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Flashcards for final exam review
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Big Bang Theory
The prevailing model for the Universe's origin, stating it expanded from an extremely hot, dense state.
Properties of stars
Characteristics such as size, temperature, color, brightness, and composition.
Star Color
Indicates its surface temperature; hotter stars are blue, cooler stars are red.
Universe Changes
It is expanding, and the rate of expansion is accelerating.
Life Cycle of Low/Average Mass Star
Nebula, Protostar, Main Sequence Star, Red Giant, Planetary Nebula, White Dwarf.
Life Cycle of High Mass Star
Nebula, Protostar, Main Sequence Star, Red Supergiant, Supernova, Neutron Star or Black Hole.
Star Spectrum
Chemical composition, temperature, density, and motion.
Age of the Sun
Approximately 4.6 billion years old.
Major Features on the Sun’s Surface
Sunspots, Prominences, Solar Flares, Coronal Mass Ejections. Sunspots are cooler areas. Prominences are large, bright features extending from the Sun's surface. Solar flares are sudden releases of energy. CMEs are large expulsions of plasma and magnetic field from the Sun’s corona.
Light Year
The distance that light travels in one year.
Lunar Phases
New Moon, Waxing Crescent, First Quarter, Waxing Gibbous, Full Moon, Waning Gibbous, Third Quarter, Waning Crescent.
Average vs. Massive Stars
Both fuse hydrogen into helium in their cores, but massive stars are hotter, brighter, and have shorter lifespans.
Size of Our Sun
Average size. It will become a red giant, then a white dwarf.
Causes of Lunar Phases
The changing angles at which we view the illuminated surface of the Moon as it orbits Earth.
Earth's Movement Impact
Rotation causes day and night; revolution causes the year and seasons.
Major Parts of the Electromagnetic Spectrum
Radio waves, microwaves, infrared, visible light, ultraviolet, X-rays, gamma rays.
Wavelength Differences
Wavelengths vary inversely with energy; radio waves have long wavelengths, gamma rays have short wavelengths.
Parts of a Transverse Wave
Crest, trough, wavelength, amplitude.
Red Shift vs. Blue Shift
Red shift indicates that a star is moving away from us, blue shift indicates it’s moving towards us.
One Side of the Moon
The Moon is tidally locked with Earth, so its rotation period matches its orbital period.
Lunar Features
Maria (dark, smooth plains), highlands (bright, heavily cratered areas), craters.
HR Diagram
A graph that plots stars according to their luminosity and temperature which helps understand stellar evolution.
Lunar Eclipse vs. Solar Eclipse
Lunar eclipse is when Earth blocks sunlight from reaching the Moon; solar eclipse is when the Moon blocks sunlight from reaching Earth.
Lunar Phase for Eclipses
Lunar eclipses occur during a Full Moon; solar eclipses occur during a New Moon.
Major Planets of Our Solar System
Mercury, Venus, Earth, Mars (terrestrial); Jupiter, Saturn, Uranus, Neptune (gas giants). Terrestrial planets are rocky and dense; gas giants are large and made of gas.
Formation of Our Solar System
Formed from a rotating cloud of gas and dust (solar nebula) that collapsed under gravity.
Planetesimals
Small rocky or icy bodies that collided and merged to form planets.
Two Parts of Shadow
Umbra (inner, dark part of the shadow) and penumbra (outer, lighter part of the shadow).
Energy Source for Atmosphere
The Sun.
Wind Movement and Pressure
Wind moves from areas of high pressure to areas of low pressure.
Latitude Effect on Climate
Affects the angle of sunlight and the distribution of heat.
Climate Zone
Temperate.
Coriolis Effect
The apparent deflection of moving objects (like air currents) due to Earth's rotation.
Cause of Coriolis Effect
Earth's rotation.
Major Air Masses in North America
Continental polar (cP), maritime polar (mP), continental tropical (cT), maritime tropical (mT), and arctic (A).
Air Mass Over Canada
Continental polar (cP) and Arctic (A).
Layers of the Atmosphere
Troposphere, stratosphere, mesosphere, thermosphere, exosphere.
Atmospheric Layer We Live In
Troposphere.
Conditions for Hurricanes
Warm ocean water, low wind shear, and a pre-existing weather disturbance.
Types of Fronts
Cold, warm, stationary, and occluded. Air moves differently depending on the front.
Examples of Greenhouse Gasses
Carbon dioxide, methane, water vapor.
Gasses in Our Atmosphere
Nitrogen (78%), oxygen (21%), argon (0.9%), and trace amounts of other gasses.
Major Global Winds
Trade winds, westerlies, polar easterlies.
Temperature Change in Atmosphere
Temperature generally decreases with altitude in the troposphere and mesosphere, and increases with altitude in the stratosphere and thermosphere.
Conditions for Quickest Evaporation
Warm temperatures, low humidity, and high wind speeds.
Greenhouse Effect vs. Global Warming
The greenhouse effect is a natural process that warms the Earth; global warming is the increase in Earth’s average temperature due to human activities.
UV Protection
Ozone layer.
Heat Transfer from the Sun
Radiation.
Orographic Effect
The effect of mountains on rainfall. Windward side gets more precipitation, leeward side is drier.
Heat Absorption and Reflection
Earth absorbs solar radiation and reflects some back into space.
Climate vs. Weather
Climate is long-term average weather conditions; weather is short-term atmospheric conditions.
Types of Clouds
Cumulus, stratus, cirrus, and cumulonimbus. Cumulonimbus are associated with thunderstorms.
Tornado Location in the US
The Great Plains, also known as 'Tornado Alley'.
What Fossils Tell Us
They provide evidence of past life, environmental conditions, and evolutionary changes.
Movement of Land Masses
Convection currents in the mantle.
Formation of Hawaiian Islands
A hot spot.
Age of the Earth
Approximately 4.54 billion years.
Types of Volcanoes
Shield, cinder cone, and composite. Shield volcanoes erupt effusively. Cinder cone volcanoes erupt explosively. Composite volcanoes have alternating explosive and effusive eruptions.
Oceanic Fossils on Mountains
Tectonic plates have shifted, uplifting the sea floor.
Evidence of Seafloor Spreading
Magnetic striping of the ocean floor and radiometric dating of rocks.
Alfred Wegener
Proposed the Theory of Continental Drift, citing evidence such as the fit of continents, fossil distribution, and matching rock formations.
Major Layers of the Earth
Crust (solid), mantle (mostly solid, but with a plastic-like asthenosphere), outer core (liquid), inner core (solid).
Lithosphere vs. Asthenosphere
The lithosphere is the rigid outer layer made up of the crust and upper mantle; the asthenosphere is the partially molten layer below the lithosphere.
Features at Plate Boundaries
Divergent (mid-ocean ridges, rift valleys), convergent (mountains, volcanoes, trenches), transform (faults).
Youngest Ocean Floor
At mid-ocean ridges.
Theory of Plate Tectonics
Explains the movement of Earth’s lithosphere and the features and events that occur at plate boundaries.
Volcano Explosivity
The amount of dissolved gas and the viscosity of the magma.
Epicenter of an Earthquake
Using seismic waves to determine the distance from at least three seismograph stations.
Reading a Travel-Time Curve
Determining the time difference between the arrival of P-waves and S-waves.
Examples of Minerals
Quartz, feldspar, mica, etc.
Formation of Each Rock Type
Igneous rocks form from cooled magma or lava; sedimentary rocks form from compacted and cemented sediments; metamorphic rocks form when existing rocks are changed by heat and pressure.
Rocks Tell Us About History
They can indicate past environmental conditions, geological events, and the presence of resources.
Weathering vs. Erosion
Weathering is the breakdown of rocks; erosion is the transport of weathered material.
Compaction vs. Cementation
Compaction is the squeezing together of sediments; cementation is the hardening and gluing together of sediments.
Textures of the Three Types of Rocks
Igneous (coarse-grained, fine-grained, glassy), sedimentary (clastic, chemical, organic), metamorphic (foliated, non-foliated).
Glassy Texture
Rapid cooling of lava.
Intrusive vs. Extrusive Igneous Rocks
Intrusive igneous rocks cool slowly inside the Earth forming large crystals; extrusive igneous rocks cool quickly on the Earth’s surface forming small crystals or glass.
Fossil Fuels
Formed from the remains of ancient organisms.
Mohs Hardness Scale
A scale to measure the relative hardness of minerals.
Rock Cycle
A model that describes how rocks change from one type to another.
Renewable Resource
A resource that can be replenished naturally.
Characteristics of a Mineral
Naturally occurring, inorganic, solid, definite chemical composition, and ordered internal structure.
Law of Superposition
The oldest layers are on the bottom and the youngest layers are on the top.
Major Eras of Earth History
Precambrian, Paleozoic, Mesozoic, Cenozoic.
Water Distribution
97% saltwater, 3% freshwater.
Salinity
The saltiness or amount of dissolved salt in water.
Polarity
A molecule with opposite charges on either end.
Adhesion vs. Cohesion
Adhesion is the attraction of water molecules to other substances; cohesion is the attraction of water molecules to each other other.
Causes of Tides
The gravitational pull of the Moon and the Sun.
Examples of Renewable and Non-Renewable Resources
Renewable (solar, wind, water); non-renewable (coal, oil, natural gas).
Why Coal in PA
PA used to be a swampy area with lots of plant life that turned into coal over millions of years.
Parts of the Water Cycle
Evaporation, condensation, precipitation, runoff, infiltration, transpiration.
Water Doesn't Mix With Oil
Water is polar and oil is non-polar.
Water Be Created
No.
What Makes Biome Unique
Temperature and precipitation.
Ecology
The study of the interactions between organisms and their environment.
Organism Feeds On Dead Material
Detritivore or decomposer.
Producers vs. Consumers
Producers create their own food; consumers obtain food by eating other organisms.
Types of Symbiotic Relationships
Mutualism, commensalism, parasitism.
Tick/Flea Relationship
Parasitism.