocks in the lithosphere suddenly shift, releasing store energy
the energy relesae during an earthquake is carriedby vibrations called seismic waves
stress is a force that squeezes rockstogether, stretches or pulls them apart, or pushes them in different directions
as tectonic plates move,they cause stree in the crust, which in turn produces faults and folds
a fault is a breakin the mass of rock along which movement occurs
a fold is a bendin layers of rock
earthquakes occur because stressforces have exceeded the strength of rock
the location beneath Earth's surfacewhere an earthquake begins is called the focus
P waves (primary waves) arelongitudinal waves similar to sound waves
S waves aretransverse waves
Surface waves are waves that developwhen seismic waves reach earth's surface
to measure earthquakes and pinpoint their epicenters,geologists record seismic waves using seismograhs
a device that can detect and recordseismic waves is called a seismograph
the richter scalerates earthquakes based on measurements of the times and amplitudes of seismic waves by certain seismographs
most earthquakes are concentrated along plate boundaries,where many faults are found
a volcano is a mountain that formswhen magma reaches the surface
under certain conditions, small amounts of mantle rock can melt,forming liquid magma
the magma rises upward through the crusterupting at the surface as a volcano
before an eruptionmagma often collects in a pocket called a magma chamber
after the magma forms in a magma chamberit rises to the surface in a narrow, verticla channel called a pipe
volcanoes erupt explosively or quietlydepending on the characteristics of the magma
most volcanoes occur along plate boundaries or athot spots in the crust
a hot spot is a regionwhere hot rock extends from deep within the mantle to the surface
the tree major types of volcanos areshield volcanoes, cinder cones and composite volcanoes
a flat volcano is called ashield volcano
a small, steep-sided volcanois called a cinder cone
a volcano that produces a combinationof lava and ash is called a composite volcano
igneous features formed by magmainclude batholiths, sills, dikes and volcanic necks
kinetic energyenergy of motion
potential energyenergy that is stored as a result of position or shape
renewable resourcesare resources that grow back after they are consumed, like trees
nonrenewable resourcescannot be renewed, they are gone once they are used
the law of conservation of energystates energy can't be created or destroyed
what factors affect the strength and direction of electric fields and forceslike and opposite charges
how are electric charges transferredcharges can be tranferred by friction contacts and induction
the two types of current aredirect current and alternating current
a conductor is a materialthrough which charges can flow easily
an insulator is a material through whicha charge cannot flow
factors that affect resistance arethickness, length and temperature
how does voltage produce electric currentvoltage does work to increase the potential energy of electric charges
voltage =current (I) x resistance (r)
in a series circuita charge has only one path through which it can flow
in a parallel circutthere are two or more paths through which charges can flow
fuses preventcurrent overload in a circuit, they help maintain electrical safety
a circuit breaker is a switchthat opens when current in a circuit is too h igh
insulation protectswires
grounding is the transferof excess energy through a conductor to earth
an analog signal is a smoothlyvarying signal produced by continuously changing the voltage or current
a digital signal codesinformation as a "1" or a "0"
what factors affect the magnetic force between two magnetsopposite, attract and like repels
how can you identify the north and south poles on a diagram with field linesit is the opposite
what makes ferromagnetic materials magneticits magnetic domains
what factors will weaken the magnetic force of a magnethow the domains are aligned
geology is a way of lookingat earth. Study of planet earth including it's composition and structure
what are the layers of the earth's interiorcrus, mantle and the core
what properties are used to identify materialsluster, hardness, cleavage, color and streak
igneous rockforms when molten material cools and solidifies either inside earth or at the surface
sedimentary rockis a rock that forms over time as sediment is squeezed and cemented
metamorphic rockhas been changed by temperature, pressure or in reactions with hot water
explain the hypotheses of continental driftaccourding to Wegner's hypothesis, continents move slowly across earth's surface
describe the causes and effects of stress in Earth's crustit can make volcanoes and earthquakes
the water cycle is made up of several processes includingevaporation, transpiration, consdensation, precipitation and enventual return of flowing water
erosion cuts canyonsthrough solid rock and wears away the cliffs above beaches
the force of gravity contributes to erosionby mass movement when rain comes down it will help erode the land
when a glacier meltsit deposits its load of sediment creating a variety of landforms
glaciers cause many distinctive features in the landscapeincludes cirques, horns, u-shapped valleys and glacial lakes
wind erosed the lad bydeflation and abrasion
features depsoited by windinclude sand dunes and loess deposits
geologists use radioactivedating to determine the absolute ages of rocks
the time scale is based onrelative ages of rock layers and the use of radioactive dating t ofind the absolute ages of rock



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