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CRCT REVIEW SCI ENCE

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CRCT Review. Science. Rock and Minerals. Ways to Identify Minerals. Ways to Identify Minerals. Density -D=M/V. Color. Hardness -Mohs Hardness Scale. Streak (more reliable than color). Luster. Metallic -bright and reflective. Cleavage & Fracture. Nonmetallic. Submetallic - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: CRCT Review

CRCT REVIEW

S C I EN C E

Page 2: CRCT Review

ROCK AND MINERALSMineral A naturally formed,

inorganic solid that has definite chemical structure

Elements A substance that cannot be separated or broken down into simpler substances by chemical means

Compound A substance made up of atoms of two or more different elements joined by chemical bonds

Crystals A solid whose atoms, ions, or molecules are arranged in a definite pattern

Silicate minerals(1 of 2 types of minerals)

A mineral that contains a combination of silicon, oxygen, and one or more metals

Nonsilicate minerals (2 of 2 types of minerals)

A mineral that does not contain compounds of silicon and oxygen

Luster The way in which a mineral reflects light

Streak The color of the powder of a mineral

Cleavage The splitting of a mineral along smooth, flat surfaces

Fracture The manner in which a mineral breaks along either curved or irregular surfaces

Hardness A measure of the ability of a mineral to resist scratching

Density The ratio of the mass of a substance to the volume of a substance D=M/V

Reclamation

The process of returning land to its original condition after mining is completed

Ore A natural material whose concentration of economically valuable minerals is high enough for the material to be mined profitably

Rock A naturally occurring solid mixture of one or more minerals or organic matter

Way

s to

Iden

tify

Min

eral

s

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Rock Cycle

The series of processes in which a rock forms, changes from one type to another, is destroyed, and forms again by geological processes

Weathering

The process in which water, wind, ice and heat break down rock

Erosion The process by which wind, water, ice or gravity transports soil and sediment from one location to another

Deposition

The process in which material is laid down

Composition

The chemical makeup of a rock; describes either the minerals or other materials in the rock

Texture The quality of a rock that is based on the sizes, shapes, and positions of the rock’s grains

Igneous rock

Rocks formed when magma cools

Intrusive Igneous Rock

Rock formed from the cooling and solidification of magma beneath the Earth’s surface; cools slowly; large crystals

Extrusive Igneous Rock

Rock that forms as a result of volcanic activity at or near the Earth’s surface; cools fast; small or no crystals

Sedimentary Rock

Formed through erosion; 3 types: clastic, chemical, organic

Strata Layers of rockClastic Forms when rock or mineral

fragments are cemented together

Chemical Forms when minerals crystallize out of a solution such as sea water to become rock

Organic Forms from the remains of once living plants and animals

Stratification

The process in which sedimentary rocks are arranged in layers

Metamorphic rock

Result of a change in structure, texture, or composition; can be changed by heat and/or pressure

Foliated Metamorphic rock

Describes the texture of metamorphic rock in which he mineral grains are arranged in planes or bands

Nonfoliated metamorphic rock

Describes the texture of metamorphic rock in which the mineral grains are not arranged in planes or bands

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Mohs Hardness Scale1 is the softest and 10 is hardestA mineral can scratch any other minerals that are softer than itself.1 Talc 2 Gypsum3 Calcite4 Fluorite5 Apatite 6 Orthoclase7 Quartz8 Topaz 9 Corundum10 Diamond

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Ways to Identify MineralsColor

Special Propertie

s-

radioactivity

-optical-taste

-magnetism-

fluorescence

-chemical reaction

Density-D=M/V

Hardness

-Mohs Hardness

Scale

Streak(more

reliable than color)

Cleavage & Fracture

LusterMetallic-bright and reflective

Submetallic-dull and reflective

Nonmetallic

Vitreous-glass, brilliant Pearly-creamy

Waxy-greasy, oily

Silky-fibrous Earthy-rough, dull

Resinous

-plastic

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Earth’s ResourcesNatural Resource

Any natural material that is used by humans, such as water, petroleum, minerals, forests and animals

Renewable Resources

A natural resource that can be replaced at the same rate at which the resource is consumedExamples: trees, fresh water, wind, sunlight

Nonrenewable Resources

A resource that forms at a rate that is much slower than the rate at which it is consumed

Fossil Fuels A nonrenewable energy resource formed from the remains of organisms that lived long ago; examples include oil, coal, and natural gas

Mining The removal process of resources through one of two processes; surface or subsurface mining

Deforestation

The process of removing trees

Reclamation

The process of returning land to its original condition after mining is completed

Ore A natural material whose concentration of economically valuable minerals is high enough for the material to be mined profitably

Energy Conservation

The act of saving energy: ex. Turning off lights when you leave the room

Water Conversation

The act of saving water: ex. Taking shorter showers, turning off the water when brushing teeth

Air Conservation

The act of saving air by not polluting: ex. Walking, riding bikes instead of driving cars

Soil Conservation

The act of saving soil: ex: not polluting (throwing trash on side of road)

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sedimentary

clastic

extrusive

rocks

metamorphicnonfoliatedigneous

intrusive

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Weathering and ErosionWeathering

The process by which rock materials are broken down by the action of physical and chemical processes

Mechanical Weathering

The breakdown of rock into smaller pieces by physical means-extreme temperature changes and water increases rate of weathering

--agents: Ice, abrasion, wind, water, gravity, plants, animals

Ice Wedging

Result of water seeping into cracks during warm weather, then freezing and expanding during cold weather. This process continues and the crack widens.

Abrasion The grinding and wearing away of rock surfaces through the mechanical action of other rock or sand particles

Chemical Weathering

The process by which rocks break down as a result of chemical reactions-weathering is faster in warm, humid climates

--agents: Water, weak acids, airAcid Precipitation

Rain, sleet, or snow that contains a high concentration of acids

Oxidation A chemical reaction in which an element, such as iron, combines with oxygen to form an oxide

Gravity -affects weathering-the steepness of the slope of a mountain will cause the rainwater to run quicker

Erosion The process by which wind, water, ice or gravity transports soil and sediment from one location to another

Deposition The process in which material is laid

-agents: Water, wind, ice, gravity

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SoilSoil A loose mixture of

rock fragments, organic material, water, and air that can support the growth of vegetation

Bedrock The layer of rock beneath the soil

Top soil The upper, outer most layer of soil that is richest in organic material; usually 2-8 inches deep

Sub soil The soil laying directly under the top soil

Soil Texture

The soil quality that is based on the proportions of soil particles; sand, silt, clay

Sand A particle in soil that is .05-2mm in size

Silt A particle in soil that is .002-.05mm in size

Clay A particle in soil that is less than .002mm in size

Humus The dark, organic material formed in soil from the decayed remains of plants and animals

Loam Soil that contains almost equal amounts of sand, silt and clay. Soil is rich with nutrients and best suited for gardening.

Soil horizons

Series of layers of soil with humus-rich soil on top (top soil), sediment below that and bedrock on the bottom

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Ice wedging

Rock

Mechanical weathering

soil

oxidation

Chemical weathering

Parent Rock

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Layers of the EarthCrust The thin and solid

outermost layer of the Earth above the mantle

Mantle The layer of rock between the earth’s crust and core

Core The central part of the earth below the mantle

Outer Core The liquid layer of the Earth’s core that lies beneath the mantle and surrounds the inner core

Inner Core The solid, dense center of the planet that extends from the bottom of the outer core to the center of the Earth

Lithosphere

The outermost, rigid layer of the Earth. Made of two parts-the crust and rigid upper part of the mantle. The lithosphere is divided into pieces called tectonic plates

Asthenosphere

The plastic layer of the mantle on which pieces of the lithosphere move. It is made of solid rock that flows very slowly

Mesosphere The strong, lower part of the mantle, beneath the asthenosphere. It extends from the bottom of the asthenosphere to the core.

Seismic Waves

A wave of energy that travels through the Earth and away from an earthquake in all directions. Their speed depends on the density and composition of material that they pass through. A seismic wave traveling through a solid (inner core) will go faster than a seismic wave traveling through a liquid (outer core).

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Layer

Temperature

Composition

Other

Crust 0-1000OC

Oxygen, silicon, aluminum

-Thinnest layer (5-100km)-Oceanic and continental crust

Mantle

1000-3700OC

More magnesium, less aluminum and silicon than crust

-Thicker than crust-Contains more of Earth’s mass

Core 3700-7000OC

Iron, small amounts of nickel

-Roughly 1/3 of the earth’s mass

       The core is denser than the mantle because it contains materials that are denser. The crust is the least dense of the layers because it contains materials that are less dense.

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Plate TectonicsTectonic Plates

A block of lithosphere that consists of the crust and the rigid, outermost part of the mantle

Continental Drift

The hypothesis that states that the continents once formed a single landmass, broke up, and drifted to their present locations

Pangaea The single, large continent that existed 245 million years ago, before the continents drifted to their current location

Sea-floor Spreading

The process by which new oceanic lithosphere forms as magma rises toward the surface and solidifies

Plate Tectonics

The theory that explains how large pieces of the Earth’s outermost layer, called tectonic plates, move and change shape

Convergent Boundary

The boundary formed by the collision of two lithospheric plates

Divergent Boundary

The boundary between two tectonic plates that are moving away from each other

Transform Boundary

The boundary between tectonic plates that are sliding past each other horizontally

Fault A break in a body of rock along which one block slides relative to another ex: normal, reverse, strike-slip

As a result of plate tectonics:

-mountain building-uplift (rising of regions of crust)-subsidence (sinking of regions of crust)-earthquake

Fossils Fossils are used to show the age of the Earth and how it has/it changed

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Continental-Continental Collisions--When two tectonic plates with continental crust collide, they buckle and

thicken, which pushes the continental crust upward.Continental-Oceanic Collisions--When a plate with oceanic crust collides with a plate with continental

crust, the denser oceanic crust sinks into the asthenosphere. This convergent boundary has a special name: the subduction zone. Old ocean crust gets pushed into the asthenosphere, where it is remelted and recycled.

Oceanic-Oceanic Collisions--When two tectonic plates with oceanic lithosphere collide, one of the

plates with oceanic lithosphere is subducted, or sinks, under the other plate.

Moving Apart--At a divergent boundary, two tectonic plates separate from each other. As

they move apart, magma rises to fill the gap. At a mid-ocean ridge, the rising magma cools to form new sea floor.

Sliding Past--At a transform boundary, two tectonic plates slide past one another.

Because tectonic plates have irregular edges, they grind and jerk as they slide, which produces earthquakes.

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Normal Faults often form when rocks are pulled apart because of tension.

Reverse Faults often form when rocks are pushed together by compression.

Strike-Slip Faults are often formed when rocks are moved horizontally by opposing forces.

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Transform boundary

Tectonic plates

collide

separate

Divergentboundary

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Currents, Waves, TidesOcean Current

A movement of ocean water that follows a regular pattern

Surface Current

A horizontal movement of ocean water that is caused by wind and that occurs at or near the ocean’s surface

Deep Current

A streamline movement of ocean water far below the surfaceHow they form: (pg. 420)-Decreasing Temperatures-Increasing Salinity Through Freezing-Increasing Salinity Through Evaporation

Waves Movement of water formed by wind, earthquakes, or other factors

crest top of the wavetrough bottom of the wave

Tides The periodic rise and fall of the water level in the oceans and other large bodies of water

Caused: By rotation of Earth and moon’s revolution

Spring Tide

A tide of increased range that occurs two times a month, at the new and full moon

Neap Tide A tide of minimum range that occurs during the first and third quarters of the moon

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Moon Phases and EclipsesPhases The change in the sunlit

area of one celestial body (moon) as seen from another celestial body (Earth).

Waxing The sunlit fraction that we can see is from Earth is getting larger

Waning The sunlit fraction that we can see from Earth is getting smaller

   Eclipse An event in which the

shadow on one celestial body falls on another

Solar Eclipse

Occurs when the sun, moon and Earth are in line where the moon is between the sun and Earth. The moon seems to block out the sun.

Lunar Eclipse

Occurs when the sun, Earth and moon are in line where the Earth is between the sun and moon. The Earth blocks most of the sun and the reflecting light gives the moon a reddish tint.

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Earth’s Water—The Water CycleWater in the World

97% Salt Water (Oceans)3% Fresh Water (Ice Caps, Underground, Rivers, Lakes)

Salinity A measure of the amount of dissolved salts in a given amount of liquid

Composition of Ocean Water

~55% chlorine (Cl)~30% Sodium (Na)NaCl (salt)

Desalination

The process of removing salt from ocean water

Water Cycle

The continuous movement of water from the ocean to the atmosphere to the land and back to the ocean

Condensation

A change from a gas to a liquid. As water vapor rises into the atmosphere, it cools and interacts with dust particles. Eventually, the water vapor turns to liquid water

Precipitation

Solid or liquid water that falls to Earth. When water droplets become heavy enough, they fall back to Earth’s surface as precipitation. Most precipitation falls directly back to the ocean

Evaporation

The physical change from a liquid to a gas. The sun heats liquid water, causing it to rise into the atmosphere as water vapor. Water evaporates directly from oceans, lakes, rivers, falling rain, plants, animals, and other sources

Transpiration

The process by which moisture is carried through plants from roots to small pores on the underside of leaves, where it changes to vapor and is released to the atmosphere

Infiltration (percolation)

The movement of water through the ground

Runoff The water flow that occurs when the soil is infiltrated to full capacity and excess water from rain or other sources flows over the land

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Subsurface TopographySubsurface Topography

The features of the ocean floor

Seamount

A submerged mountain on the ocean floor that is at least 1,000 m high and that has a volcanic origin

Continental Shelf

The gently sloping section of the continental margin located between the shoreline and the continental slope

Continental Slope

The steeply inclined section of the continental margin located between the continental rise and continental shelf

Continental Rise

The gently sloping section of the continental margin located between the continental slope and abyssal plain

Abyssal Plain

A large, flat, almost level area of the deep-ocean basin

Mid-Ocean Ridge

A long, undersea mountain chain that forms along the floor of the major oceans

Ocean Trenches

A steep, long depression in the deep-sea floor that runs parallel to a chain of volcanic islands or a continental margin

Rift Valley A long, narrow valley that forms as tectonic plates separate

Pacific Ocean

Location: West of North AmericaLargest ocean

   Atlantic Ocean

Location: East of North America2nd largest ocean

   Indian Ocean

Location: Between Africa, Asia, and Australia3rd largest ocean

   Artic Ocean

Location: North of EuropeSmallest ocean

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Abyssal plain Mid-ocean ridge

trench

Continental shelf

Continental slope

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Waves

wavelengthcrest

Wave heightWave speed

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Atmosphere and WeatherAtmosphere

A mixture of gases that surrounds a planet or moon

Composition:

78% Nitrogen21% Oxygen1% Other (argon, carbon dioxide, water vapor, other gases)

Air pressure

The measure of the force with which are molecules push on a surface. Air pressure increases closer to the Earth’s surface.

Layers of the atmosphere

Troposphere, Stratosphere, mesosphere, Thermosphere

Troposphere

The lowest layer of the atmosphere, in which temperature decreases at a constant rate as altitude increases. ‘tropo-‘ meaning turning or change‘-sphere’ meaning ball (surrounding)

Stratosphere

The layer of the atmosphere that is above the troposphere and in which temperature increases as altitude increases. In this layer the gases are layered and do not mix much.‘strata-‘ meaning layer‘-sphere’ meaning ball

Mesosphere

The layer of the atmosphere between the stratosphere and the thermosphere and in which temperature decreases as altitude increases. ‘meso-‘ meaning middle‘-sphere’ meaning ball

Thermosphere

The uppermost layer of the atmosphere, in which temperature increases at altitude increases. In this layer the temperatures are the highest.‘thermo-‘ meaning heat‘-sphere’ meaning ball

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Atmospheric Heating

The Earth and its atmosphere are heated by processes of radiation, thermal conduction, and convection.

Radiation That transfer of energy as electromagnetic waves. Energy from the sun is absorbed by the atmosphere, land, and water and changed into thermal energy. 50% is absorbed by Earth’s surface, 25% is reflected by clouds and air, 20% is absorbed by ozone, clouds, and atmospheric gases, and 5% is reflected by Earth’s surface.

Thermal Conduction

The transfer of energy as heat through a material

Convection The movement of matter due to differences in density; the transfer of energy due to the movement of matter; circulation

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Greenhouse Effect

The warming of the surface and lower atmosphere of Earth that occurs when water vapor, carbon dioxide, and other gases absorb and reradiate thermal energy.

Global Warming

A gradual increase in average global temperature

Wind The movement of air caused by differences in air pressure

Coriolis Effect

The apparent curving of the path of a moving object from an otherwise straight path due to the Earth’s rotation

Global Winds:

Polar easterlies-prevailing winds that blow from east to west between 60o and 90o latitude in both hemispheres Westerlies-prevailing winds that blow from weat to east between 30o and 60o latitude in both hemispheresTrade winds-prevailing winds that blow northeast from 30o north latitude to the equator and that blow southeast from 30o south latitude to the equator Doldrums-area between Northern and Southern hemispheres where there is very little wind because the warm, rising air created an area of low pressureHorse latitudes-area of weak winds with sinking dry air that is about 30o to 60o south latitude. Jet streams-a narrow belt of strong winds that blow in the upper troposphere

Local Winds:

Sea and land breezes: Mountain breezes, valley breezes

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radiationpressuremesosphereatmosphere

nitrogen

troposphere

oxygen

thermosphere

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Air Masses Air Mass

A large body of air where temperature and moisture content are constant throughout

Maritime (m)

Forms over water; wet

Continental (c)

Forms over land; dry

Polar (P)

Forms over the polar regions; cold

Tropical (T)

Develops over the Tropics; warm

Cold Air Masses affecting North America:Continental polar (cP)Maritime polar (mP)Warm Air Masses affecting North America:Maritime tropical (mT)Continental tropical (cT)

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Fronts The boundary between air masses of different densities and usually different temperatures

Cold Front

Forms where cold air moves under warm air, which is less dense, and pushes the warm air up. Usually move quickly and cause thunderstorms, heavy rain or snow. Cooler air usually follows.

Warm Front

Forms where warm air moves over cold, denser air. The warm air gradually replaces the cold air. Generally brings drizzly rain followed by clear and warm weather.

Occluded Front

Forms when a warm air mass is caught between two colder air masses. The coldest air mass pushes up the warm up air mass and moves forward and meets the other cold air mass. Has cool temperatures and large amount of rain and snow.

Stationary Front

Forms when a cold air mass meets a warm air mass but does not have enough force to lift it. They remain separated and brings many days of cloudy, wet weather.

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CloudsHumidity The amount of water

vapor in the airRelative Humidity

The ratio of the amount of water vapor in the air to the amount of water vapor needed to reach saturation at a given temperature

Factors affecting relative humidity:

-Amount of water vapor-Temperature 

Measuring relative humidity:

Psychrometer which consists of a wet and dry bulb. Use a chart that shows differences in bulb readings to find relative humidity.

Condensation

The change of state from a gas to a liquid

Cloud A collection of small water droplets or ice crystals suspended in the air, which forms when the air is cooled and condensation occurs

Cumulus Cloud

A fluffy white cloud with a flat bottom that is formed with warm air rises. This type of cloud generally indicates fair weather but when large in size, cause thunderstorms (cumulonimbus cloud).

Stratus Clouds

A type of cloud that forms in layers that cover large areas and often block out sun. Fog is a type of status cloud that forms near the ground.

Cirrus Clouds

Thin, feathery, white clouds found at high altitudes that are formed when the wind is strong.

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waterhailcumulus

humidityweatherAir massescirrus

clouds

front

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Ocean currents

seasonslatitudeclimate

Prevailing windscurved

mountains

Large bodies of water

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Severe WeatherThunderstorm

A usually brief, heavy storm that consists of rain, strong winds, lightning, and thunder

Lightning An electric discharge that takes place between two oppositely charged surfaces, such as between a cloud and the ground, between two clouds, or between two parts of the same cloud.

Thunder The sound caused by the rapid expansion of air along an electric strike

Tornadoes A destructive, rotating column of air that has very high wind speeds, is visible as a funnel-shaped could, and touches the ground. Caused when wind moving in two directions causes a layer of air in the middle and begins to spin.

Hurricane A severe storm that develops over tropical oceans and whose strong winds of more than 120 km/h spiral in toward the intensely low-pressure storm center. Caused when a group of thunderstorms is moving over the water and wind in different directions meet and spin.

Eye Center of a hurricaneEl Nino A change in the

surface water temperature in the Pacific Ocean that produces a warm current

La Nina A change in the eastern Pacific Ocean in which the surface water temperature becomes unusually cool

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Tilt of the EarthWeather The short-term state

of the atmosphere, including temperature, humidity, precipitation, wind and visibility

Climate The average weather condition in an area over a long period of time

Sun’s rays…

Strike the earth’s surface at different angles because the surface of the earth is curved. More direct angle near equator and less at the poles

Seasons Differing weather during different times of the year due to the fact that the earth is tilted on its axis at 23.5o angle. The tilt affects how much solar energy an area receives at the Earth moves around the sun. Locations near the equator have less seasonal change.

Rotation The spin of a body on its axis. As the Earth rotates, only ½ of the Earth faces the sun. The half facing the sun is day and the half facing away is night.

Revolution

The motion of a body that travels around another body in space. Earth’s revolution around the Sun is about 365.25 days.

Orbit The path that a body follows as it travels around another body in space

Gravity The force that pulls two objects together. The gravity between the Earth and the moon allow for the moon to orbit the earth.

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PlanetsSatellites A natural or artificial body that

revolves around a planetMoon Revolves planets and has not

atmosphere. All planets except Mercury and Venus have moons. Earth’s moon is called Luna

Inner Planets

Consisting of Mercury, Venus, Earth and Mars. These inner planets are closets to the sun and are more closely spaced.

Terrestrial Planets

Also known as the inner planets because their surfaces are dense and rocky.

Outer Planets

Consisting of Jupiter, Saturn, Uranus, and Neptune. These outer planets are large and composed mostly of gases.

Dwarf Planet

Any object that orbits the sun, is round because of its own gravity, but has not cleared its orbital path-Pluto: demoted to dwarf planet in 2006, less than half the size of Mercury, made of ice and rock, moon named Charon

Comet A small body of ice, rock, and cosmic dust that follows an elliptical orbit around the sun and that gives off gas and dust in the form of a tail as it passes close to the sun

Asteroid

A small, rocky object that orbits the sun, usually in a band between the orbits of Mars and Jupiter

Asteroid Belt

The region of the solar system that is between the orbits of Mars and Jupiter (between the inner and outer planets) in which asteroids orbit

Meteors

A bright streak of light that results when a meteoroid burns up in the Earth’s atmosphere

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PLANETSMercury -Closest to the sun

-Takes 88 Earth days to revolve one time around sun-One day on Mercury is 59 Earth Days-Distance from the sun: 3.2 light-minutes (35, 983, 095 miles)-Surface features: Large craters, diverse temperatures (-279 to 801*F) but no atmosphere to trap the heat so it cools rapidly-Size: Diameter 3,032 miles (4,879 km), smaller than Earth-Ability to support life: No, not much of atmosphere and high temps.

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Venus

-Known as Earth’s twin/sister-Length of a year is 225 Earth days-Length of Year is 5,832 hours-Revolution is retrograde/clockwise (opposite of Earth)-Distance from the sun: 6 light-minutes (67, 237, 910 miles)-Surface features: Very high temperature of 864o*F or 462*C), Volcanoes on surface, reflective cloud cover-Size: Diameter 7,521 miles (12,104 km), similar to size of Earth -Ability to support life: No, atmosphere is mostly carbon dioxide and destructive acids

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Earth

-Only known planet to support life-Length of day is 23 hours, 56 minutes-Length of year is 365 days, 6 hours, 16 minutes-Only has one natural satellite (Moon) that keeps our climate steady and is 238,855 miles from Earth -Distance from the sun: 8.3 light minutes (92,955,820 miles)-Surface features: Water, air, weather, land-Size: Diameter 7,926 miles (12,765 km)-Ability to support life: Yes, mostly covered in water and healthy air

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Mars

-Known as the Red planet-Length of year is 687 Earth days (1 year, 322 days)-Length of day is 24 hours, 37 minutes-Two moons (Phobos and Deimos)-Distance from the sun: 12.7 light-minutes (141,633,260 miles)-Surface features: Rocky surface, volcanoes, shifting tectonic plates, dust storms, polar ice caps, temperature range from -125 to 23*F, low air pressure-Size: Diameter 4,222 miles (6,794 km), smaller than Earth-Ability to support life: No, temperature is too cold, low air pressure that water boils away

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Jupiter

-Largest planet in our solar system-See beautiful colors due to small amounts of organic compounds-Length of year is 4,331 Earth days (11 years, 313 days)-Length of the days is 9 hours, 56 minutes-63 moons—4 largest are Europa, lo, Callisto, Ganymede-Distance from the sun: 43.3 light-minutes (483,682,810 miles)-Surface features: Made mostly of hydrogen and helium like the sun, average temperature -234*F-Size: Diameter 88,846 miles (142,984 km), larger than Earth-Ability to support life: No because of the atmosphere

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Saturn

-Second largest planet-Most prominent rings (but all gas giants have rings) made of icy particles-Length of year is 10,759 Earth days (29 years, 155 days)-Length of the day is 10 hours, 39 minutes-52 moons—(Janus, Mimas, Enceladus, Tethys, Dione, Titan)-Distance from the sun: 1.3 light-hours -Surface features: Made of mostly hydrogen and helium, fast winds and rising heat cause yellow/gold banding, average temp -288*F-Size: Diameter 74,898 miles (120,536 km), larger than Earth, 764 times the volume of Earth and 95 times more massive-Ability to support life: No because of the atmosphere

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Uranus

-Tilted on its axis maybe caused from being hit by massive object -Length of year is 30,687 Earth days (83 years, 273 days)-Length of day is 17 hours, 15 minutes- Revolution is retrograde/clockwise (opposite of Earth)-27 Moons—5 major moons (Miranda, Ariel, Umbriel, Oberon, Titania)-Distance from the sun: 2.7 light-hours (1,783,939,400 miles)-Surface features: Atmosphere made up of hydrogen and methane causing bright blue color, average temperature -357*F-Size: Diameter 31,764 miles (51,118 km), larger than Earth-Ability to support life: No because of the atmosphere

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Neptune

-Outermost planet-Length of year is 60,190 Earth days (163 years, 263 days)-Length of day is 16 hours, 7 minutes-13 moons—(Nereid, Triton)-Distance from the sun: 4.2 light-hours (2,795,084,800 miles)-Surface features: Hurricane like storms, belts of clouds, blue in color from methane gas, average temperature -353*F-Size: Diameter 30,776 miles (49, 528 km), larger than Earth-Ability to support life: No because of atmosphere

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Universe and Solar SystemHeliocentric

‘sun-centered’ theory in which the sun is the center of the solar system and the Earth and other planets revolve around the sun

Geocentric

‘Earth-centered’ theory in which the Earth is the center of the solar system and the sun and other planets revolve around the Earth (old theory)

Big Bang Theory

The theory that states that the universe began with a tremendous explosion (gases under pressure) 13.7 billion years ago

Universe A vast area of loosely repeated structures. Contains our galaxy ‘The Milky Way’

Galaxy A collection of stars, dust, and gas bound together by gravity

Milky Way The galaxy that contains out solar system which contains Earth

Solar System

The collection of planets, stars, etc. that contains our planet Earth.

Hubble Telescope

A large telescope in space that astronomers use to study the solar system.

Star A collection of gases held together by gravity. The closest star to Earth is the sun.

Inertia An objects resistance in speed or direction until outside force acts on the object.

Gravity The force that attracts plants, stars, etc. and is responsible for keeping objects in orbit. Ex. Earth around the sun, moon around Earth, etc. Gravity is the force that governs the motion of the solar system.

Elliptical The shape of an elongated circle/oval. The shape of our solar system

Revolution

The motion of a body that travels around another body in space; one complete trip along an orbit

Page 52: CRCT Review